{"type": "FeatureCollection", "features": [{"id": "10.1029/2019gb006393", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:18:15Z", "type": "Journal Article", "created": "2020-02-07", "title": "Sources of Uncertainty in Regional and Global Terrestrial CO 2 Exchange Estimates", "description": "<p>The Global Carbon Budget 2018 (GCB2018) estimated by the atmospheric CO  growth rate, fossil fuel emissions, and modeled (bottom\uffe2\uff80\uff90up) land and ocean fluxes cannot be fully closed, leading to a \uffe2\uff80\uff9cbudget imbalance,\uffe2\uff80\uff9d highlighting uncertainties in GCB components. However, no systematic analysis has been performed on which regions or processes contribute to this term. To obtain deeper insight on the sources of uncertainty in global and regional carbon budgets, we analyzed differences in Net Biome Productivity (NBP) for all possible combinations of bottom\uffe2\uff80\uff90up and top\uffe2\uff80\uff90down data sets in GCB2018: (i) 16 dynamic global vegetation models (DGVMs), and (ii) 5 atmospheric inversions that match the atmospheric CO  growth rate. We find that the global mismatch between the two ensembles matches well the GCB2018 budget imbalance, with Brazil, Southeast Asia, and Oceania as the largest contributors. Differences between DGVMs dominate global mismatches, while at regional scale differences between inversions contribute the most to uncertainty. At both global and regional scales, disagreement on NBP interannual variability between the two approaches explains a large fraction of differences. We attribute this mismatch to distinct responses to El\uffc2\uffa0Ni\uffc3\uffb1o\uffe2\uff80\uff93Southern Oscillation variability between DGVMs and inversions and to uncertainties in land use change emissions, especially in South America and Southeast Asia. We identify key needs to reduce uncertainty in carbon budgets: reducing uncertainty in atmospheric inversions (e.g., through more observations in the tropics) and in land use change fluxes, including more land use processes and evaluating land use transitions (e.g., using high\uffe2\uff80\uff90resolution remote\uffe2\uff80\uff90sensing), and, finally, improving tropical hydroecological processes and fire representation within DGVMs.</p>", "keywords": ["[SDE] Environmental Sciences", "FLUXES", "550", "BURNED AREA PRODUCT", "atmospheric inversions", "01 natural sciences", "Environnement et pollution", "DATA ASSIMILATION", "Ph\u00e9nom\u00e8nes atmosph\u00e9riques", "PLANT FUNCTIONAL TYPES", "global carbon budget", "carbon cycle", "ATMOSPHERIC CO2", "0105 earth and related environmental sciences", "LAND-COVER CHANGE", "FOSSIL-FUEL", "VEGETATION MODEL ORCHIDEE", "15. Life on land", "ddc:910", "CARBON-DIOXIDE EMISSIONS", "13. Climate action", "[SDE]Environmental Sciences", "dynamic global vegetation models", "contr\u00f4le de la pollution", "Technologie de l'environnement", "INCORPORATING SPITFIRE"]}, "links": [{"href": "https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2019GB006393"}, {"href": "https://doi.org/10.1029/2019gb006393"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Global%20Biogeochemical%20Cycles", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1029/2019gb006393", "name": "item", "description": "10.1029/2019gb006393", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1029/2019gb006393"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2020-02-01T00:00:00Z"}}, {"id": "10.1029/2019ms001776", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:18:15Z", "type": "Journal Article", "created": "2019-12-20", "title": "Mathematical Reconstruction of Land Carbon Models From Their Numerical Output: Computing Soil Radiocarbon From C Dynamics", "description": "Abstract<p>Radiocarbon (14C) is a powerful tracer of the global carbon cycle that is commonly used to assess carbon cycling rates in various Earth system reservoirs and as a benchmark to assess model performance. Therefore, it has been recommended that Earth System Models (ESMs) participating in the Coupled Model Intercomparison Project Phase 6 report predicted radiocarbon values for relevant carbon pools. However, a detailed representation of radiocarbon dynamics may be an impractical burden on model developers. Here, we present an alternative approach to compute radiocarbon values from the numerical output of an ESM that does not explicitly represent these dynamics. The approach requires computed 12C stocks and fluxes among all carbon pools for a particular simulation of the model. From this output, a time\uffe2\uff80\uff90dependent linear compartmental system is computed with its respective state\uffe2\uff80\uff90transition matrix. Using transient atmospheric 14C values as inputs, the state\uffe2\uff80\uff90transition matrix is then applied to compute radiocarbon values for each pool, the average value for the entire system, and component fluxes. We demonstrate the approach with ELMv1\uffe2\uff80\uff90ECA, the land component of an ESM model that explicitly represents 12C, and 14C in 7 soil pools and 10 vertical layers. Results from our proposed method are highly accurate (relative error &lt;0.01%) compared with the ELMv1\uffe2\uff80\uff90ECA 12C and 14C predictions, demonstrating the potential to use this approach in CMIP6 and other model simulations that do not explicitly represent 14C.</p>", "keywords": ["Atmospheric sciences", "Life on Land", "Bioengineering", "Earth system models", "dynamical systems", "compartmental systems", "01 natural sciences", "Atmospheric Sciences", "13. Climate action", "Geoinformatics", "Earth Sciences", "radiocarbon", "model diagnostics", "carbon cycle models", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2019MS001776"}, {"href": "https://doi.org/10.1029/2019ms001776"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Journal%20of%20Advances%20in%20Modeling%20Earth%20Systems", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1029/2019ms001776", "name": "item", "description": "10.1029/2019ms001776", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1029/2019ms001776"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2020-01-01T00:00:00Z"}}, {"id": "10.1029/2020gl088561", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:18:15Z", "type": "Journal Article", "created": "2020-07-17", "title": "Nearshore Zone Dynamics Determine Pathway of Organic Carbon From Eroding Permafrost Coasts", "description": "Abstract<p>Collapse of permafrost coasts delivers large quantities of particulate organic carbon (POC) to Arctic coastal areas. With rapidly changing environmental conditions, sediment and organic carbon (OC) mobilization and transport pathways are also changing. Here, we assess the sources and sinks of POC in the highly dynamic nearshore zone of Herschel Island\uffe2\uff80\uff90Qikiqtaruk (Yukon, Canada). Our results show that POC concentrations sharply decrease, from 15.9 to 0.3\uffc2\uffa0mg\uffc2\uffa0L\uffe2\uff88\uff921, within the first 100\uffe2\uff80\uff93300\uffc2\uffa0m offshore. Simultaneously, radiocarbon ages of POC drop from 16,400 to 3,600 14C years, indicating rapid settling of old permafrost POC to underlying sediments. This suggests that permafrost OC is, apart from a very narrow resuspension zone (&lt;5\uffc2\uffa0m water depth), predominantly deposited in nearshore sediments. While long\uffe2\uff80\uff90term storage of permafrost OC in marine sediments potentially limits biodegradation and its subsequent release as greenhouse gas, resuspension of fine\uffe2\uff80\uff90grained, OC\uffe2\uff80\uff90rich sediments in the nearshore zone potentially enhances OC turnover.</p", "keywords": ["nearshore zone", "particulate organic carbon", "Arctic", "13. Climate action", "carbon cycle", "SDG 14 - Life Below Water", "14. Life underwater", "01 natural sciences", "Research Letters", "coastal erosion", "permafrost", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2020GL088561"}, {"href": "https://doi.org/10.1029/2020gl088561"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Geophysical%20Research%20Letters", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1029/2020gl088561", "name": "item", "description": "10.1029/2020gl088561", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1029/2020gl088561"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2020-07-31T00:00:00Z"}}, {"id": "10.1029/2022gb007489", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:18:16Z", "type": "Journal Article", "created": "2022-11-09", "title": "Mineral Soils Are an Important Intermediate Storage Pool of Black Carbon in Fennoscandian Boreal Forests", "description": "Abstract<p>Approximately 40% of earth's carbon (C) stored in land vegetation and soil is within the boreal region. This large C pool is subjected to substantial removals and transformations during periodic wildfire. Fire\uffe2\uff80\uff90altered C, commonly known as pyrogenic carbon (PyC), plays a significant role in forest ecosystem functioning and composes a considerable fraction of C transport to limnic and oceanic sediments. While PyC stores are beginning to be quantified globally, knowledge is lacking regarding the drivers of their production and transport across ecosystems. This study used the chemo\uffe2\uff80\uff90thermal oxidation at 375\uffc2\uffb0C (CTO\uffe2\uff80\uff90375) method to isolate a particularly refractory subset of PyC compounds, here called black carbon (BC), finding an average increase of 11.6\uffc2\uffa0g BC m\uffe2\uff88\uff922 at 1\uffc2\uffa0year postfire in 50 separate wildfires occurring in Sweden during 2018. These increases could not be linked to proposed drivers, however BC storage in 50 additional nearby unburnt soils related strongly to soil mass while its proportion of the larger C pool related negatively to soil C:N. Fire approximately doubled BC stocks in the mineral layer but had no significant effect on BC in the organic layer where it was likely produced. Suppressed decomposition rates and low heating during fire in mineral subsoil relative to upper layers suggests potential removals of the doubled mineral layer BC are more likely transported out of the soil system than degraded in situ. Therefore, mineral soils are suggested to be an important storage pool for BC that can buffer short\uffe2\uff80\uff90term (production in fire) and long\uffe2\uff80\uff90term (cross\uffe2\uff80\uff90ecosystem transport) BC cycling.</p", "keywords": ["Ekologi", "Ecology", "mineral soil", "Soil Science", "Geokemi", "15. Life on land", "black carbon", "Markvetenskap", "01 natural sciences", "pyrogenic carbon", "fire severity", "Geochemistry", "13. Climate action", "carbon cycle", "boreal wildfire", "Research Article", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/10.1029/2022gb007489"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Global%20Biogeochemical%20Cycles", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1029/2022gb007489", "name": "item", "description": "10.1029/2022gb007489", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1029/2022gb007489"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2022-11-01T00:00:00Z"}}, {"id": "10.1029/2024gb008104", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-06-24T16:18:17Z", "type": "Journal Article", "created": "2024-09-06", "title": "Off\u2010Shelf Transport and Biogeochemical Cycling of Terrestrial Organic Carbon Along the East Siberian Continental Margin", "description": "Abstract<p>Continental margins receive, process and sequester most of the terrestrial organic carbon (terrOC) released into the ocean. In the Arctic, increasing fluvial discharge and collapsing permafrost are expected to enhance terrOC release and degradation, leading to ocean acidification and translocated CO2 release to the atmosphere. However, the processes controlling terrOC transport beyond the continental shelf, and the amount of terrOC that reaches the slope and the rise are poorly described. Here we study terrOC transport to the Laptev Sea continental slope and rise by probing surface sediments with dual\uffe2\uff80\uff90isotope (\uffce\uffb413C/\uffce\uff9414C) source apportionment, degradation\uffe2\uff80\uff90diagnostic terrestrial biomarkers (n\uffe2\uff80\uff90alkanes, n\uffe2\uff80\uff90alkanoic acids, lignin phenols) and 210Pbxs\uffe2\uff80\uff90based mass accumulation rates (MAR). The MAR\uffe2\uff80\uff90terrOC (g\uffc2\uffa0m\uffe2\uff88\uff922\uffc2\uffa0yr\uffe2\uff88\uff921) decrease from 14.7\uffc2\uffa0\uffc2\uffb1\uffc2\uffa012.2 on the shelf, to 7.0\uffc2\uffa0\uffc2\uffb1\uffc2\uffa05.8 over the slope, to 2.3\uffc2\uffa0\uffc2\uffb1\uffc2\uffa00.3 for the rise. Scaling this to the respective regimes yields that 80% of the terrOC accumulates on the shelf, while 11% and 9% of the accumulation occurs in slope and rise sediments, respectively. TerrOC remineralization is evidenced by biomarker degradation proxies (CPI of n\uffe2\uff80\uff90alkanes and 3,5Bd/V) indicating 40% and 60% more terrOC degradation from slope to rise, consistent with a decline in terrOC concentrations by 57%. TerrOC degradation only partially explains this decline. An updated Laptev Sea terrOC budget suggests that sediment transport dynamics such as turbidity currents may drive terrOC shelf\uffe2\uff80\uff90basin export, contributing to the observed accumulation pattern. This study quantitatively demonstrates that Arctic shelf seas are key receptor systems for remobilized terrOC, emphasizing their importance in the carbon cycle of the rapidly changing Arctic.</p", "keywords": ["Arctic carbon cycle", "Arctic warming", "permafrost carbon", "Laptev Sea", "terrestrial carbon", "land-ocean carbon transfer"]}, "links": [{"href": "https://doi.org/10.1029/2024gb008104"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Global%20Biogeochemical%20Cycles", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1029/2024gb008104", "name": "item", "description": "10.1029/2024gb008104", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1029/2024gb008104"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2024-09-01T00:00:00Z"}}, {"id": "10.1038/s41586-024-07274-7", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:18:25Z", "type": "Journal Article", "created": "2024-04-17", "title": "Environmental drivers of increased ecosystem respiration in a warming tundra", "description": "Abstract<p>Arctic and alpine tundra ecosystems are large reservoirs of organic carbon1,2. Climate warming may stimulate ecosystem respiration and release carbon into the atmosphere3,4. The magnitude and persistency of this stimulation and the environmental mechanisms that drive its variation remain uncertain5\uffe2\uff80\uff937. This hampers the accuracy of global land carbon\uffe2\uff80\uff93climate feedback projections7,8. Here we synthesize 136 datasets from 56 open-top chamber in situ warming experiments located at 28 arctic and alpine tundra sites which have been running for less than 1\uffe2\uff80\uff89year up to 25\uffe2\uff80\uff89years. We show that a mean rise of 1.4\uffe2\uff80\uff89\uffc2\uffb0C [confidence interval (CI) 0.9\uffe2\uff80\uff932.0\uffe2\uff80\uff89\uffc2\uffb0C] in air and 0.4\uffe2\uff80\uff89\uffc2\uffb0C [CI 0.2\uffe2\uff80\uff930.7\uffe2\uff80\uff89\uffc2\uffb0C] in soil temperature results in an increase in growing season ecosystem respiration by 30% [CI 22\uffe2\uff80\uff9338%] (n\uffe2\uff80\uff89=\uffe2\uff80\uff89136). Our findings indicate that the stimulation of ecosystem respiration was due to increases in both plant-related and microbial respiration (n\uffe2\uff80\uff89=\uffe2\uff80\uff899) and continued for at least 25\uffe2\uff80\uff89years (n\uffe2\uff80\uff89=\uffe2\uff80\uff89136). The magnitude of the warming effects on respiration was driven by variation in warming-induced changes in local soil conditions, that is, changes in total nitrogen concentration and pH and by context-dependent spatial variation in these conditions, in particular total nitrogen concentration and the carbon:nitrogen ratio. Tundra sites with stronger nitrogen limitations and sites in which warming had stimulated plant and microbial nutrient turnover seemed particularly sensitive in their respiration response to warming. The results highlight the importance of local soil conditions and warming-induced changes therein for future climatic impacts on respiration.</p", "keywords": ["0301 basic medicine", "570", "Climatologie et m\u00e9t\u00e9orologie", "Ecosystem respiration", "tundra", "Time Factors", "ecosystem respiration", "550", "Nitrogen", "Cell Respiration", "Datasets as Topic", "Global Warming", "Article", "climate warming", "Carbon Cycle", "Soil", "03 medical and health sciences", "Tundra", "Ecosystem", "Soil Microbiology", "0303 health sciences", "Arctic Regions", "organic carbon", "Temperature", "Hydrogen-Ion Concentration", "Plants", "15. Life on land", "Settore BIOS-01/C - Botanica ambientale e applicata", "Carbon", "Climate Science", "Biologie et autres sciences connexes", "climate change", "Settore BIOS-05/A - Ecologia", "13. Climate action", "Seasons", "Warming", "Klimatvetenskap"]}, "links": [{"href": "https://www.nature.com/articles/s41586-024-07274-7.pdf"}, {"href": "https://constellation.uqac.ca/id/eprint/9807/1/Maes_et_al_2024_Nature.pdf"}, {"href": "https://doi.org/10.1038/s41586-024-07274-7"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Nature", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1038/s41586-024-07274-7", "name": "item", "description": "10.1038/s41586-024-07274-7", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1038/s41586-024-07274-7"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2024-04-17T00:00:00Z"}}, {"id": "10.1038/ismej.2011.124", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:18:19Z", "type": "Journal Article", "created": "2011-09-22", "title": "Shifts In Soil Microorganisms In Response To Warming Are Consistent Across A Range Of Antarctic Environments", "description": "Abstract<p>Because of severe abiotic limitations, Antarctic soils represent simplified systems, where microorganisms are the principal drivers of nutrient cycling. This relative simplicity makes these ecosystems particularly vulnerable to perturbations, like global warming, and the Antarctic Peninsula is among the most rapidly warming regions on the planet. However, the consequences of the ongoing warming of Antarctica on microorganisms and the processes they mediate are unknown. Here, using 16S rRNA gene pyrosequencing and qPCR, we report highly consistent responses in microbial communities across disparate sub-Antarctic and Antarctic environments in response to 3 years of experimental field warming (+0.5 to 2 \uffc2\uffb0C). Specifically, we found significant increases in the abundance of fungi and bacteria and in the Alphaproteobacteria-to-Acidobacteria ratio, which could result in an increase in soil respiration. Furthermore, shifts toward generalist bacterial communities following warming weakened the linkage between the bacterial taxonomic and functional richness. GeoChip microarray analyses also revealed significant warming effects on functional communities, specifically in the N-cycling microorganisms. Our results demonstrate that soil microorganisms across a range of sub-Antarctic and Antarctic environments can respond consistently and rapidly to increasing temperatures.</p>", "keywords": ["0301 basic medicine", "Climate Change", "Antarctic Regions", "global warming", "open-top chambers", "Soil", "03 medical and health sciences", "RNA", " Ribosomal", " 16S", "carbon cycle", "nitrogen cycle", "SDG 13 - Climate Action", "SDG 14 - Life Below Water", "14. Life underwater", "Soil Microbiology", "0303 health sciences", "Bacteria", "GeoChip microarrays", "Fungi", "Temperature", "Nitrogen Cycle", "15. Life on land", "Microarray Analysis", "Biota", "13. Climate action", "international", "Antarctica"]}, "links": [{"href": "https://doi.org/10.1038/ismej.2011.124"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/The%20ISME%20Journal", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1038/ismej.2011.124", "name": "item", "description": "10.1038/ismej.2011.124", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1038/ismej.2011.124"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2011-09-22T00:00:00Z"}}, {"id": "10.1038/ismej.2013.177", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-06-24T16:18:19Z", "type": "Journal Article", "created": "2013-10-10", "title": "Distinct Responses Of Soil Microbial Communities To Elevated Co2 And O-3 In A Soybean Agro-Ecosystem", "description": "Abstract                <p>The concentrations of atmospheric carbon dioxide (CO2) and tropospheric ozone (O3) have been rising due to human activities. However, little is known about how such increases influence soil microbial communities. We hypothesized that elevated CO2 (eCO2) and elevated O3 (eO3) would significantly affect the functional composition, structure and metabolic potential of soil microbial communities, and that various functional groups would respond to such atmospheric changes differentially. To test these hypotheses, we analyzed 96 soil samples from a soybean free-air CO2 enrichment (SoyFACE) experimental site using a comprehensive functional gene microarray (GeoChip 3.0). The results showed the overall functional composition and structure of soil microbial communities shifted under eCO2, eO3 or eCO2+eO3. Key functional genes involved in carbon fixation and degradation, nitrogen fixation, denitrification and methane metabolism were stimulated under eCO2, whereas those involved in N fixation, denitrification and N mineralization were suppressed under eO3, resulting in the fact that the abundance of some eO3-supressed genes was promoted to ambient, or eCO2-induced levels by the interaction of eCO2+eO3. Such effects appeared distinct for each treatment and significantly correlated with soil properties and soybean yield. Overall, our analysis suggests possible mechanisms of microbial responses to global atmospheric change factors through the stimulation of C and N cycling by eCO2, the inhibition of N functional processes by eO3 and the interaction by eCO2 and eO3. This study provides new insights into our understanding of microbial functional processes in response to global atmospheric change in soybean agro-ecosystems.</p>", "keywords": ["0301 basic medicine", "2. Zero hunger", "0303 health sciences", "Glycine max", "Nitrogen", "Phosphorus", "Carbon Dioxide", "15. Life on land", "Carbon", "Carbon Cycle", "03 medical and health sciences", "Ozone", "13. Climate action", "Ecosystem", "Soil Microbiology", "Sulfur"]}, "links": [{"href": "https://doi.org/10.1038/ismej.2013.177"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/The%20ISME%20Journal", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1038/ismej.2013.177", "name": "item", "description": "10.1038/ismej.2013.177", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1038/ismej.2013.177"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2013-10-10T00:00:00Z"}}, {"id": "10.1038/nature12129", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:18:19Z", "type": "Journal Article", "created": "2013-05-14", "title": "Long-Term Warming Restructures Arctic Tundra Without Changing Net Soil Carbon Storage", "description": "High latitudes contain nearly half of global soil carbon, prompting interest in understanding how the Arctic terrestrial carbon balance will respond to rising temperatures. Low temperatures suppress the activity of soil biota, retarding decomposition and nitrogen release, which limits plant and microbial growth. Warming initially accelerates decomposition, increasing nitrogen availability, productivity and woody-plant dominance. However, these responses may be transitory, because coupled abiotic-biotic feedback loops that alter soil-temperature dynamics and change the structure and activity of soil communities, can develop. Here we report the results of a two-decade summer warming experiment in an Alaskan tundra ecosystem. Warming increased plant biomass and woody dominance, indirectly increased winter soil temperature, homogenized the soil trophic structure across horizons and suppressed surface-soil-decomposer activity, but did not change total soil carbon or nitrogen stocks, thereby increasing net ecosystem carbon storage. Notably, the strongest effects were in the mineral horizon, where warming increased decomposer activity and carbon stock: a 'biotic awakening' at depth.", "keywords": ["Food Chain", "Time Factors", "Nitrogen", "Rain", "Global Warming", "History", " 21st Century", "01 natural sciences", "Carbon Cycle", "Soil", "Animals", "Biomass", "Photosynthesis", "Ecosystem", "Soil Microbiology", "0105 earth and related environmental sciences", "Arctic Regions", "Temperature", "Discriminant Analysis", "04 agricultural and veterinary sciences", "History", " 20th Century", "Plants", "15. Life on land", "Cold Climate", "Carbon", "13. Climate action", "0401 agriculture", " forestry", " and fisheries"], "contacts": [{"organization": "Gaius R. Shaver, John C. Moore, Joshua P. Schimel, Seeta A. Sistla, Rodney T. Simpson, Laura Gough,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.1038/nature12129"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Nature", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1038/nature12129", "name": "item", "description": "10.1038/nature12129", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1038/nature12129"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2013-05-01T00:00:00Z"}}, {"id": "10.1038/nature12670", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:18:19Z", "type": "Journal Article", "created": "2013-10-29", "title": "Decoupling Of Soil Nutrient Cycles As A Function Of Aridity In Global Drylands", "description": "The biogeochemical cycles of carbon (C), nitrogen (N) and phosphorus (P) are interlinked by primary production, respiration and decomposition in terrestrial ecosystems. It has been suggested that the C, N and P cycles could become uncoupled under rapid climate change because of the different degrees of control exerted on the supply of these elements by biological and geochemical processes. Climatic controls on biogeochemical cycles are particularly relevant in arid, semi-arid and dry sub-humid ecosystems (drylands) because their biological activity is mainly driven by water availability. The increase in aridity predicted for the twenty-first century in many drylands worldwide may therefore threaten the balance between these cycles, differentially affecting the availability of essential nutrients. Here we evaluate how aridity affects the balance between C, N and P in soils collected from 224 dryland sites from all continents except Antarctica. We find a negative effect of aridity on the concentration of soil organic C and total N, but a positive effect on the concentration of inorganic P. Aridity is negatively related to plant cover, which may favour the dominance of physical processes such as rock weathering, a major source of P to ecosystems, over biological processes that provide more C and N, such as litter decomposition. Our findings suggest that any predicted increase in aridity with climate change will probably reduce the concentrations of N and C in global drylands, but increase that of P. These changes would uncouple the C, N and P cycles in drylands and could negatively affect the provision of key services provided by these ecosystems.", "keywords": ["0301 basic medicine", "Nitrogen", "Biolog\u00eda", "Climate Change", "Carbon Cycle", "Soil", "03 medical and health sciences", "Ecological Impacts of Climate Change", "XXXXXX - Unknown", "Ecological impacts of climate change and ecological adaptation", "Biomass", "Desiccation", "Ecosystem", "Soil Chemistry (excl Carbon Sequestration Science)", "2. Zero hunger", "drylands", "Geography", "soil fertility", "Phosphorus", "04 agricultural and veterinary sciences", "biogeochemical cycle", "Models", " Theoretical", "Nitrogen Cycle", "Plants", "15. Life on land", "Carbon", "Phosphoric Monoester Hydrolases", "Soil chemistry and soil carbon sequestration (excl. carbon sequestration science)", "climate change", "Medio Ambiente", "13. Climate action", "Ecosystem Function", "Clay", "0401 agriculture", " forestry", " and fisheries", "Aluminum Silicates", "Desert Climate"]}, "links": [{"href": "https://doi.org/10.1038/nature12670"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Nature", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1038/nature12670", "name": "item", "description": "10.1038/nature12670", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1038/nature12670"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2013-10-01T00:00:00Z"}}, {"id": "10.1038/nature24668", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:18:19Z", "type": "Journal Article", "created": "2017-12-08", "title": "Fire frequency drives decadal changes in soil carbon and nitrogen and ecosystem productivity", "description": "Fire frequency is changing globally and is projected to affect the global carbon cycle and climate. However, uncertainty about how ecosystems respond to decadal changes in fire frequency makes it difficult to predict the effects of altered fire regimes on the carbon cycle; for instance, we do not fully understand the long-term effects of fire on soil carbon and nutrient storage, or whether fire-driven nutrient losses limit plant productivity. Here we analyse data from 48 sites in savanna grasslands, broadleaf forests and needleleaf forests spanning up to 65 years, during which time the frequency of fires was altered at each site. We find that frequently burned plots experienced a decline in surface soil carbon and nitrogen that was non-saturating through time, having 36 per cent (\u00b113 per cent) less carbon and 38 per cent (\u00b116 per cent) less nitrogen after 64 years than plots that were protected from fire. Fire-driven carbon and nitrogen losses were substantial in savanna grasslands and broadleaf forests, but not in temperate and boreal needleleaf forests. We also observe comparable soil carbon and nitrogen losses in an independent field dataset and in dynamic model simulations of global vegetation. The model study predicts that the long-term losses of soil nitrogen that result from more frequent burning may in turn decrease the carbon that is sequestered by net primary productivity by about 20 per cent of the total carbon that is emitted from burning biomass over the same period. Furthermore, we estimate that the effects of changes in fire frequency on ecosystem carbon storage may be 30 per cent too low if they do not include multidecadal changes in soil carbon, especially in drier savanna grasslands. Future changes in fire frequency may shift ecosystem carbon storage by changing soil carbon pools and nitrogen limitations on plant growth, altering the carbon sink capacity of frequently burning savanna grasslands and broadleaf forests.", "keywords": ["2. Zero hunger", "Carbon Sequestration", "Time Factors", "Nitrogen", "carbon", "Geographic Mapping", "Phosphorus", "15. Life on land", "Grassland", "01 natural sciences", "nitrogen", "Carbon", "Wildfires", "Soil", "Spatio-Temporal Analysis", "13. Climate action", "XXXXXX - Unknown", "Potassium", "carbon cycle (biogeochemistry)", "Calcium", "ecosystems", "soils", "fire", "Ecosystem", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/10.1038/nature24668"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Nature", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1038/nature24668", "name": "item", "description": "10.1038/nature24668", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1038/nature24668"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2017-12-11T00:00:00Z"}}, {"id": "10.1038/ncomms13653", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:18:20Z", "type": "Journal Article", "created": "2016-11-29", "title": "Massive remobilization of permafrost carbon during post-glacial warming", "description": "Abstract<p>Recent hypotheses, based on atmospheric records and models, suggest that permafrost carbon (PF-C) accumulated during the last glaciation may have been an important source for the atmospheric CO2 rise during post-glacial warming. However, direct physical indications for such PF-C release have so far been absent. Here we use the Laptev Sea (Arctic Ocean) as an archive to investigate PF-C destabilization during the last glacial\uffe2\uff80\uff93interglacial period. Our results show evidence for massive supply of PF-C from Siberian soils as a result of severe active layer deepening in response to the warming. Thawing of PF-C must also have brought about an enhanced organic matter respiration and, thus, these findings suggest that PF-C may indeed have been an important source of CO2 across the extensive permafrost domain. The results challenge current paradigms on the post-glacial CO2 rise and, at the same time, serve as a harbinger for possible consequences of the present-day warming of PF-C soils.</p", "keywords": ["550", "Science", "Q", "Permafrost", "Carbon cycle (Biogeochemistry)", "Climatic changes", "Biogeochemistry", "15. Life on land", "01 natural sciences", "Article", "13. Climate action", "SDG 13 - Climate Action", "SDG 14 - Life Below Water", "LAPTEV SEA SHELF; PARTICULATE ORGANIC-MATTER; LAST GLACIAL TERMINATION; ADJACENT NEARSHORE ZONE; GREENLAND STADIAL 1; LENA RIVER DELTA; INTERIOR ALASKA; YOUNGER DRYAS; ARCTIC-OCEAN; NE SIBERIA", "Cryosphere", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://www.nature.com/articles/ncomms13653.pdf"}, {"href": "https://doi.org/10.1038/ncomms13653"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Nature%20Communications", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1038/ncomms13653", "name": "item", "description": "10.1038/ncomms13653", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1038/ncomms13653"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2016-11-29T00:00:00Z"}}, {"id": "10.1038/ncomms15347", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:18:20Z", "type": "Journal Article", "created": "2017-05-17", "title": "Global perturbation of organic carbon cycling by river damming", "description": "Abstract<p>The damming of rivers represents one of the most far-reaching human modifications of the flows of water and associated matter from land to sea. Dam reservoirs are hotspots of sediment accumulation, primary productivity (P) and carbon mineralization (R) along the river continuum. Here we show that for the period 1970\uffe2\uff80\uff932030, global carbon mineralization in reservoirs exceeds carbon fixation (P&lt;R); the global P/R ratio, however, varies significantly, from 0.20 to 0.58 because of the changing age distribution of dams. We further estimate that at the start of the twenty-first century, in-reservoir burial plus mineralization eliminated 4.0\uffc2\uffb10.9\uffe2\uff80\uff89Tmol per year (48\uffc2\uffb111 Tg C per year) or 13% of total organic carbon (OC) carried by rivers to the oceans. Because of the ongoing boom in dam building, in particular in emerging economies, this value could rise to 6.9\uffc2\uffb11.5\uffe2\uff80\uff89Tmol per year (83\uffc2\uffb118 Tg C per year) or 19% by 2030.</p", "keywords": ["Environnement et pollution", "13. Climate action", "Science", "Q", "Earth Sciences", "G\u00e9ochimie", "Biogeochemistry", " carbon cycle", " dams and reservoirs", "01 natural sciences", "Article", "6. Clean water", "Atmospheric Sciences", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://escholarship.org/content/qt341579vd/qt341579vd.pdf"}, {"href": "https://dipot.ulb.ac.be/dspace/bitstream/2013/251365/3/doi_234992.pdf"}, {"href": "https://doi.org/10.1038/ncomms15347"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Nature%20Communications", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1038/ncomms15347", "name": "item", "description": "10.1038/ncomms15347", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1038/ncomms15347"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2017-05-17T00:00:00Z"}}, {"id": "10.1038/s41396-021-01110-w", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-06-24T16:18:21Z", "type": "Journal Article", "created": "2021-09-30", "title": "Microbial storage and its implications for soil ecology", "description": "Abstract                <p>Organisms throughout the tree of life accumulate chemical resources, in particular forms or compartments, to secure their availability for future use. Here we review microbial storage and its ecological significance by assembling several rich but disconnected lines of research in microbiology, biogeochemistry, and the ecology of macroscopic organisms. Evidence is drawn from various systems, but we pay particular attention to soils, where microorganisms play crucial roles in global element cycles. An assembly of genus-level data demonstrates the likely prevalence of storage traits in soil. We provide a theoretical basis for microbial storage ecology by distinguishing a spectrum of storage strategies ranging from surplus storage (storage of abundant resources that are not immediately required) to reserve storage (storage of limited resources at the cost of other metabolic functions). This distinction highlights that microorganisms can invest in storage at times of surplus and under conditions of scarcity. We then align storage with trait-based microbial life-history strategies, leading to the hypothesis that ruderal species, which are adapted to disturbance, rely less on storage than microorganisms adapted to stress or high competition. We explore the implications of storage for soil biogeochemistry, microbial biomass, and element transformations and present a process-based model of intracellular carbon storage. Our model indicates that storage can mitigate against stoichiometric imbalances, thereby enhancing biomass growth and resource-use efficiency in the face of unbalanced resources. Given the central roles of microbes in biogeochemical cycles, we propose that microbial storage may be influential on macroscopic scales, from carbon cycling to ecosystem stability.</p", "keywords": ["0301 basic medicine", "2. Zero hunger", "Soil", "0303 health sciences", "03 medical and health sciences", "13. Climate action", "international", "Life Science", "15. Life on land", "Carbon", "Ecosystem", "Soil Microbiology", "Carbon Cycle"]}, "links": [{"href": "https://www.nature.com/articles/s41396-021-01110-w.pdf"}, {"href": "https://doi.org/10.1038/s41396-021-01110-w"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/The%20ISME%20Journal", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1038/s41396-021-01110-w", "name": "item", "description": "10.1038/s41396-021-01110-w", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1038/s41396-021-01110-w"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2021-09-30T00:00:00Z"}}, {"id": "10.1038/s41396-023-01467-0", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-06-24T16:18:21Z", "type": "Journal Article", "created": "2023-07-14", "title": "Nitrification and beyond: metabolic versatility of ammonia oxidising archaea", "description": "Abstract                <p>Ammonia oxidising archaea are among the most abundant living organisms on Earth and key microbial players in the global nitrogen cycle. They carry out oxidation of ammonia to nitrite, and their activity is relevant for both food security and climate change. Since their discovery nearly 20 years ago, major insights have been gained into their nitrogen and carbon metabolism, growth preferences and their mechanisms of adaptation to the environment, as well as their diversity, abundance and activity in the environment. Despite significant strides forward through the cultivation of novel organisms and omics-based approaches, there are still many knowledge gaps on their metabolism and the mechanisms which enable them to adapt to the environment. Ammonia oxidising microorganisms are typically considered metabolically streamlined and highly specialised. Here we review the physiology of ammonia oxidising archaea, with focus on aspects of metabolic versatility and regulation, and discuss these traits in the context of nitrifier ecology.</p", "keywords": ["2. Zero hunger", "Ammonia", "13. Climate action", "Review Article", "Nitrogen Cycle", "15. Life on land", "Archaea", "Nitrification", "Oxidation-Reduction", "Soil Microbiology"], "contacts": [{"organization": "Chloe L Wright, Laura E Lehtovirta-Morley,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.1038/s41396-023-01467-0"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/The%20ISME%20Journal", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1038/s41396-023-01467-0", "name": "item", "description": "10.1038/s41396-023-01467-0", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1038/s41396-023-01467-0"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2023-07-14T00:00:00Z"}}, {"id": "10.1038/s41467-017-00114-5", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:18:21Z", "type": "Journal Article", "created": "2017-07-17", "title": "Recent increases in terrestrial carbon uptake at little cost to the water cycle", "description": "Abstract<p>Quantifying the responses of the coupled carbon and water cycles to current global warming and rising atmospheric CO2 concentration is crucial for predicting and adapting to climate changes. Here we show that terrestrial carbon uptake (i.e. gross primary production) increased significantly from 1982 to 2011 using a combination of ground-based and remotely sensed land and atmospheric observations. Importantly, we find that the terrestrial carbon uptake increase is not accompanied by a proportional increase in water use (i.e. evapotranspiration) but is largely (about 90%) driven by increased carbon uptake per unit of water use, i.e. water use efficiency. The increased water use efficiency is positively related to rising CO2 concentration and increased canopy leaf area index, and negatively influenced by increased vapour pressure deficits. Our findings suggest that rising atmospheric CO2 concentration has caused a shift in terrestrial water economics of carbon uptake.</p>", "keywords": ["Atmospheric sciences", "GLOBAL-SCALE", "Climate Change and Variability Research", "02 engineering and technology", "7. Clean energy", "01 natural sciences", "Terrestrial ecosystem", "Carbon fibers", "Climate change", "Terrestrial plant", "Global and Planetary Change", "CLIMATE-CHANGE", "EVAPOTRANSPIRATION", "Evapotranspiration", "Primary production", "Ecology", "Global warming", "Q", "TRANSPIRATION", "Composite number", "Geology", "Carbon cycle", "6. Clean water", "Physical Sciences", "8. Economic growth", "DIOXIDE", "Water-use efficiency", "Composite material", "Atmospheric carbon cycle", "Science", "Carbon dioxide in Earth's atmosphere", "STOMATAL CONDUCTANCE", "0207 environmental engineering", "Article", "Environmental science", "USE EFFICIENCY", "ATMOSPHERIC CO2", "Irrigation", "Biology", "Ecosystem", "0105 earth and related environmental sciences", "Global Forest Drought Response and Climate Change", "FOS: Earth and related environmental sciences", "15. Life on land", "TRENDS", "Materials science", "Carbon dioxide", "13. Climate action", "Earth and Environmental Sciences", "FOS: Biological sciences", "Environmental Science", "Global Methane Emissions and Impacts", "VEGETATION", "Water cycle", "Climate Modeling", "Water use"]}, "links": [{"href": "https://www.nature.com/articles/s41467-017-00114-5.pdf"}, {"href": "https://doi.org/10.1038/s41467-017-00114-5"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Nature%20Communications", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1038/s41467-017-00114-5", "name": "item", "description": "10.1038/s41467-017-00114-5", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1038/s41467-017-00114-5"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2017-07-24T00:00:00Z"}}, {"id": "10.1038/s41467-018-05980-1", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:18:22Z", "type": "Journal Article", "created": "2018-08-29", "title": "Land use driven change in soil pH affects microbial carbon cycling processes", "description": "Abstract<p>Soil microorganisms act as gatekeepers for soil\uffe2\uff80\uff93atmosphere carbon exchange by balancing the accumulation and release of soil organic matter. However, poor understanding of the mechanisms responsible hinders the development of effective land management strategies to enhance soil carbon storage. Here we empirically test the link between microbial ecophysiological traits and topsoil carbon content across geographically distributed soils and land use contrasts. We discovered distinct pH controls on microbial mechanisms of carbon accumulation. Land use intensification in low-pH soils that increased the pH above a threshold (~6.2) leads to carbon loss through increased decomposition, following alleviation of acid retardation of microbial growth. However, loss of carbon with intensification in near-neutral pH soils was linked to decreased microbial biomass and reduced growth efficiency that was, in turn, related to trade-offs with stress alleviation and resource acquisition. Thus, less-intensive management practices in near-neutral pH soils have more potential for carbon storage through increased microbial growth efficiency, whereas in acidic soils, microbial growth is a bigger constraint on decomposition rates.</p", "keywords": ["572 Biochemistry", "BACTERIAL", "ILLUMINA SEQUENCING PLATFORM", "550", "Supplementary Data", "QH301 Biology", "General Physics and Astronomy", "microbial ecology", "Soil", "Biomass", "Soil Microbiology", "SDG 15 - Life on Land", "FUNGAL", "2. Zero hunger", "Carbon Isotopes", "Environmental microbiology", "Ecology", "Q", "ecosystem ecology", "Agriculture", "04 agricultural and veterinary sciences", "Hydrogen-Ion Concentration", "Grassland", "soil microbiology", "6. Clean water", "COMMUNITY", "GROWTH", "TURNOVER", "570", "PIPELINE", "Science", "Culture and Communities", "General Biochemistry", "Genetics and Molecular Biology", "Microbial Consortia", "General Biochemistry", " Genetics and Molecular Biology", "Article", "Applied microbiology", "QH301", "carbon cycle", "USE EFFICIENCY", "PHYSIOLOGY", "QD415-436 Biochemistry", "Natural Environment Research Council (NERC)", "NE/M017125/1", "General Chemistry", "Carbon Dioxide", "15. Life on land", "Carbon", "United Kingdom", "CLIMATE", "13. Climate action", "0401 agriculture", " forestry", " and fisheries"]}, "links": [{"href": "https://centaur.reading.ac.uk/78980/8/s41467-018-05980-1.pdf"}, {"href": "https://doi.org/10.1038/s41467-018-05980-1"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Nature%20Communications", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1038/s41467-018-05980-1", "name": "item", "description": "10.1038/s41467-018-05980-1", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1038/s41467-018-05980-1"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2018-09-04T00:00:00Z"}}, {"id": "10.1038/s41558-025-02356-4", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:18:24Z", "type": "Journal Article", "created": "2025-06-13", "title": "Future climate-driven fires may boost ocean productivity in the iron-limited North Atlantic", "description": "Rapid shifts in fire regimes affect the carbon cycle by releasing carbon and nutrients such as iron (Fe), potentially enhancing marine productivity and carbon export. Here we use fire emission projections and Earth system models to examine how climate-driven changes in fire emissions may alter soluble Fe (SFe) deposition and productivity. By century\u2019s end, climate change could increase Fe emissions from fires by 1.7\u20131.8 times beyond projections considering only direct human influences. Model projections show rising SFe deposition in Northern Hemisphere high latitudes under increasing socio-economic activity, potentially boosting the impact of SFe deposition on productivity in the Fe-limited North Atlantic by up to 20% annually (40% in summer), assuming stable macronutrient levels. However, declining macronutrient availability may shrink Fe-limited areas, where climate-driven fires could offset productivity losses by 7\u20138%. In the Southern Ocean, fossil fuel emissions primarily control SFe deposition, as reductions in anthropogenic fires counterbalance climate-driven increases.", "keywords": ["Fire emissions", "\u00c0rees tem\u00e0tiques de la UPC::Desenvolupament hum\u00e0 i sostenible::Degradaci\u00f3 ambiental::Canvi clim\u00e0tic", "Climate change", "Carbon cycle", "Iron (Fe)", "Article"]}, "links": [{"href": "https://doi.org/10.1038/s41558-025-02356-4"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Nature%20Climate%20Change", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1038/s41558-025-02356-4", "name": "item", "description": "10.1038/s41558-025-02356-4", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1038/s41558-025-02356-4"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2025-06-13T00:00:00Z"}}, {"id": "10.1038/s41467-022-31833-z", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-06-24T16:18:23Z", "type": "Journal Article", "created": "2022-07-20", "title": "Drivers and trends of global soil microbial carbon over two decades", "description": "Abstract<p>Soil microorganisms are central to sustain soil functions and services, like carbon and nutrient cycling. Currently, we only have a limited understanding of the spatial-temporal dynamics of soil microorganisms, restricting our ability to assess long-term effects of climate and land-cover change on microbial roles in soil biogeochemistry. This study assesses the temporal trends in soil microbial biomass carbon and identifies the main drivers of biomass change regionally and globally to detect the areas sensitive to these environmental factors. Here, we combined a global soil microbial biomass carbon data set, random forest modelling, and environmental layers to predict spatial-temporal dynamics of microbial biomass carbon stocks from 1992 to 2013. Soil microbial biomass carbon stocks decreased globally by 3.4\uffe2\uff80\uff89\uffc2\uffb1\uffe2\uff80\uff893.0% (mean\uffe2\uff80\uff89\uffc2\uffb1\uffe2\uff80\uff8995% CI) between 1992 and 2013 for the predictable regions, equivalent to 149 Mt being lost over the period, or ~1\uffe2\uff80\uffb0 of soil C. Northern areas with high soil microbial carbon stocks experienced the strongest decrease, mostly driven by increasing temperatures. In contrast, land-cover change was a weaker global driver of change in microbial carbon, but had, in some cases, important regional effects.</p", "keywords": ["0301 basic medicine", "2. Zero hunger", "0303 health sciences", "Science", "Q", "15. Life on land", "Article", "Carbon", "Carbon Cycle", "Soil", "03 medical and health sciences", "13. Climate action", "Biomass", "Ecosystem", "Soil Microbiology"]}, "links": [{"href": "https://www.nature.com/articles/s41467-022-31833-z.pdf"}, {"href": "https://doi.org/10.1038/s41467-022-31833-z"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Nature%20Communications", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1038/s41467-022-31833-z", "name": "item", "description": "10.1038/s41467-022-31833-z", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1038/s41467-022-31833-z"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2022-07-20T00:00:00Z"}}, {"id": "10.1038/s41467-024-50245-9", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:18:23Z", "type": "Journal Article", "created": "2024-07-17", "title": "The impact of insect herbivory on biogeochemical cycling in broadleaved forests varies with temperature", "description": "Abstract<p>Herbivorous insects alter biogeochemical cycling within forests, but the magnitude of these impacts, their global variation, and drivers of this variation remain poorly understood. To address this knowledge gap and help improve biogeochemical models, we established a global network of 74 plots within 40 mature, undisturbed broadleaved forests. We analyzed freshly senesced and green leaves for carbon, nitrogen, phosphorus and silica concentrations, foliar production and herbivory, and stand-level nutrient fluxes. We show more nutrient release by insect herbivores at non-outbreak levels in tropical forests than temperate and boreal forests, that these fluxes increase strongly with mean annual temperature, and that they exceed atmospheric deposition inputs in some localities. Thus, background levels of insect herbivory are sufficiently large to both alter ecosystem element cycling and influence terrestrial carbon cycling. Further, climate can affect interactions between natural populations of plants and herbivores with important consequences for global biogeochemical cycles across broadleaved forests.</p", "keywords": ["0106 biological sciences", "0301 basic medicine", "Insecta", "Nitrogen", "Science", "Q", "Temperature", "Phosphorus", "Forests", "15. Life on land", "01 natural sciences", "Article", "Carbon", "Climate Science", "Carbon Cycle", "Trees", "Plant Leaves", "03 medical and health sciences", "13. Climate action", "Animals", "Herbivory", "14. Life underwater", "Ecosystem", "Klimatvetenskap"]}, "links": [{"href": "https://doi.org/10.1038/s41467-024-50245-9"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Nature%20Communications", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1038/s41467-024-50245-9", "name": "item", "description": "10.1038/s41467-024-50245-9", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1038/s41467-024-50245-9"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2024-07-17T00:00:00Z"}}, {"id": "10.1038/s41467-024-52160-5", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:18:23Z", "type": "Journal Article", "created": "2024-09-13", "title": "Emerging multiscale insights on microbial carbon use efficiency in the land carbon cycle", "description": "Abstract<p>Microbial carbon use efficiency (CUE) affects the fate and storage of carbon in terrestrial ecosystems, but its global importance remains uncertain. Accurately modeling and predicting CUE on a global scale is challenging due to inconsistencies in measurement techniques and the complex interactions of climatic, edaphic, and biological factors across scales. The link between microbial CUE and soil organic carbon relies on the stabilization of microbial necromass within soil aggregates or its association with minerals, necessitating an integration of microbial and stabilization processes in modeling approaches. In this perspective, we propose a comprehensive framework that integrates diverse data sources, ranging from genomic information to traditional soil carbon assessments, to refine carbon cycle models by incorporating variations in CUE, thereby enhancing our understanding of the microbial contribution to carbon cycling.</p", "keywords": ["580", "570", "[SDU.OCEAN]Sciences of the Universe [physics]/Ocean", "Agricultural", "550", "Bacteria", "Atmosphere", "Life on Land", "[SDU.OCEAN] Sciences of the Universe [physics]/Ocean", " Atmosphere", "Forestry Sciences", "Science", "Q", "Veterinary and Food Sciences", "Biological Sciences", "[SDU.ENVI] Sciences of the Universe [physics]/Continental interfaces", " environment", "Carbon", "Carbon Cycle", "Soil", "Perspective", "[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces", "environment", "Soil Microbiology", "Ecosystem"]}, "links": [{"href": "https://doi.org/10.1038/s41467-024-52160-5"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Nature%20Communications", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1038/s41467-024-52160-5", "name": "item", "description": "10.1038/s41467-024-52160-5", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1038/s41467-024-52160-5"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2024-09-13T00:00:00Z"}}, {"id": "10.1088/1748-9326/abee4b", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-06-24T16:18:59Z", "type": "Journal Article", "created": "2021-03-12", "title": "Preferential export of permafrost-derived organic matter as retrogressive thaw slumping intensifies", "description": "Abstract                <p>Enhanced warming of the Northern high latitudes has intensified thermokarst processes throughout the permafrost zone. Retrogressive thaw slumps (RTS), where thaw-driven erosion caused by ground ice melt creates terrain disturbances extending over tens of hectares, represent particularly dynamic thermokarst features. Biogeochemical transformation of the mobilized substrate may release CO2 to the atmosphere and impact downstream ecosystems, yet its fate remains unclear. The Peel Plateau in northwestern Canada hosts some of the largest RTS features in the Arctic. Here, thick deposits of Pleistocene-aged glacial tills are overlain by a thinner layer of relatively organic-rich Holocene-aged permafrost that aggraded upward following deeper thaw and soil development during the early Holocene warm period. In this study, we characterize exposed soil layers and the mobilized material by analysing sediment properties and organic matter composition in active layer, Holocene and Pleistocene permafrost, recently thawed debris deposits and fresh deposits of slump outflow from four separate RTS features. We found that organic matter content, radiocarbon age and biomarker concentrations in debris and outflow deposits from all four sites were most similar to permafrost soils, with a lesser influence of the organic-rich active layer. Lipid biomarkers suggested a significant contribution of petrogenic carbon especially in Pleistocene permafrost. Active layer samples contained abundant intrinsically labile macromolecular components (polysaccharides, lignin markers, phenolic and N-containing compounds). All other samples were dominated by degraded organic constituents. Active layer soils, although heterogeneous, also had the highest median grain sizes, whereas debris and runoff deposits consisted of finer mineral grains and were generally more homogeneous, similar to permafrost. We thus infer that both organic matter degradation and hydrodynamic sorting during transport affect the mobilized material. Determining the relative magnitude of these two processes will be crucial to better assess the role of intensifying RTS activity in CO2 release and ecosystem carbon fluxes.</p", "keywords": ["thermokarst", "Science", "Physics", "QC1-999", "Q", "carbon cycle; climate change; cryosphere; thermokarst", "15. Life on land", "Environmental technology. Sanitary engineering", "cryosphere", "01 natural sciences", "Environmental sciences", "climate change", "13. Climate action", "carbon cycle", "GE1-350", "SDG 14 - Life Below Water", "TD1-1066", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/10.1088/1748-9326/abee4b"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Environmental%20Research%20Letters", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1088/1748-9326/abee4b", "name": "item", "description": "10.1088/1748-9326/abee4b", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1088/1748-9326/abee4b"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2021-05-01T00:00:00Z"}}, {"id": "10.1038/s41559-019-1055-3", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:18:24Z", "type": "Journal Article", "created": "2019-12-09", "title": "A systemic overreaction to years versus decades of warming in a subarctic grassland ecosystem", "description": "Temperature governs most biotic processes, yet we know little about how warming affects whole ecosystems. Here we examined the responses of 128\u2009components of a subarctic grassland to either 5-8 or >50\u2009years of soil warming. Warming of >50\u2009years drove the ecosystem to a new steady state possessing a distinct biotic composition and reduced species richness, biomass and soil organic matter. However, the warmed state was preceded by an overreaction to warming, which was related to organism physiology and was evident after 5-8\u2009years. Ignoring this overreaction yielded errors of >100% for 83\u2009variables when predicting their responses to a realistic warming scenario of 1\u2009\u00b0C over 50\u2009years, although some, including soil carbon content, remained stable after 5-8\u2009years. This study challenges long-term ecosystem predictions made from short-term observations, and provides a framework for characterization of ecosystem responses to sustained climate change.", "keywords": ["0301 basic medicine", "570", "Environmental management", "INCREASES", "Ecosystem ecology", "Climate Change", "Evolutionary biology", "TERM", "630", "Article", "Carbon Cycle", "Soil", "03 medical and health sciences", "SDG 13 - Climate Action", "106026 Ecosystem research", "Life Below Water", "Ecosystem", "106022 Mikrobiologie", "0303 health sciences", "Ecology", "Climate-change ecology", "SHIFTS", "Biological Sciences", "15. Life on land", "Grassland", "106026 \u00d6kosystemforschung", "13. Climate action", "SDG 13 \u2013 Ma\u00dfnahmen zum Klimaschutz", "FEEDBACKS", "106022 Microbiology", "VEGETATION", "SENSITIVITY", "Environmental Sciences", "SOIL RESPIRATION", "RESPONSES"]}, "links": [{"href": "https://escholarship.org/content/qt99v0g8pc/qt99v0g8pc.pdf"}, {"href": "https://doi.org/10.1038/s41559-019-1055-3"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Nature%20Ecology%20%26amp%3B%20Evolution", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1038/s41559-019-1055-3", "name": "item", "description": "10.1038/s41559-019-1055-3", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1038/s41559-019-1055-3"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2019-12-09T00:00:00Z"}}, {"id": "10.1038/s41598-018-32229-0", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:18:26Z", "type": "Journal Article", "created": "2018-09-07", "title": "Soil resources and element stocks in drylands to face global issues", "description": "Abstract<p>Drylands (hyperarid, arid, semiarid, and dry subhumid ecosystems) cover almost half of Earth\uffe2\uff80\uff99s land surface and are highly vulnerable to environmental pressures. Here we provide an inventory of soil properties including carbon (C), nitrogen (N), and phosphorus (P) stocks within the current boundaries of drylands, aimed at serving as a benchmark in the face of future challenges including increased population, food security, desertification, and climate change. Aridity limits plant production and results in poorly developed soils, with coarse texture, low C:N and C:P, scarce organic matter, and high vulnerability to erosion. Dryland soils store 646 Pg of organic C to 2\uffe2\uff80\uff89m, the equivalent of 32% of the global soil organic C pool. The magnitude of the historic loss of C from dryland soils due to human land use and cover change and their typically low C:N and C:P suggest high potential to build up soil organic matter, but coarse soil textures may limit protection and stabilization processes. Restoring, preserving, and increasing soil organic matter in drylands may help slow down rising levels of atmospheric carbon dioxide by sequestering C, and is strongly needed to enhance food security and reduce the risk of land degradation and desertification.</p", "keywords": ["0301 basic medicine", "2. Zero hunger", "Conservation of Natural Resources", "0303 health sciences", "Multidisciplinary", "Nitrogen", "Climate", "Climate Change", "Phosphorus", "15. Life on land", "Article", "Carbon", "Food Supply", "Soil", "03 medical and health sciences", "element cycles", "13. Climate action", "carbon cycle", "Life Science", "Humans", "Desert Climate", "Ecosystem", "geochemistry"]}, "links": [{"href": "https://iris.univr.it/bitstream/11562/1001390/1/Soil%20resources%20and%20element%20stocks%20in%20drylands%20to%20face%20global%20issues.pdf"}, {"href": "https://www.nature.com/articles/s41598-018-32229-0.pdf"}, {"href": "https://doi.org/10.1038/s41598-018-32229-0"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Scientific%20Reports", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1038/s41598-018-32229-0", "name": "item", "description": "10.1038/s41598-018-32229-0", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1038/s41598-018-32229-0"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2018-09-13T00:00:00Z"}}, {"id": "10.1038/s41559-024-02501-w", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:18:24Z", "type": "Journal Article", "created": "2024-08-07", "title": "Water limitation regulates positive feedback of increased ecosystem respiration", "description": "Terrestrial ecosystem respiration increases exponentially with temperature, constituting a positive feedback loop accelerating global warming. However, the response of ecosystem respiration to temperature strongly depends on water availability, yet where and when the water effects are important, is presently poorly constrained, introducing uncertainties in climate-carbon cycle feedback projections. Here, we disentangle the effects of temperature and precipitation (a proxy for water availability) on ecosystem respiration by analysing eddy covariance CO2 flux measurements across 212 globally distributed sites. We reveal a threshold precipitation function, determined by the balance between precipitation and ecosystem water demand, which separates temperature-limited and water-limited respiration. Respiration is temperature limited for precipitation above that threshold function, whereas in drier areas water limitation reduces the temperature sensitivity of respiration and its positive feedback to global warming. If the trend of expansion of water-limited areas with warming climate over the last decades continues, the positive feedback of ecosystem respiration is likely to be weakened and counteracted by the increasing water limitation.", "keywords": ["0301 basic medicine", "0303 health sciences", "Naturgeografi", "Climate Change", "Rain", "Temperature", "Water", "Carbon Dioxide", "15. Life on land", "Global Warming", "6. Clean water", "Carbon Cycle", "03 medical and health sciences", "Physical Geography", "13. Climate action", "SDG 13 - Climate Action", "Ecosystem", "SDG 15 - Life on Land"]}, "links": [{"href": "https://doi.org/10.1038/s41559-024-02501-w"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Nature%20Ecology%20%26amp%3B%20Evolution", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1038/s41559-024-02501-w", "name": "item", "description": "10.1038/s41559-024-02501-w", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1038/s41559-024-02501-w"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2024-08-07T00:00:00Z"}}, {"id": "10.1038/s41561-019-0318-6", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:18:24Z", "type": "Journal Article", "created": "2019-03-11", "title": "Drought impacts on terrestrial primary production underestimated by satellite monitoring", "description": "Satellite retrievals of information about the Earth's surface are widely used to monitor global terrestrial photosynthesis and primary production and to examine the ecological impacts of droughts. Methods for estimating photosynthesis from space commonly combine information on vegetation greenness, incoming radiation, temperature and atmospheric demand for water (vapour-pressure deficit), but do not account for the direct effects of low soil moisture. They instead rely on vapour-pressure deficit as a proxy for dryness, despite widespread evidence that soil moisture deficits have a direct impact on vegetation, independent of vapour-pressure deficit. Here, we use a globally distributed measurement network to assess the effect of soil moisture on photosynthesis, and identify a common bias in an ensemble of satellite-based estimates of photosynthesis that is governed by the magnitude of soil moisture effects on photosynthetic light-use efficiency. We develop methods to account for the influence of soil moisture and estimate that soil moisture effects reduce global annual photosynthesis by ~15%, increase interannual variability by more than 100% across 25% of the global vegetated land surface, and amplify the impacts of extreme events on primary production. These results demonstrate the importance of soil moisture effects for monitoring carbon-cycle variability and drought impacts on vegetation productivity from space.", "keywords": ["550", "0207 environmental engineering", "02 engineering and technology", "01 natural sciences", "Physical Geography and Environmental Geoscience", "USE EFFICIENCY", "NET PRIMARY PRODUCTION", "Meteorology & Atmospheric Sciences", "Geosciences", " Multidisciplinary", "WATER-STRESS", "Physical geography and environmental geoscience", "0105 earth and related environmental sciences", "2. Zero hunger", "Multidisciplinary", "Science & Technology", "CLIMATE-CHANGE", "Ecology", "PHOTOSYNTHESIS", "Geology", "GROSS PRIMARY PRODUCTION", "Carbon cycle", "Biogeochemistry", "15. Life on land", "FOREST", "6. Clean water", "ATMOSPHERIC DEMAND", "13. Climate action", "Physical Sciences", "Earth Sciences", "RADIATION", "CARBON UPTAKE", "Geosciences"]}, "links": [{"href": "http://www.nature.com/articles/s41561-019-0318-6.pdf"}, {"href": "https://escholarship.org/content/qt2hr7r7gk/qt2hr7r7gk.pdf"}, {"href": "https://doi.org/10.1038/s41561-019-0318-6"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Nature%20Geoscience", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1038/s41561-019-0318-6", "name": "item", "description": "10.1038/s41561-019-0318-6", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1038/s41561-019-0318-6"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2019-03-11T00:00:00Z"}}, {"id": "10.1038/s41586-021-03629-6", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-06-24T16:18:25Z", "type": "Journal Article", "created": "2021-07-14", "title": "Amazonia as a carbon source linked to deforestation and climate change", "description": "Amazonia hosts the Earth's largest tropical forests and has been shown to be an important carbon sink over recent decades1-3. This carbon sink seems to be in decline, however, as a result of factors such as deforestation and climate change1-3. Here we investigate Amazonia's carbon budget and the main drivers responsible for its change into a carbon source. We performed 590 aircraft vertical profiling measurements of lower-tropospheric concentrations of carbon dioxide and carbon monoxide at four sites in Amazonia from 2010 to 20184. We find that total carbon emissions are greater in eastern Amazonia than in the western part, mostly as a result of spatial differences in carbon-monoxide-derived fire emissions. Southeastern Amazonia, in particular, acts as a net carbon source (total carbon flux minus fire emissions) to the atmosphere. Over the past 40 years, eastern Amazonia has been subjected to more deforestation, warming and moisture stress than the western part, especially during the dry season, with the southeast experiencing the strongest trends5-9. We explore the effect of climate change and deforestation trends on carbon emissions at our study sites, and find that the intensification of the dry season and an increase in deforestation seem to promote ecosystem stress, increase in fire occurrence, and higher carbon emissions in the eastern Amazon. This is in line with recent studies that indicate an increase in tree mortality and a reduction in photosynthesis as a result of climatic changes across Amazonia1,10.", "keywords": ["0301 basic medicine", "Carbon Monoxide", "Carbon Sequestration", "Conservation of Natural Resources", "Atmosphere", "Climate Change", "Rain", "Temperature", "Carbon Dioxide", "Forests", "15. Life on land", "01 natural sciences", "Carbon Cycle", "03 medical and health sciences", "13. Climate action", "11. Sustainability", "Life Science", "Human Activities", "Seasons", "Photosynthesis", "0105 earth and related environmental sciences"]}, "links": [{"href": "http://www.nature.com/articles/s41586-021-03629-6.pdf"}, {"href": "https://doi.org/10.1038/s41586-021-03629-6"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Nature", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1038/s41586-021-03629-6", "name": "item", "description": "10.1038/s41586-021-03629-6", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1038/s41586-021-03629-6"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2021-07-14T00:00:00Z"}}, {"id": "10.1038/s41598-019-43305-4", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:18:26Z", "type": "Journal Article", "created": "2019-05-03", "title": "Soil amendments with ethylene precursor alleviate negative impacts of salinity on soil microbial properties and productivity", "description": "Abstract<p>Some microbes enhance stress tolerance in plants by minimizing plant ethylene levels via degradation of its immediate precursor, 1-aminocyclopropane-1-carboxylate (ACC), in the rhizosphere. In return, ACC is used by these microbes as a source of nitrogen. This mutualistic relationship between plants and microbes may be used to promote soil properties in stressful environments. In this study, we tested the hypothesis that amendments of ACC in soils reshape the structure of soil microbiome and alleviate the negative impacts of salinity on soil properties. We treated non-saline and artificially-developed saline soils with ACC in different concentrations for 14 days. The structure of soil microbiome, soil microbial properties and productivity were examined. Our results revealed that microbial composition of bacteria, archaea and fungi in saline soils was affected by ACC amendments; whereas community composition in non-saline soils was not affected. The amendments of ACC could not fully counteract the negative effects of salinity on soil microbial activities and productivity, but increased the abundance of ACC deaminase-encoding gene (acdS), enhanced soil microbial respiration, enzymatic activity, nitrogen and carbon cycling potentials and Arabidopsis biomass in saline soils. Collectively, our study indicates that ACC amendments in soils could efficiently ameliorate salinity impacts on soil properties and plant biomass production.</p", "keywords": ["0301 basic medicine", "2. Zero hunger", "570", "Salinity", "0303 health sciences", "Multidisciplinary", "soil salinization", "Fungi", "Amino Acids", " Cyclic", "Nitrogen Cycle", "15. Life on land", "630", "Article", "Carbon Cycle", "Actinobacteria", "Soil", "03 medical and health sciences", "13. Climate action", "1000 General", "XXXXXX - Unknown", "ethylene", "Carbon-Carbon Lyases", "bacteria", "soils", "Soil Microbiology"]}, "links": [{"href": "https://doi.org/10.1038/s41598-019-43305-4"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Scientific%20Reports", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1038/s41598-019-43305-4", "name": "item", "description": "10.1038/s41598-019-43305-4", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1038/s41598-019-43305-4"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2019-05-03T00:00:00Z"}}, {"id": "10.1038/s42949-024-00154-z", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:18:27Z", "type": "Journal Article", "created": "2024-03-16", "title": "Urban greenspaces and nearby natural areas support similar levels of soil ecosystem services", "description": "Abstract<p>Greenspaces are important for sustaining healthy urban environments and their human populations. Yet their capacity to support multiple ecosystem services simultaneously (multiservices) compared with nearby natural ecosystems remains virtually unknown. We conducted a global field survey in 56 urban areas to investigate the influence of urban greenspaces on 23 soil and plant attributes and compared them with nearby natural environments. We show that, in general, urban greenspaces and nearby natural areas support similar levels of soil multiservices, with only six of 23 attributes (available phosphorus, water holding capacity, water respiration, plant cover, arbuscular mycorrhizal fungi (AMF), and arachnid richness) significantly greater in greenspaces, and one (available ammonium) greater in natural areas. Further analyses showed that, although natural areas and urban greenspaces delivered a similar number of services at low (&gt;25% threshold) and moderate (&gt;50%) levels of functioning, natural systems supported significantly more functions at high (&gt;75%) levels of functioning. Management practices (mowing) played an important role in explaining urban ecosystem services, but there were no effects of fertilisation or irrigation. Some services declined with increasing site size, for both greenspaces and natural areas. Our work highlights the fact that urban greenspaces are more similar to natural environments than previously reported and underscores the importance of managing urban greenspaces not only for their social and recreational values, but for supporting multiple ecosystem services on which soils and human well-being depends.</p", "keywords": ["Medio ambiente natural", "2410.05 Ecolog\u00eda Humana", "Health", " Toxicology and Mutagenesis", "0211 other engineering and technologies", "710", "Urban Green Space", "02 engineering and technology", "01 natural sciences", "zelene povr\u0161ine", "ekosistemske storitve", " zelene povr\u0161ine", " urbani gozdovi", " tla", "Urban planning", "Natural (archaeology)", "11. Sustainability", "Urban Heat Islands and Mitigation Strategies", "info:eu-repo/classification/udc/630*1:630*9", "2. Zero hunger", "Global and Planetary Change", "Global Analysis of Ecosystem Services and Land Use", "Geography", "Ecology", "2417.13 Ecolog\u00eda Vegetal", "Carbon cycle", "3. Good health", "soil", " ecosystem services", " urban forests", "2511 Ciencias del Suelo (Edafolog\u00eda)", "Archaeology", "Physical Sciences", "urban forests", "HT361-384", "Ecolog\u00eda (Biolog\u00eda)", "Urbanization. City and country", "Environmental Engineering", "711.4:911.375", "631.4", "Environmental science", "soil", "12. Responsible consumption", "Impact of Urban Green Space on Public Health", "Urban ecosystem", "XXXXXX - Unknown", "Ecosystem services", "14. Life underwater", "Agroforestry", "info:eu-repo/classification/udc/630*1", "Biology", "City planning", "Ecosystem", "0105 earth and related environmental sciences", "SDG-15: Life on land", "tla", "FOS: Environmental engineering", "15. Life on land", "ekosistemske storitve", "Urban ecology", "HT165.5-169.9", "13. Climate action", "FOS: Biological sciences", "Environmental Science", "urbani gozdovi", "502.3", "ecosystem services"]}, "links": [{"href": "https://www.nature.com/articles/s42949-024-00154-z.pdf"}, {"href": "https://doi.org/10.1038/s42949-024-00154-z"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/npj%20Urban%20Sustainability", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1038/s42949-024-00154-z", "name": "item", "description": "10.1038/s42949-024-00154-z", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1038/s42949-024-00154-z"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2024-03-16T00:00:00Z"}}, {"id": "10.1038/s43247-021-00192-w", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:18:28Z", "type": "Journal Article", "created": "2021-06-10", "title": "Carbon dioxide fluxes increase from day to night across European streams", "description": "Abstract<p>Globally, inland waters emit over 2 Pg of carbon per year as carbon dioxide, of which the majority originates from streams and rivers. Despite the global significance of fluvial carbon dioxide emissions, little is known about their diel dynamics. Here we present a large-scale assessment of day- and night-time carbon dioxide fluxes at the water-air interface across 34 European streams. We directly measured fluxes four times between October 2016 and July 2017 using drifting chambers. Median fluxes are 1.4 and 2.1\uffe2\uff80\uff89mmol\uffe2\uff80\uff89m\uffe2\uff88\uff922 h\uffe2\uff88\uff921 at midday and midnight, respectively, with night fluxes exceeding those during the day by 39%. We attribute diel carbon dioxide flux variability mainly to changes in the water partial pressure of carbon dioxide. However, no consistent drivers could be identified across sites. Our findings highlight widespread day-night changes in fluvial carbon dioxide fluxes and suggest that the time of day greatly influences measured carbon dioxide fluxes across European streams.</p", "keywords": ["DYNAMICS", "0106 biological sciences", "DIURNAL-VARIATION", "550", "Naturgeografi", "PCO(2)", "Geography & travel", "Oceanografi", " hydrologi och vattenresurser", "910", "01 natural sciences", "Oceanography", " Hydrology and Water Resources", "105205 Klimawandel", "Limnology", "105304 Hydrologie", "SDG 13 - Climate Action", "info:eu-repo/classification/ddc/910", "106026 Ecosystem research", "1ST-ORDER STREAM", "106020 Limnology", "105205 Climate change", "0105 earth and related environmental sciences", "[SDU.OCEAN]Sciences of the Universe [physics]/Ocean", "Atmosphere", "[SDU.OCEAN] Sciences of the Universe [physics]/Ocean", " Atmosphere", "EVASION", "Carbon cycle", "ddc:910", "106020 Limnologie", "Climate Science", "ECOSYSTEM METABOLISM", "WATER-AIR", "Physical Geography", "106026 \u00d6kosystemforschung", "CO2 EMISSIONS", "13. Climate action", "SDG 13 \u2013 Ma\u00dfnahmen zum Klimaschutz", "Environmental chemistry", "DISSOLVED ORGANIC-MATTER", "Klimatvetenskap", "105304 Hydrology", "GAS-EXCHANGE"]}, "links": [{"href": "https://eprints.bournemouth.ac.uk/35763/1/s43247-021-00192-w.pdf"}, {"href": "https://iris.unito.it/bitstream/2318/1799544/1/106%20EURORUN.pdf"}, {"href": "https://www.nature.com/articles/s43247-021-00192-w.pdf"}, {"href": "https://doi.org/10.1038/s43247-021-00192-w"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Communications%20Earth%20%26amp%3B%20Environment", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1038/s43247-021-00192-w", "name": "item", "description": "10.1038/s43247-021-00192-w", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1038/s43247-021-00192-w"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2021-03-22T00:00:00Z"}}, {"id": "10.1038/s43247-022-00523-5", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:18:28Z", "type": "Journal Article", "created": "2022-08-18", "title": "Ecoenzymatic stoichiometry reveals widespread soil phosphorus limitation to microbial metabolism across Chinese forests", "description": "Abstract<p>Forest soils contain a large amount of organic carbon and contribute to terrestrial carbon sequestration. However, we still have a poor understanding of what nutrients limit soil microbial metabolism that drives soil carbon release across the range of boreal to tropical forests. Here we used ecoenzymatic stoichiometry methods to investigate the patterns of microbial nutrient limitations within soil profiles (organic, eluvial and parent material horizons) across 181 forest sites throughout China. Results show that, in 80% of these forests, soil microbes were limited by phosphorus availability. Microbial phosphorus limitation increased with soil depth and from boreal to tropical forests as ecosystems become wetter, warmer, more productive, and is affected by anthropogenic nitrogen deposition. We also observed an unexpected shift in the latitudinal pattern of microbial phosphorus limitation with the lowest phosphorus limitation in the warm temperate zone (41-42\uffc2\uffb0N). Our study highlights the importance of soil phosphorus limitation to restoring forests and predicting their carbon sinks.</p", "keywords": ["0301 basic medicine", "Biogeochemical Cycling of Nutrients in Aquatic Ecosystems", "Nitrogen", "Soil Science", "Organic chemistry", "Carbon Dynamics in Peatland Ecosystems", "Nitrogen cycle", "Environmental science", "Nutrient cycle", "Agricultural and Biological Sciences", "03 medical and health sciences", "Terrestrial ecosystem", "XXXXXX - Unknown", "Taiga", "Soil water", "Environmental Chemistry", "GE1-350", "Biology", "Ecosystem", "Soil science", "2. Zero hunger", "QE1-996.5", "Soil organic matter", "Ecology", "Life Sciences", "Geology", "Phosphorus", "Carbon cycle", "04 agricultural and veterinary sciences", "15. Life on land", "Soil carbon", "Environmental sciences", "Temperate climate", "Chemistry", "13. Climate action", "FOS: Biological sciences", "Environmental Science", "Physical Sciences", "0401 agriculture", " forestry", " and fisheries", "Soil Carbon Dynamics and Nutrient Cycling in Ecosystems", "Ecosystem Functioning", "Nutrient"]}, "links": [{"href": "https://doi.org/10.1038/s43247-022-00523-5"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Communications%20Earth%20%26amp%3B%20Environment", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1038/s43247-022-00523-5", "name": "item", "description": "10.1038/s43247-022-00523-5", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1038/s43247-022-00523-5"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2022-08-18T00:00:00Z"}}, {"id": "10.1046/j.1365-2486.2001.00388.x", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:18:33Z", "type": "Journal Article", "created": "2003-03-11", "title": "Chemistry And Decomposition Of Litter From Populus Tremuloides Michaux Grown At Elevated Atmospheric Co2 And Varying N Availability", "description": "Summary<p>It has been hypothesized that greater production of total nonstructural carbohydrates (TNC) in foliage grown under elevated atmospheric carbon dioxide (CO2) will result in higher concentrations of defensive compounds in tree leaf litter, possibly leading to reduced rates of decomposition and nutrient cycling in forest ecosystems of the future. To evaluate the effects of elevated atmospheric CO2on litter chemistry and decomposition, we performed a 111 day laboratory incubation with leaf litter of trembling aspen (Populus tremuloidesMichaux) produced at 36\uffe2\uff80\uff83Pa and 56\uffe2\uff80\uff83Pa CO2and two levels of soil nitrogen (N) availability. Decomposition was quantified as microbially respired CO2and dissolved organic carbon (DOC) in soil solution, and concentrations of nonstructural carbohydrates, N, carbon (C), and condensed tannins were monitored throughout the incubation. Growth under elevated atmospheric CO2did not significantly affect initial litter concentrations of TNC, N, or condensed tannins. Rates of decomposition, measured as both microbially respired CO2and DOC did not differ between litter produced under ambient and elevated CO2. Total C lost from the samples was 38\uffe2\uff80\uff83mg\uffe2\uff80\uff83g\uffe2\uff88\uff921litter as respired CO2and 138\uffe2\uff80\uff83mg\uffe2\uff80\uff83g\uffe2\uff88\uff921litter as DOC, suggesting short\uffe2\uff80\uff90term pulses of dissolved C in soil solution are important components of the terrestrial C cycle. We conclude that litter chemistry and decomposition in trembling aspen are minimally affected by growth under higher concentrations of CO2.</p>", "keywords": ["Ecology and Evolutionary Biology", "carbohydrates", "Quaking aspen", "forest-soil", "litter-plant", "nitrogen", "nitrogen-", "Microlysimeter", "soil-chemistry", "cycling-", "populus-tremuloides", "Geology and Earth Sciences", "Soil Carbon", "Microbiology of soils", "Carbon cycle", "04 agricultural and veterinary sciences", "GLOBAL-ECOLOGY", "chemical-composition", "Organic-matter", "soil-solution", "nutrient-availability", "Tannin", "leaf-litter", "Science", "decomposition-", "Nutrient enrichment", "Carbohydrates", "carbohydrates-", "respiration-", "carbon-dioxide-enrichment", "Nitrogen in soil", "michigan-", "carbon sinks", "C", "Nutrient budget of forests", "Litter", "Populus tremuloides", "Global Change", "tannins-", "Decomposition", "forest-litter", "Foliage", "Carbon dioxide effects on forest litter", "Climatic changes", "15. Life on land", "carbon-nitrogen-ratio", "Forest litter decomposition", "N Ratio", "13. Climate action", "0401 agriculture", " forestry", " and fisheries", "microbial-activities", "nitrogen-content"]}, "links": [{"href": "https://doi.org/10.1046/j.1365-2486.2001.00388.x"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Global%20Change%20Biology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1046/j.1365-2486.2001.00388.x", "name": "item", "description": "10.1046/j.1365-2486.2001.00388.x", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1046/j.1365-2486.2001.00388.x"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2001-01-01T00:00:00Z"}}, {"id": "10.1038/srep08280", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:18:28Z", "type": "Journal Article", "created": "2015-02-06", "title": "Convergence Of Soil Nitrogen Isotopes Across Global Climate Gradients", "description": "Abstract<p>Quantifying global patterns of terrestrial nitrogen (N) cycling is central to predicting future patterns of primary productivity, carbon sequestration, nutrient fluxes to aquatic systems and climate forcing. With limited direct measures of soil N cycling at the global scale, syntheses of the 15N:14N ratio of soil organic matter across climate gradients provide key insights into understanding global patterns of N cycling. In synthesizing data from over 6000 soil samples, we show strong global relationships among soil N isotopes, mean annual temperature (MAT), mean annual precipitation (MAP) and the concentrations of organic carbon and clay in soil. In both hot ecosystems and dry ecosystems, soil organic matter was more enriched in 15N than in corresponding cold ecosystems or wet ecosystems. Below a MAT of 9.8\uffc2\uffb0C, soil \uffce\uffb415N was invariant with MAT. At the global scale, soil organic C concentrations also declined with increasing MAT and decreasing MAP. After standardizing for variation among mineral soils in soil C and clay concentrations, soil \uffce\uffb415N showed no consistent trends across global climate and latitudinal gradients. Our analyses could place new constraints on interpretations of patterns of ecosystem N cycling and global budgets of gaseous N loss.</p>", "keywords": ["N-15 Natural-Abundance", "550", "Ecosystem ecology", "TROPICAL FORESTS", "Organic chemistry", "Suelo", "Nitrogen cycle", "01 natural sciences", "Nutrient cycle", "cycle de l'azote", "CARBON", "Agricultural and Biological Sciences", "Soil", "Terrestrial ecosystem", "Isotopes", "https://purl.org/becyt/ford/1.6", "Soil water", "SDG 13 - Climate Action", "N-15 NATURAL-ABUNDANCE", "Climate change", "croisement de donn\u00e9es", "Milieux et Changements globaux", "SDG 15 \u2013 Leben an Land", "Global change", "SDG 15 - Life on Land", "2. Zero hunger", "106022 Mikrobiologie", "Climatic Factors", "Tropical Forests", "Ecology", "Geography", "Nitr\u00f3geno", "Nutrient Cycling", "FRACTIONATION", "Litter Decomposition", "ECOSYSTEM ECOLOGY", "Life Sciences", "ecosystem ecology", "Cycling", "Forestry", "Is\u00f3topos", "Carbon cycle", "04 agricultural and veterinary sciences", "Nitrogen Cycle", "Soil carbon", "6. Clean water", "Organic-Matter", "Earth and Planetary Sciences", "ORGANIC-MATTER", "Chemistry", "PRECIPITATION", "SDG 13 \u2013 Ma\u00dfnahmen zum Klimaschutz", "Physical Sciences", "106022 Microbiology", "carbone du sol", "Stable Isotope Analysis of Groundwater and Precipitation", "Ecosystem Functioning", "570", "STABLE ISOTOPE", "Biogeochemical Cycling of Nutrients in Aquatic Ecosystems", "Stable isotope analysis", "Nitrogen", "[SDE.MCG]Environmental Sciences/Global Changes", "Soil Science", "stable isotope analysis;ecosystem ecology", "Article", "Environmental science", "LITTER DECOMPOSITION", "sol min\u00e9ral", "INORGANIC NITROGEN", "Geochemistry and Petrology", "stable isotope analysis", "Carbono", "Environmental Chemistry", "Factores Clim\u00e1ticos", "https://purl.org/becyt/ford/1", "Biology", "Ecosystem", "0105 earth and related environmental sciences", "Soil science", "Soil organic matter", "Soil Fertility", "climat", "AVAILABILITY", "Nitrogen Dynamics", "15. Life on land", "Carbon", "Inorganic", "NITROGEN", "MODEL", "[SDE.MCG] Environmental Sciences/Global Changes", "13. Climate action", "FOS: Biological sciences", "Environmental Science", "PATTERNS", "0401 agriculture", " forestry", " and fisheries", "Soil Carbon Dynamics and Nutrient Cycling in Ecosystems"]}, "links": [{"href": "https://scholars.unh.edu/context/faculty_pubs/article/1042/viewcontent/srep08280.pdf"}, {"href": "https://edoc.unibas.ch/37215/1/srep08280.pdf"}, {"href": "https://doi.org/10.1038/srep08280"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Scientific%20Reports", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1038/srep08280", "name": "item", "description": "10.1038/srep08280", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1038/srep08280"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2015-02-06T00:00:00Z"}}, {"id": "10.1038/srep14378", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-06-24T16:18:28Z", "type": "Journal Article", "created": "2015-09-23", "title": "Effects Of Nitrogen And Phosphorus Additions On Soil Microbial Biomass And Community Structure In Two Reforested Tropical Forests", "description": "Abstract<p>Elevated nitrogen (N) deposition may aggravate phosphorus (P) deficiency in forests in the warm humid regions of China. To our knowledge, the interactive effects of long-term N deposition and P availability on soil microorganisms in tropical replanted forests remain unclear. We conducted an N and P manipulation experiment with four treatments: control, N addition (15\uffe2\uff80\uff89g N m\uffe2\uff88\uff922\uffc2\uffb7yr\uffe2\uff88\uff921), P addition (15\uffe2\uff80\uff89g P m\uffe2\uff88\uff922\uffc2\uffb7yr\uffe2\uff88\uff921) and N and P addition (15\uffe2\uff80\uff89+\uffe2\uff80\uff8915\uffe2\uff80\uff89g N and P m\uffe2\uff88\uff922\uffc2\uffb7yr\uffe2\uff88\uff921, respectively) in disturbed (planted pine forest with recent harvests of understory vegetation and litter) and rehabilitated (planted with pine, but mixed with broadleaf returning by natural succession) forests in southern China. Nitrogen addition did not significantly affect soil microbial biomass, but significantly decreased the abundance of gram-negative bacteria PLFAs in both forest types. Microbial biomass increased significantly after P addition in the disturbed forest but not in the rehabilitated forest. No interactions between N and P additions on soil microorganisms were observed in either forest type. Our results suggest that microbial growth in replanted forests of southern China may be limited by P rather than by N and this P limitation may be greater in disturbed forests.</p>", "keywords": ["China", "Principal Component Analysis", "Nitrates", "Rainforest", "Nitrogen", "Microbiota", "Fatty Acids", "Forestry", "Phosphorus", "04 agricultural and veterinary sciences", "15. Life on land", "Gram-Positive Bacteria", "Article", "Carbon Cycle", "Phosphates", "Multidisciplinary Sciences", "Soil", "Gram-Negative Bacteria", "0401 agriculture", " forestry", " and fisheries", "Biomass", "Fertilizers", "Ecosystem", "Soil Microbiology"]}, "links": [{"href": "https://doi.org/10.1038/srep14378"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Scientific%20Reports", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1038/srep14378", "name": "item", "description": "10.1038/srep14378", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1038/srep14378"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2015-09-23T00:00:00Z"}}, {"id": "10.1038/srep15949", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:18:28Z", "type": "Journal Article", "created": "2015-10-30", "title": "Light-Intensity Grazing Improves Alpine Meadow Productivity And Adaption To Climate Change On The Tibetan Plateau", "description": "Abstract<p>To explore grazing effects on carbon fluxes in alpine meadow ecosystems, we used a paired eddy-covariance (EC) system to measure carbon fluxes in adjacent fenced (FM) and grazed (GM) meadows on the Tibetan plateau. Gross primary productivity (GPP) and ecosystem respiration (Re) were greater at GM than FM for the first two years of fencing. In the third year, the productivity at FM increased to a level similar to the GM site. The higher productivity at GM was mainly caused by its higher photosynthetic capacity. Grazing exclusion did not increase carbon sequestration capacity for this alpine grassland system. The higher optimal photosynthetic temperature and the weakened ecosystem response to climatic factors at GM may help to facilitate the adaption of alpine meadow ecosystems to changing climate.</p>", "keywords": ["2. Zero hunger", "Climate Change", "Temperature", "04 agricultural and veterinary sciences", "15. Life on land", "Tibet", "16. Peace & justice", "Grassland", "01 natural sciences", "Article", "Carbon Cycle", "Soil", "13. Climate action", "0401 agriculture", " forestry", " and fisheries", "Photosynthesis", "Ecosystem", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/10.1038/srep15949"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Scientific%20Reports", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1038/srep15949", "name": "item", "description": "10.1038/srep15949", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1038/srep15949"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2015-10-30T00:00:00Z"}}, {"id": "10.1038/srep15991", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:18:28Z", "type": "Journal Article", "created": "2015-11-04", "title": "Forest soil carbon is threatened by intensive biomass harvesting", "description": "Abstract<p>Forests play a key role in the carbon cycle as they store huge quantities of organic carbon, most of which is stored in soils, with a smaller part being held in vegetation. While the carbon storage capacity of forests is influenced by forestry, the long-term impacts of forest managers\uffe2\uff80\uff99 decisions on soil organic carbon (SOC) remain unclear. Using a meta-analysis approach, we showed that conventional biomass harvests preserved the SOC of forests, unlike intensive harvests where logging residues were harvested to produce fuelwood. Conventional harvests caused a decrease in carbon storage in the forest floor, but when the whole soil profile was taken into account, we found that this loss in the forest floor was compensated by an accumulation of SOC in deeper soil layers. Conversely, we found that intensive harvests led to SOC losses in all layers of forest soils. We assessed the potential impact of intensive harvests on the carbon budget, focusing on managed European forests. Estimated carbon losses from forest soils suggested that intensive biomass harvests could constitute an important source of carbon transfer from forests to the atmosphere (142\uffe2\uff80\uff93497 Tg-C), partly neutralizing the role of a carbon sink played by forest soils.</p>", "keywords": ["2. Zero hunger", "0106 biological sciences", "Carbon Sequestration", "[SDE.MCG]Environmental Sciences/Global Changes", "Forestry", "04 agricultural and veterinary sciences", "Forests", "15. Life on land", "forest soil", "01 natural sciences", "Article", "Carbon", "Carbon Cycle", "Trees", "[SDE.MCG] Environmental Sciences/Global Changes", "Soil", "13. Climate action", "carbone organique du sol", "0401 agriculture", " forestry", " and fisheries", "Biomass", "Milieux et Changements globaux", "sol forestier", "Ecosystem", "Environmental Monitoring"]}, "links": [{"href": "https://hal.science/hal-01594440/file/2015_Achat_Scientific%20Reports_1.pdf"}, {"href": "https://doi.org/10.1038/srep15991"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Scientific%20Reports", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1038/srep15991", "name": "item", "description": "10.1038/srep15991", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1038/srep15991"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2015-11-04T00:00:00Z"}}, {"id": "10.1038/srep19536", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:18:29Z", "type": "Journal Article", "created": "2016-01-14", "title": "Soil Microbial Responses To Forest Floor Litter Manipulation And Nitrogen Addition In A Mixed-Wood Forest Of Northern China", "description": "Abstract<p>Changes in litterfall dynamics and soil properties due to anthropogenic or natural perturbations have important implications to soil carbon (C) and nutrient cycling via microbial pathway. Here we determine soil microbial responses to contrasting types of litter inputs (leaf vs. fine woody litter) and nitrogen (N) deposition by conducting a multi-year litter manipulation and N addition experiment in a mixed-wood forest. We found significantly higher soil organic C, total N, microbial biomass C (MBC) and N (MBN), microbial activity (MR) and activities of four soil extracellular enzymes, including \uffce\uffb2-glucosidase (BG), N-acetyl-\uffce\uffb2-glucosaminidase (NAG), phenol oxidase (PO) and peroxidase (PER), as well as greater total bacteria biomass and relative abundance of gram-negative bacteria (G-) community, in top soils of plots with presence of leaf litter than of those without litter or with presence of only fine woody litter. No apparent additive or interactive effects of N addition were observed in this study. The occurrence of more labile leaf litter stimulated G-, which may facilitate microbial community growth and soil C stabilization as inferred by findings in literature. A continued treatment with contrasting types of litter inputs is likely to result in divergence in soil microbial community structure and function.</p>", "keywords": ["Biomass (ecology)", "China", "Biogeochemical Cycling of Nutrients in Aquatic Ecosystems", "Microbial population biology", "Nitrogen", "Soil Science", "Organic chemistry", "Forests", "Nitrogen cycle", "Article", "Plant litter", "Nutrient cycle", "Environmental science", "Microbial Ecology", "Agricultural and Biological Sciences", "Soil", "Soil biology", "Litter", "Soil water", "Genetics", "Environmental Chemistry", "Biomass", "Forest floor", "Biology", "Soil Microbiology", "Ecosystem", "2. Zero hunger", "Ecology", "Bacteria", "Marine Microbial Diversity and Biogeography", "Life Sciences", "04 agricultural and veterinary sciences", "15. Life on land", "Wood", "Soil carbon", "Carbon", "Agronomy", "6. Clean water", "3. Good health", "Chemistry", "FOS: Biological sciences", "Environmental Science", "Physical Sciences", "0401 agriculture", " forestry", " and fisheries", "Soil Carbon Dynamics and Nutrient Cycling in Ecosystems", "Nutrient"]}, "links": [{"href": "https://doi.org/10.1038/srep19536"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Scientific%20Reports", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1038/srep19536", "name": "item", "description": "10.1038/srep19536", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1038/srep19536"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2016-01-14T00:00:00Z"}}, {"id": "10.1038/srep33190", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:18:29Z", "type": "Journal Article", "created": "2016-09-12", "title": "Grazing improves C and N cycling in the Northern Great Plains: a meta-analysis", "description": "Abstract<p>Grazing potentially alters grassland ecosystem carbon (C) and nitrogen (N) storage and cycles, however, the overall direction and magnitude of such alterations are poorly understood on the Northern Great Plains (NGP). By synthesizing data from multiple studies on grazed NGP ecosystems, we quantified the response of 30 variables to C and N pools and fluxes to grazing using a comprehensive meta-analysis method. Results showed that grazing enhanced soil C (5.2\uffe2\uff80\uff89\uffc2\uffb1\uffe2\uff80\uff894.6% relative) and N (11.3\uffe2\uff80\uff89\uffc2\uffb1\uffe2\uff80\uff899.1%) pools in the top layer, stimulated litter decomposition (26.8\uffe2\uff80\uff89\uffc2\uffb1\uffe2\uff80\uff8918.4%) and soil N mineralization (22.3\uffe2\uff80\uff89\uffc2\uffb1\uffe2\uff80\uff8918.4%) and enhanced soil NH4+(51.5\uffe2\uff80\uff89\uffc2\uffb1\uffe2\uff80\uff8942.9%) and NO3\uffe2\uff88\uff92(47.5\uffe2\uff80\uff89\uffc2\uffb1\uffe2\uff80\uff8920.7%) concentrations. Our results indicate that the NGP grasslands have sequestered C and N in the past 70 to 80 years, recovering C and N lost during a period of widespread grassland deterioration that occurred in the first half of the 20thcentury. Sustainable grazing management employed after this deterioration has acted as a critical factor for C and N amelioration of degraded NGP grasslands and about 5.84\uffe2\uff80\uff89Mg C ha\uffe2\uff88\uff921CO2-equivalent of anthropogenic CO2emissions has been offset by these grassland soils.</p>", "keywords": ["0106 biological sciences", "2. Zero hunger", "Conservation of Natural Resources", "Agriculture", "04 agricultural and veterinary sciences", "Nitrogen Cycle", "15. Life on land", "Grassland", "01 natural sciences", "Article", "United States", "Carbon Cycle", "13. Climate action", "Animals", "0401 agriculture", " forestry", " and fisheries", "Herbivory"]}, "links": [{"href": "https://doi.org/10.1038/srep33190"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Scientific%20Reports", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1038/srep33190", "name": "item", "description": "10.1038/srep33190", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1038/srep33190"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2016-09-12T00:00:00Z"}}, {"id": "10.1073/pnas.1811797116", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:18:44Z", "type": "Journal Article", "created": "2019-05-14", "title": "Rivers across the Siberian Arctic unearth the patterns of carbon release from thawing permafrost", "description": "<p>             Climate warming is expected to mobilize northern permafrost and peat organic carbon (PP-C), yet magnitudes and system specifics of even current releases are poorly constrained. While part of the PP-C will degrade at point of thaw to CO             2             and CH             4             to directly amplify global warming, another part will enter the fluvial network, potentially providing a window to observe large-scale PP-C remobilization patterns. Here, we employ a decade-long, high-temporal resolution record of             14             C in dissolved and particulate organic carbon (DOC and POC, respectively) to deconvolute PP-C release in the large drainage basins of rivers across Siberia: Ob, Yenisey, Lena, and Kolyma. The             14             C-constrained estimate of export specifically from PP-C corresponds to only 17 \uffc2\uffb1 8% of total fluvial organic carbon and serves as a benchmark for monitoring changes to fluvial PP-C remobilization in a warming Arctic. Whereas DOC was dominated by recent organic carbon and poorly traced PP-C (12 \uffc2\uffb1 8%), POC carried a much stronger signature of PP-C (63 \uffc2\uffb1 10%) and represents the best window to detect spatial and temporal dynamics of PP-C release. Distinct seasonal patterns suggest that while DOC primarily stems from gradual leaching of surface soils, POC reflects abrupt collapse of deeper deposits. Higher dissolved PP-C export by Ob and Yenisey aligns with discontinuous permafrost that facilitates leaching, whereas higher particulate PP-C export by Lena and Kolyma likely echoes the thermokarst-induced collapse of Pleistocene deposits. Quantitative             14             C-based fingerprinting of fluvial organic carbon thus provides an opportunity to elucidate large-scale dynamics of PP-C remobilization in response to Arctic warming.           </p", "keywords": ["15. Life on land", "01 natural sciences", "6. Clean water", "leaching", "climate change", "13. Climate action", "carbon cycle", "Physical Sciences", "peat", "radiocarbon", "SDG 13 - Climate Action", "SDG 14 - Life Below Water", "14. Life underwater", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://pnas.org/doi/pdf/10.1073/pnas.1811797116"}, {"href": "https://doi.org/10.1073/pnas.1811797116"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Proceedings%20of%20the%20National%20Academy%20of%20Sciences", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1073/pnas.1811797116", "name": "item", "description": "10.1073/pnas.1811797116", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1073/pnas.1811797116"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2019-05-06T00:00:00Z"}}, {"id": "10.1073/pnas.2019672118", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:18:45Z", "type": "Journal Article", "created": "2021-03-01", "title": "Source apportionment of methane escaping the subsea permafrost system in the outer Eurasian Arctic Shelf", "description": "Significance           <p>Extensive release of methane from sediments of the world\uffe2\uff80\uff99s largest continental shelf, the East Siberian Arctic Ocean (ESAO), is one of the few Earth system processes that can cause a net transfer of carbon from land/ocean to the atmosphere and thus amplify global warming on the timescale of this century. An important gap in our current knowledge concerns the contributions of different subsea pools to the observed methane releases. This knowledge is a prerequisite to robust predictions on how these releases will develop in the future. Triple-isotope\uffe2\uff80\uff93based fingerprinting of the origin of the highly elevated ESAO methane levels points to a limited contribution from shallow microbial sources and instead a dominating contribution from a deep thermogenic pool.</p", "keywords": ["Carbon cycle/climate change", "G\u00e9n\u00e9ralit\u00e9s", "15. Life on land", "01 natural sciences", "Isotopes/radiocarbon", "3. Good health", "Subsea permafrost", "Arctic", "13. Climate action", "Physical Sciences", "14. Life underwater", "Methane", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://pnas.org/doi/pdf/10.1073/pnas.2019672118"}, {"href": "https://dipot.ulb.ac.be/dspace/bitstream/2013/321210/1/doi_304854.pdf"}, {"href": "https://doi.org/10.1073/pnas.2019672118"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Proceedings%20of%20the%20National%20Academy%20of%20Sciences", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1073/pnas.2019672118", "name": "item", "description": "10.1073/pnas.2019672118", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1073/pnas.2019672118"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2021-03-01T00:00:00Z"}}, {"id": "10.1073/pnas.2309881120", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:18:45Z", "type": "Journal Article", "created": "2024-01-08", "title": "Extreme drought impacts have been underestimated in grasslands and shrublands globally", "description": "<?xml version='1.0' encoding='UTF-8'?><article><p>Climate change is increasing the frequency and severity of short-term (~1 y) drought events\u2014the most common duration of drought\u2014globally. Yet the impact of this intensification of drought on ecosystem functioning remains poorly resolved. This is due in part to the widely disparate approaches ecologists have employed to study drought, variation in the severity and duration of drought studied, and differences among ecosystems in vegetation, edaphic and climatic attributes that can mediate drought impacts. To overcome these problems and better identify the factors that modulate drought responses, we used a coordinated distributed experiment to quantify the impact of short-term drought on grassland and shrubland ecosystems. With a standardized approach, we imposed ~a single year of drought at 100 sites on six continents. Here we show that loss of a foundational ecosystem function\u2014aboveground net primary production (ANPP)\u2014was 60% greater at sites that experienced statistically extreme drought (1-in-100-y event) vs. those sites where drought was nominal (historically more common) in magnitude (35% vs. 21%, respectively). This reduction in a key carbon cycle process with a single year of extreme drought greatly exceeds previously reported losses for grasslands and shrublands. Our global experiment also revealed high variability in drought response but that relative reductions in ANPP were greater in drier ecosystems and those with fewer plant species. Overall, our results demonstrate with unprecedented rigor that the global impacts of projected increases in drought severity have been significantly underestimated and that drier and less diverse sites are likely to be most vulnerable to extreme drought.</p></article>", "keywords": ["[SDE] Environmental Sciences", "Medical Sciences", "Drought Severity", "550", "580 Plants (Botany)", "551", "Tierras de Matorral", "Medical Specialties", "Medicine and Health Sciences", "SDG 13 - Climate Action", "climate extreme | Drought-Net | International Drought Experiment | productivity", "Productividad Primaria Neta", "Net Primary Productivity", "Productivity", "2. Zero hunger", "Praderas", "Productividad", "Life Sciences", "Biological Sciences", "Grassland", "6. Clean water", "Droughts", "Grasslands", "[SDE]Environmental Sciences", "Drought-Net", "Public Health", "International Drought Experiment", "Ciclo del Carbono", "Severidad de la Sequ\u00eda", "Global Impacts", "productivity", "Climate Change", "climate extreme", "333", "Carbon Cycle", "Environmental Public Health", "XXXXXX - Unknown", "Impacto Global", "Scrublands", "General", "Biology", "Ecosystem", "Experimento internacional de Sequ\u00eda", "500", "Receptor Protein-Tyrosine Kinases", "15. Life on land", "Clima Extremo", "Climate Science", "13. Climate action", "Cambio Clim\u00e1tico", "Extreme Climate", "Climate extreme", "Klimatvetenskap"]}, "links": [{"href": "https://boris.unibe.ch/191349/1/smith-et-al-2024-extreme-drought-impacts-have-been-underestimated-in-grasslands-and-shrublands-globally.pdf"}, {"href": "https://escholarship.org/content/qt9b707158/qt9b707158.pdf"}, {"href": "https://doi.org/10.1073/pnas.2309881120"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Proceedings%20of%20the%20National%20Academy%20of%20Sciences", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1073/pnas.2309881120", "name": "item", "description": "10.1073/pnas.2309881120", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1073/pnas.2309881120"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2024-01-08T00:00:00Z"}}, {"id": "10.1073/pnas.2317332121", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:18:45Z", "type": "Journal Article", "created": "2024-04-26", "title": "Negative correlation between soil salinity and soil organic carbon variability", "description": "<p>Soil organic carbon (SOC) is vital for terrestrial ecosystems, affecting biogeochemical processes, and soil health. It is known that soil salinity impacts SOC content, yet the specific direction and magnitude of SOC variability in relation to soil salinity remain poorly understood. Analyzing 43,459 mineral soil samples (SOC &lt; 150 g kg\uffe2\uff88\uff921) collected across different land covers since 1992, we approximate a soil salinity increase from 1 to 5 dS m\uffe2\uff88\uff921in croplands would be associated with a decline in mineral soils SOC from 0.14 g kg\uffe2\uff88\uff921above the mean predicted SOC (SOC\uffc2\uffafc= 18.47 g kg\uffe2\uff88\uff921) to 0.46 g kg\uffe2\uff88\uff921belowSOC\uffc2\uffafc(~\uffe2\uff88\uff92430%), while for noncroplands, such decline is sharper, from 0.96 aboveSOC\uffc2\uffafnc= 35.96 g kg\uffe2\uff88\uff921to 4.99 belowSOC\uffc2\uffafnc(~\uffe2\uff88\uff92620%). Although salinity\uffe2\uff80\uff99s significance in explaining SOC variability is minor (&lt;6%), we estimate a one SD increase in salinity of topsoil samples (0 to 7 cm) correlates with respectiveSOC\uffc2\uffafdeclines of ~4.4% and ~9.26%, relative toSOC\uffc2\uffafcandSOC\uffc2\uffafnc. TheSOC\uffc2\uffafdecline in croplands is greatest in vegetation/cropland mosaics while lands covered with evergreen needle-leaved trees are estimated with the highestSOC\uffc2\uffafdecline in noncroplands. We identify soil nitrogen, land cover, and precipitation Seasonality Index as the most significant parameters in explaining the SOC\uffe2\uff80\uff99s variability. The findings provide insights into SOC dynamics under increased soil salinity, improving understanding of SOC stock responses to land degradation and climate warming.</p", "keywords": ["570", "soil salinity", "Supplementary Data", "QH301 Biology", "500", "04 agricultural and veterinary sciences", "environmental impact", "01 natural sciences", "soil organic carbon", "QH301", "biogeochemistry", "carbon cycle", "Physical Sciences", "SDG 13 - Climate Action", "0401 agriculture", " forestry", " and fisheries", "General", "SDG 15 - Life on Land", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/10.1073/pnas.2317332121"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Proceedings%20of%20the%20National%20Academy%20of%20Sciences", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1073/pnas.2317332121", "name": "item", "description": "10.1073/pnas.2317332121", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1073/pnas.2317332121"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2024-04-26T00:00:00Z"}}, {"id": "10.1111/gcb.16122", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:19:23Z", "type": "Journal Article", "created": "2022-02-06", "title": "Soil fauna drives vertical redistribution of soil organic carbon in a long\u2010term irrigated dry pine forest", "description": "Abstract<p>Summer droughts strongly affect soil organic carbon (SOC) cycling, but net effects on SOC storage are unclear as drought affects both C inputs and outputs from soils. Here, we explored the overlooked role of soil fauna on SOC storage in forests, hypothesizing that soil faunal activity is particularly drought\uffe2\uff80\uff90sensitive, thereby reducing litter incorporation into the mineral soil and, eventually, long\uffe2\uff80\uff90term SOC storage.</p><p>In a drought\uffe2\uff80\uff90prone pine forest (Switzerland), we performed a large\uffe2\uff80\uff90scale irrigation experiment for 17\uffc2\uffa0years and assessed its impact on vertical SOC distribution and composition. We also examined litter mass loss of dominant tree species using different mesh\uffe2\uff80\uff90size litterbags and determined soil fauna abundance and community composition.</p><p>The 17\uffe2\uff80\uff90year\uffe2\uff80\uff90long irrigation resulted in a C loss in the organic layers (\uffe2\uff88\uff921.0\uffc2\uffa0kg\uffc2\uffa0C\uffc2\uffa0m\uffe2\uff88\uff922) and a comparable C gain in the mineral soil (+0.8\uffc2\uffa0kg\uffc2\uffa0C\uffc2\uffa0m\uffe2\uff88\uff922) and thus did not affect total SOC stocks. Irrigation increased the mass loss ofQuercus pubescensandViburnum lantanaleaf litter, with greater effect sizes when meso\uffe2\uff80\uff90 and macrofauna were included (+215%) than when excluded (+44%). The enhanced faunal\uffe2\uff80\uff90mediated litter mass loss was paralleled by a many\uffe2\uff80\uff90fold increase in the abundance of meso\uffe2\uff80\uff90 and macrofauna during irrigation. Moreover, Acari and Collembola community composition shifted, with a higher presence of drought\uffe2\uff80\uff90sensitive species in irrigated soils. In comparison, microbial SOC mineralization was less sensitive to soil moisture. Our results suggest that the vertical redistribution of SOC with irrigation was mainly driven by faunal\uffe2\uff80\uff90mediated litter incorporation, together with increased root C inputs.</p><p>Our study shows that soil fauna is highly sensitive to natural drought, which leads to a reduced C transfer from organic layers to the mineral soil. In the longer term, this potentially affects SOC storage and, therefore, soil fauna plays a key but so far largely overlooked role in shaping SOC responses to drought.</p", "keywords": ["2. Zero hunger", "550", "carbon cycling", "drought", "litter decomposition", "04 agricultural and veterinary sciences", "Forests", "carbon storage", "15. Life on land", "Pinus", "Carbon", "soil biota", "6. Clean water", "Carbon Cycle", "Soil", "forest", "carbon cycling; carbon storage; climate change; drought; forest; litter decomposition; mesofauna communities; soil biota", "climate change", "mesofauna communities", "13. Climate action", "0401 agriculture", " forestry", " and fisheries", "Research Articles"]}, "links": [{"href": "https://onlinelibrary.wiley.com/doi/pdf/10.1111/gcb.16122"}, {"href": "https://doi.org/10.1111/gcb.16122"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Global%20Change%20Biology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1111/gcb.16122", "name": "item", "description": "10.1111/gcb.16122", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1111/gcb.16122"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2022-02-21T00:00:00Z"}}, {"id": "10.1111/gcb.70071", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:19:24Z", "type": "Journal Article", "created": "2025-02-14", "title": "Greenhouse Gas Emissions and Lateral Carbon Dynamics at an Eroding Yedoma Permafrost Site in Siberia (Duvanny Yar)", "description": "ABSTRACT<p>Rapid Arctic warming is accelerating permafrost thaw and mobilizing previously frozen organic carbon (OC) into waterways. Upon thaw, permafrost\uffe2\uff80\uff90derived OC can become susceptible to microbial degradation that may lead to greenhouse gas emissions (GHG), thus accelerating climate change. Abrupt permafrost thaw (e.g., riverbank erosion, retrogressive thaw slumps) occurs in areas rich in OC. Given the high OC content and the increase in frequency of abrupt thaw events, these environments may increasingly contribute to permafrost GHG emissions in the future. To better assess these emissions from abrupt permafrost thaw, we incubated thaw stream waters from an abrupt permafrost thaw site (Duvanny Yar, Siberia) and additionally, waters from their outflow to the Kolyma River. Our results show that CO2 release by volume from thaw streams was substantially higher than CO2 emissions from the river outflow waters, while the opposite was true for CO2 release normalized to the suspended sediment weight (gram dry weight). The CH4 emissions from both thaw streams and outflow waters were at a similar range, but an order of magnitude lower than those of CO2. Additionally, we show that nearshore riverbank waters differ in their biogeochemistry from thaw streams and Kolyma River mainstem: particles resemble thaw streams while dissolved fraction is more alike to the Kolyma River thalweg. In these waters dissolved OC losses are faster than in the river thalweg. Our incubations offer a first insight into the GHG release from permafrost thaw streams that connect exposed and degrading permafrost outcrops to larger river systems.</p", "keywords": ["CH4", "Arctic Regions", "Climate Change", "Permafrost", "Carbon Dioxide", "incubation", "Carbon", "Carbon Cycle", "Siberia", "CH4; CO2; incubation; riverbank erosion", "Greenhouse Gases", "Rivers", "CO2", "riverbank erosion", "Methane", "Research Article"], "contacts": [{"organization": "Kirsi H. Keskitalo, Lisa Br\u00f6der, Dirk J. Jong, Paul J. Mann, Tommaso Tesi, Anna Davydova, Nikita Zimov, Negar Haghipour, Timothy I. Eglinton, Jorien E. Vonk,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.1111/gcb.70071"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Global%20Change%20Biology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1111/gcb.70071", "name": "item", "description": "10.1111/gcb.70071", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1111/gcb.70071"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2025-02-01T00:00:00Z"}}, {"id": "10.1111/gcb.70179", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:19:24Z", "type": "Journal Article", "created": "2025-04-07", "title": "Lightning Impacts on Global Forest and Carbon Dynamics: Current Understanding and Knowledge Gaps", "description": "Lightning is a fundamental Earth system process that influences the world's major forest biomes and their carbon storage through two primary pathways. Lightning is the major cause of boreal forest fires, while lightning strikes kill patches of trees in tropical forests. We summarized the current understanding of these processes and identified knowledge gaps.", "keywords": ["carbon", "tropical", "Forests", "Lightning", "Carbon", "Carbon Cycle", "Trees", "forest", "Perspective", "boreal", "tree mortality", "Life Science", "lightning", "fire"], "contacts": [{"organization": "Sander Veraverbeke, Thomas A. J. Janssen, Esther Brambleby, Matt Jones, Bianca Zoletto, Masha T. van der Sande,", "roles": ["creator"]}]}, "links": [{"href": "https://ueaeprints.uea.ac.uk/id/eprint/99058/1/Veraverbeke_etal_2025_GlobalChangeBiology.pdf"}, {"href": "https://doi.org/10.1111/gcb.70179"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Global%20Change%20Biology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1111/gcb.70179", "name": "item", "description": "10.1111/gcb.70179", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1111/gcb.70179"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2025-04-01T00:00:00Z"}}, {"id": "10.1080/02571862.2005.10634705", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:18:51Z", "type": "Journal Article", "created": "2013-01-15", "title": "Ecosystem Carbon Storage Under Different Land Uses In Three Semi-Arid Shrublands And A Mesic Grassland In South Africa", "description": "Carbon (C) storage in biomass and soils is a function of climate, vegetation type, soil type and land management. Carbon storage was examined in intact indigenous vegetation and under different land uses in thicket (250\u2013400 mm mean annual precipitation), xeric shrubland (350 mm), karoo (250 mm), and grassland (900\u20131200 mm). Carbon storage was as follows: (i) mean soil C (0\u201350 cm): thicket (T) = grassland (G) > xeric shrubland on Dwyka sediments (XS) > xeric shrubland on dolerite (XSD) > karoo (K) (168, 164, 65, 34 & 26 t ha\u22121, respectively); (ii) mean root C: T > G > XS = XSD (25.4, 11.4, 7.2 & 7.1 t ha\u22121); (iii) mean above-ground C including leaf litter: T>XS>G>K> XSD (51.6, 12.9, 2.0, 1.7 & 1.51 ha\u22121). Carbon stocks in intact indigenous vegetation were related more to woodiness of vegetation and frequency of fire than to climate. Biomass C was greatest in woody thicket and soil C stocks were greatest in thicket and grassland. Total C storage of 245 t ha\u22129 in thicket is exceptionally high for a semi-arid...", "keywords": ["580", "2. Zero hunger", "biomass", "Sub-Saharan Africa", "Eastern Hemisphere", "World", "land management", "land use", "04 agricultural and veterinary sciences", "15. Life on land", "South Africa", "carbon cycle", "Africa", "0401 agriculture", " forestry", " and fisheries", "Arida", "Southern Africa"]}, "links": [{"href": "https://doi.org/10.1080/02571862.2005.10634705"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/South%20African%20Journal%20of%20Plant%20and%20Soil", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1080/02571862.2005.10634705", "name": "item", "description": "10.1080/02571862.2005.10634705", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1080/02571862.2005.10634705"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2005-01-01T00:00:00Z"}}, {"id": "10.1111/gcb.15849", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-06-24T16:19:23Z", "type": "Journal Article", "created": "2021-08-17", "title": "Connectivity and pore accessibility in models of soil carbon cycling", "description": "<p>This article is a Letter to the Editor on:https://onlinelibrary.wiley.com/doi/10.1111/gcb.15365. See also Response to this Letter at https://onlinelibrary.wiley.com/doi/10.1111/gcb.15850.</p><p>This is a letter to Waring et al., 27, e15\uffe2\uff80\uff93e16.</p", "keywords": ["[SDE] Environmental Sciences", "Soil", "13. Climate action", "[SDE]Environmental Sciences", "01 natural sciences", "Carbon", "Carbon Cycle", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://onlinelibrary.wiley.com/doi/pdf/10.1111/gcb.15849"}, {"href": "https://doi.org/10.1111/gcb.15849"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Global%20Change%20Biology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1111/gcb.15849", "name": "item", "description": "10.1111/gcb.15849", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1111/gcb.15849"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2021-08-25T00:00:00Z"}}, {"id": "10.1111/gcb.15933", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-06-24T16:19:23Z", "type": "Journal Article", "created": "2021-10-13", "title": "Long\u2010term ecosystem nitrogen limitation from foliar \u03b4 15 N data and a land surface model", "description": "Abstract<p>The effect of nutrient availability on plant growth and the terrestrial carbon sink under climate change and elevated CO2 remains one of the main uncertainties of the terrestrial carbon cycle. This is partially due to the difficulty of assessing nutrient limitation at large scales over long periods of time. Consistent declines in leaf nitrogen (N) content and leaf \uffce\uffb415N have been used to suggest that nitrogen limitation has increased in recent decades, most likely due to the concurrent increase in atmospheric CO2. However, such data sets are often not straightforward to interpret due to the complex factors that contribute to the spatial and temporal variation in leaf N and isotope concentration. We use the land surface model (LSM) QUINCY, which has the unique capacity to represent N isotopic processes, in conjunction with two large data sets of foliar N and N isotope content. We run the model with different scenarios to test whether foliar \uffce\uffb415N isotopic data can be used to infer large\uffe2\uff80\uff90scale N limitation and if the observed trends are caused by increasing atmospheric CO2, changes in climate or changes in sources and magnitude of anthropogenic N deposition. We show that while the model can capture the observed change in leaf N content and predict widespread increases in N limitation, it does not capture the pronounced, but very spatially heterogeneous, decrease in foliar \uffce\uffb415N observed in the data across the globe. The addition of an observation\uffe2\uff80\uff90based temporal trend in isotopic composition of N deposition leads to a more pronounced decrease in simulated leaf \uffce\uffb415N. Our results show that leaf \uffce\uffb415N observations cannot, on their own, be used to assess global\uffe2\uff80\uff90scale N limitation and that using such a data set in conjunction with an LSM can reveal the drivers behind the observed patterns.</p>", "keywords": ["0106 biological sciences", "Plant Leaves", "Carbon Sequestration", "Nitrogen", "13. Climate action", "Climate Change", "0401 agriculture", " forestry", " and fisheries", "04 agricultural and veterinary sciences", "15. Life on land", "01 natural sciences", "Ecosystem", "Carbon Cycle", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://onlinelibrary.wiley.com/doi/pdf/10.1111/gcb.15933"}, {"href": "https://doi.org/10.1111/gcb.15933"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Global%20Change%20Biology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1111/gcb.15933", "name": "item", "description": "10.1111/gcb.15933", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1111/gcb.15933"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2021-07-16T00:00:00Z"}}, {"id": "10.1111/gcb.17268", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-06-24T16:19:23Z", "type": "Journal Article", "created": "2024-04-02", "title": "Microbial evolution\u2014An under\u2010appreciated driver of soil carbon cycling", "description": "Abstract<p>Although substantial advances in predicting the ecological impacts of global change have been made, predictions of the evolutionary impacts have lagged behind. In soil ecosystems, microbes act as the primary energetic drivers of carbon cycling; however, microbes are also capable of evolving on timescales comparable to rates of global change. Given the importance of soil ecosystems in global carbon cycling, we assess the potential impact of microbial evolution on carbon\uffe2\uff80\uff90climate feedbacks in this system. We begin by reviewing the current state of knowledge concerning microbial evolution in response to global change and its specific effect on soil carbon dynamics. Through this integration, we synthesize a roadmap detailing how to integrate microbial evolution into ecosystem biogeochemical models. Specifically, we highlight the importance of microscale mechanistic soil carbon models, including choosing an appropriate evolutionary model (e.g., adaptive dynamics, quantitative genetics), validating model predictions with \uffe2\uff80\uff98omics\uffe2\uff80\uff99 and experimental data, scaling microbial adaptations to ecosystem level processes, and validating with ecosystem\uffe2\uff80\uff90scale measurements. The proposed steps will require significant investment of scientific resources and might require 10\uffe2\uff80\uff9320\uffe2\uff80\uff89years to be fully implemented. However, through the application of multi\uffe2\uff80\uff90scale integrated approaches, we will advance the integration of microbial evolution into predictive understanding of ecosystems, providing clarity on its role and impact within the broader context of environmental change.</p", "keywords": ["cycle evolution global change microbe", "570", "550", "Climate", "Evolutionsbiologi", "Soil", "biogeochemistry", "carbon cycle", "evolution", "global change", "Ecosystem", "Soil Microbiology", "Ekologi", "2. Zero hunger", "[SDU.OCEAN]Sciences of the Universe [physics]/Ocean", "Evolutionary Biology", "Ecology", "Atmosphere", "cycle", "[SDU.OCEAN] Sciences of the Universe [physics]/Ocean", " Atmosphere", "Biological Sciences", "15. Life on land", "[SDU.ENVI] Sciences of the Universe [physics]/Continental interfaces", " environment", "Carbon", "6. Clean water", "Environmental sciences", "microbe", "Biological sciences", "Earth sciences", "13. Climate action", "[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces", "environment", "Environmental Sciences"]}, "links": [{"href": "https://onlinelibrary.wiley.com/doi/pdf/10.1111/gcb.17268"}, {"href": "https://doi.org/10.1111/gcb.17268"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Global%20Change%20Biology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1111/gcb.17268", "name": "item", "description": "10.1111/gcb.17268", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1111/gcb.17268"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2024-04-01T00:00:00Z"}}, {"id": "10.1111/gcb.17297", "type": "Feature", "geometry": null, "properties": {"updated": "2026-06-24T16:19:23Z", "type": "Journal Article", "created": "2024-05-13", "title": "Convergence in simulating global soil organic carbon by structurally different models after data assimilation", "description": "Abstract<p>Current biogeochemical models produce carbon\uffe2\uff80\uff93climate feedback projections with large uncertainties, often attributed to their structural differences when simulating soil organic carbon (SOC) dynamics worldwide. However, choices of model parameter values that quantify the strength and represent properties of different soil carbon cycle processes could also contribute to model simulation uncertainties. Here, we demonstrate the critical role of using common observational data in reducing model uncertainty in estimates of global SOC storage. Two structurally different models featuring distinctive carbon pools, decomposition kinetics, and carbon transfer pathways simulate opposite global SOC distributions with their customary parameter values yet converge to similar results after being informed by the same global SOC database using a data assimilation approach. The converged spatial SOC simulations result from similar simulations in key model components such as carbon transfer efficiency, baseline decomposition rate, and environmental effects on carbon fluxes by these two models after data assimilation. Moreover, data assimilation results suggest equally effective simulations of SOC using models following either first\uffe2\uff80\uff90order or Michaelis\uffe2\uff80\uff93Menten kinetics at the global scale. Nevertheless, a wider range of data with high\uffe2\uff80\uff90quality control and assurance are needed to further constrain SOC dynamics simulations and reduce unconstrained parameters. New sets of data, such as microbial genomics\uffe2\uff80\uff90function relationships, may also suggest novel structures to account for in future model development. Overall, our results highlight the importance of observational data in informing model development and constraining model predictions.</p", "keywords": ["Soil", "13. Climate action", "0401 agriculture", " forestry", " and fisheries", "Computer Simulation", "04 agricultural and veterinary sciences", "Models", " Theoretical", "15. Life on land", "01 natural sciences", "Carbon", "Carbon Cycle", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/10.1111/gcb.17297"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Global%20Change%20Biology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1111/gcb.17297", "name": "item", "description": "10.1111/gcb.17297", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1111/gcb.17297"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2024-05-01T00:00:00Z"}}], "links": [{"rel": "self", "type": "application/geo+json", "title": "This document as GeoJSON", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items?keywords=N+cycle&offset=50&f=json", "hreflang": "en-US"}, {"rel": "alternate", "type": "text/html", "title": "This document as HTML", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items?keywords=N+cycle&offset=50&f=html", "hreflang": "en-US"}, {"rel": "collection", "type": "application/json", "title": "Collection URL", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main", "hreflang": "en-US"}, {"type": "application/geo+json", "rel": "prev", "title": "items (prev)", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items?keywords=N+cycle&offset=0", "hreflang": "en-US"}, {"rel": "next", "type": "application/geo+json", "title": "items (next)", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items?keywords=N+cycle&offset=100", "hreflang": "en-US"}], "numberMatched": 282, "numberReturned": 50, "distributedFeatures": [], "timeStamp": "2026-06-25T05:17:36.585079Z"}