{"type": "FeatureCollection", "facets": {"type": {"type": "terms", "property": "type", "buckets": [{"value": "Journal Article", "count": 25}, {"value": "Dataset", "count": 1}]}, "soil_chemical_properties": {"type": "terms", "property": "soil_chemical_properties", "buckets": [{"value": "soil organic matter", "count": 4}, {"value": "carbon", "count": 3}]}, "soil_biological_properties": {"type": "terms", "property": "soil_biological_properties", "buckets": [{"value": "biomass production", "count": 1}, {"value": "plants", "count": 1}, {"value": "respiration", "count": 1}, {"value": "vegetation", "count": 1}]}, "soil_physical_properties": {"type": "terms", "property": "soil_physical_properties", "buckets": []}, "soil_classification": {"type": "terms", "property": "soil_classification", "buckets": []}, "soil_functions": {"type": "terms", "property": "soil_functions", "buckets": [{"value": "soil biodiversity", "count": 4}, {"value": "soil fertility", "count": 3}, {"value": "species diversity", "count": 2}, {"value": "decomposition", "count": 1}, {"value": "ecosystem services", "count": 1}, {"value": "land cover change", "count": 1}, {"value": "productivity", "count": 1}, {"value": "water conservation", "count": 1}]}, "soil_threats": {"type": "terms", "property": "soil_threats", "buckets": [{"value": "soil degradation", "count": 2}, {"value": "desertification", "count": 1}]}, "soil_processes": {"type": "terms", "property": "soil_processes", "buckets": [{"value": "soil functioning", "count": 1}]}, "soil_management": {"type": "terms", "property": "soil_management", "buckets": []}, "ecosystem_services": {"type": "terms", "property": "ecosystem_services", "buckets": [{"value": "ecosystem functioning", "count": 26}, {"value": "terrestrial ecosystems", "count": 8}, {"value": "hydrological cycle", "count": 1}]}}, "features": [{"id": "10.1002/ldr.2784", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-04-04T16:14:19Z", "type": "Journal Article", "created": "2017-08-24", "title": "Alleviating Nitrogen Limitation in Mediterranean Maquis Vegetation Leads to Ecological Degradation", "description": "Abstract<p>Soils are being degraded at an alarming rate and thereby also crucial ecosystem goods and services. Nitrogen (N) enrichment is a major driver of this degradation. While the negative impacts of N enrichment on vegetation are well known globally, those on various ecological interactions, and on ecosystem functioning, remain largely unknown. Because Mediterranean ecosystems are N limited, they are good model systems for evaluating how N enrichment impacts not only vegetation but also ecological partnerships and ecosystem functioning. Using a 7\uffe2\uff80\uff90year N\uffe2\uff80\uff90manipulation (dose and form) field experiment running in a Mediterranean Basin maquis located in a region with naturally low ambient N deposition (&lt;4\uffc2\uffa0kg\uffc2\uffa0N\uffc2\uffa0ha\uffe2\uff88\uff921\uffc2\uffa0y\uffe2\uff88\uff921), we assessed the impacts of the N additions on (i) the dominant plant species (photosynthetic N\uffe2\uff80\uff90use efficiency); (ii) plant\uffe2\uff80\uff93soil ecological partnerships with ectomycorrhiza and N\uffe2\uff80\uff90fixing bacteria; and (iii) ecosystem degradation (plant\uffe2\uff80\uff93soil cover, biological mineral weathering and soil N fixation). N additions significantly disrupted plant\uffe2\uff80\uff93soil cover, plant\uffe2\uff80\uff93soil biotic interactions, and ecosystem functioning compared with ambient N deposition conditions. However, the higher the ammonium dose (alone or with nitrate), the more drastic these disruptions were. We report a critical threshold at 20\uffe2\uff80\uff9340\uffc2\uffa0kg ammonium ha\uffe2\uff88\uff921\uffc2\uffa0y\uffe2\uff88\uff921 whereby severe ecosystem degradation can be expected. These observations are critical to help explain the mechanisms behind ecosystem degradation, to describe the collective loss of organisms and multifunction in the landscape, and to predict potential fragmentation of Mediterranean maquis under conditions of unrelieved N enrichment. Copyright \uffc2\uffa9 2017 John Wiley &amp; Sons, Ltd.</p>", "keywords": ["0106 biological sciences", "2. Zero hunger", "plant\u2013soil ecological partnerships", "04 agricultural and veterinary sciences", "Mediterranean", "15. Life on land", "01 natural sciences", "nitrogen", "ammonium", "soil degradation", "13. Climate action", "ecosystem functioning", "XXXXXX - Unknown", "Plant-soil ecological partnerships", "Ecosystem functioning", "ecosystem degradation", "0401 agriculture", " forestry", " and fisheries", "Ecosystem degradation", "ecosystems", "Ammonium"]}, "links": [{"href": "https://onlinelibrary.wiley.com/doi/pdf/10.1002/ldr.2784"}, {"href": "https://doi.org/10.1002/ldr.2784"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Land%20Degradation%20%26amp%3B%20Development", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1002/ldr.2784", "name": "item", "description": "10.1002/ldr.2784", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1002/ldr.2784"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2017-09-12T00:00:00Z"}}, {"id": "10.1016/j.soilbio.2008.05.007", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-04T16:17:05Z", "type": "Journal Article", "created": "2008-06-12", "title": "Long-Term Organic Farming Fosters Below And Aboveground Biota: Implications For Soil Quality, Biological Control And Productivity", "description": "Organic farming may contribute substantially to future agricultural production worldwide by improving soil quality and pest control, thereby reducing environmental impacts of conventional farming. We investigated in a comprehensive way soil chemical, as well as below and aboveground biological parameters of two organic and two conventional wheat farming systems that primarily differed in fertilization and weed management strategies. Contrast analyses identified management related differences between \u201cherbicide-free\u201d bioorganic (BIOORG) and biodynamic (BIODYN) systems and conventional systems with (CONFYM) or without manure (CONMIN) and herbicide application within a long-term agricultural experiment (DOK trial, Switzerland). Soil carbon content was significantly higher in systems receiving farmyard manure and concomitantly microbial biomass (fungi and bacteria) was increased. Microbial activity parameters, such as microbial basal respiration and nitrogen mineralization, showed an opposite pattern, suggesting that soil carbon in the conventional system (CONFYM) was more easily accessible to microorganisms than in organic systems. Bacterivorous nematodes and earthworms were most abundant in systems that received farmyard manure, which is in line with the responses of their potential food sources (microbes and organic matter). Mineral fertilizer application detrimentally affected enchytraeids and Diptera larvae, whereas aphids benefited. Spider abundance was favoured by organic management, most likely a response to increased prey availability from the belowground subsystem or increased weed coverage. In contrast to most soil-based, bottom-up controlled interactions, the twofold higher abundance of this generalist predator group in organic systems likely contributed to the significantly lower abundance of aboveground herbivore pests (aphids) in these systems. Long-term organic farming and the application of farmyard manure promoted soil quality, microbial biomass and fostered natural enemies and ecosystem engineers, suggesting enhanced nutrient cycling and pest control. Mineral fertilizers and herbicide application, in contrast, affected the potential for top-down control of aboveground pests negatively and reduced the organic carbon levels. Our study indicates that the use of synthetic fertilizers and herbicide application changes interactions within and between below and aboveground components, ultimately promoting negative environmental impacts of agriculture by reducing internal biological cycles and pest control. On the contrary, organic farming fosters microbial and faunal decomposers and this propagates into the aboveground system via generalist predators thereby increasing conservation biological control. However, grain and straw yields were 23% higher in systems receiving mineral fertilizers and herbicides reflecting the trade-off between productivity and environmental responsibility.", "keywords": ["[SDE] Environmental Sciences", "generalist predators", "respiration microbienne", "[SDV]Life Sciences [q-bio]", "faune du sol", "natural enemies", "alternative prey", "630", "nitrogen", "food-web", "Soil", "agriculture biologique", "cycle biologique", "herbicide", "min\u00e9ralisation de l'azote", "fertilisation organique", "fertilisation min\u00e9rale", "soil quality", "2. Zero hunger", "agriculture biodynamique", "agriculture conventionnelle", "nutrient cycling", "04 agricultural and veterinary sciences", "sustainability", "long terme", "6. Clean water", "[SDV] Life Sciences [q-bio]", "mycorrhizal fungi", "ennemi naturel", "microbial community structure", "ecosystem functioning", "[SDE]Environmental Sciences", "DOK trial;ecosystem functioning;farming system;fertilization;generalist predators;microbial community;nutrient cycling;natural enemies;soil fauna;soil quality;sustainability", "microbial community", "soil fauna", "agricultural systems", "management", "570", "agroecosystems", "Soil quality", "suisse", "productivit\u00e9", "Soil biology", "culture c\u00e9r\u00e9aliere", "triticum aestivum", "biomasse microbienne", "biomass", "DOK trial", "15. Life on land", "qualit\u00e9 biologique du sol", "fertilization", "13. Climate action", "Biodiversity and ecosystem services", "0401 agriculture", " forestry", " and fisheries", "farming system", "Cereals", " pulses and oilseeds"]}, "links": [{"href": "https://doi.org/10.1016/j.soilbio.2008.05.007"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Soil%20Biology%20and%20Biochemistry", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.soilbio.2008.05.007", "name": "item", "description": "10.1016/j.soilbio.2008.05.007", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.soilbio.2008.05.007"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2008-09-01T00:00:00Z"}}, {"id": "10.1038/s43247-022-00523-5", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-04T16:18:03Z", "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": "10.1038/srep08280", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-04T16:18:03Z", "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": "10.1111/1365-2435.12329", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-04-04T16:18:52Z", "type": "Journal Article", "created": "2014-09-05", "title": "Interactive Effects Of C, N And P Fertilization On Soil Microbial Community Structure And Function In An Amazonian Rain Forest", "description": "Summary<p>   <p>Resource control over abundance, structure and functional diversity of soil microbial communities is a key determinant of soil processes and related ecosystem functioning. Copiotrophic organisms tend to be found in environments which are rich in nutrients, particularly carbon, in contrast to oligotrophs, which survive in much lower carbon concentrations.</p>  <p>We hypothesized that microbial biomass, activity and community structure in nutrient\uffe2\uff80\uff90poor soils of an Amazonian rain forest are limited by multiple elements in interaction. We tested this hypothesis with a fertilization experiment by adding C (as cellulose), N (as urea) and P (as phosphate) in all possible combinations to a total of 40 plots of an undisturbed tropical forest in French Guiana.</p>  <p>After 2\uffc2\uffa0years of fertilization, we measured a 47% higher biomass, a 21% increase in substrate\uffe2\uff80\uff90induced respiration rate and a 5\uffe2\uff80\uff90fold higher rate of decomposition of cellulose paper discs of soil microbial communities that grew in P\uffe2\uff80\uff90fertilized plots compared to plots without P fertilization. These responses were amplified with a simultaneous C fertilization suggesting P and C colimitation of soil micro\uffe2\uff80\uff90organisms at our study site.</p>  <p>Moreover, P fertilization modified microbial community structure (PLFAs) to a more copiotrophic bacterial community indicated by a significant decrease in the Gram\uffe2\uff80\uff90positive\uffc2\uffa0:\uffc2\uffa0Gram\uffe2\uff80\uff90negative ratio. The Fungi\uffc2\uffa0:\uffc2\uffa0Bacteria ratio increased in N fertilized plots, suggesting that fungi are relatively more limited by N than bacteria. Changes in microbial community structure did not affect rates of general processes such as glucose mineralization and cellulose paper decomposition. In contrast, community level physiological profiles under P fertilization combined with either C or N fertilization or both differed strongly from all other treatments, indicating functionally different microbial communities.</p>  <p>While P appears to be the most critical from the three major elements we manipulated, the strongest effects were observed in combination with either supplementary C or N addition in support of multiple element control on soil microbial functioning and community structure.</p>  <p>We conclude that the soil microbial community in the studied tropical rain forest and the processes it drives is finely tuned by the relative availability in C, N and P. Any shifts in the relative abundance of these key elements may affect spatial and temporal heterogeneity in microbial community structure, their associated functions and the dynamics of C and nutrients in tropical ecosystems.</p>  </p>", "keywords": ["tropical forest", "2. Zero hunger", "570", "phospholipid fatty acids (PLFA)", "[SDE.MCG]Environmental Sciences/Global Changes", "functional significance", "[SDV.EE.IEO] Life Sciences [q-bio]/Ecology", " environment/Symbiosis", "04 agricultural and veterinary sciences", "15. Life on land", "16. Peace & justice", "[SDE.BE] Environmental Sciences/Biodiversity and Ecology", "[SDE.MCG] Environmental Sciences/Global Changes", "13. Climate action", "microbial community structure", "ecosystem functioning", "environment/Symbiosis", "[SDV.EE.ECO]Life Sciences [q-bio]/Ecology", "[SDV.EE.ECO] Life Sciences [q-bio]/Ecology", " environment/Ecosystems", "[SDV.EE.IEO]Life Sciences [q-bio]/Ecology", "0401 agriculture", " forestry", " and fisheries", "multiple resource limitation", "[SDE.BE]Environmental Sciences/Biodiversity and Ecology", "phosphorus", "environment/Ecosystems", "soil functioning"]}, "links": [{"href": "https://doi.org/10.1111/1365-2435.12329"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Functional%20Ecology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1111/1365-2435.12329", "name": "item", "description": "10.1111/1365-2435.12329", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1111/1365-2435.12329"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2014-09-29T00:00:00Z"}}, {"id": "10.1088/1748-9326/aaeb5f", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-04-04T16:18:35Z", "type": "Journal Article", "created": "2018-10-25", "title": "Revisiting IPCC Tier 1 coefficients for soil organic and biomass carbon storage in agroforestry systems", "description": "Open AccessLos sistemas agroforestales comprenden \u00e1rboles y cultivos, o \u00e1rboles y pastos dentro del mismo campo. A nivel mundial, cubren aproximadamente mil millones de hect\u00e1reas de tierra y contribuyen a los medios de vida de m\u00e1s de 900 millones de personas. Los sistemas agroforestales tienen la capacidad de secuestrar grandes cantidades de carbono (C) tanto en el suelo como en la biomasa. Sin embargo, estos sistemas a\u00fan no se han considerado completamente en el enfoque de la contabilidad C desarrollado por el Grupo Intergubernamental de Expertos sobre el Cambio Clim\u00e1tico, en gran parte debido a la alta diversidad de los sistemas agroforestales y la escasez de datos relevantes. Nuestra revisi\u00f3n de la literatura identific\u00f3 un total de 72 art\u00edculos cient\u00edficos revisados por pares asociados con el almacenamiento de biomasa C (50) y con el carbono org\u00e1nico del suelo (SOC) (122), que contienen un total de 542 observaciones (324 y 218, respectivamente). Con base en una s\u00edntesis de las observaciones informadas, presentamos un conjunto de coeficientes de Nivel 1 para el almacenamiento de biomasa C para cada uno de los ocho sistemas agroforestales principales identificados, incluidos cultivos en callejones, barbechos, setos, multiestratos, parques, cultivos perennes sombreados, silvoarables y sistemas silvopastoriles, desglosados por clima y regi\u00f3n. Utilizando la misma clasificaci\u00f3n agroforestal, presentamos un conjunto de factores de cambio de stock (FLU) y tasas de acumulaci\u00f3n/p\u00e9rdida de COS para tres cambios principales en el uso de la tierra (Luc): de tierras de cultivo a agroforester\u00eda; de bosques a agroforester\u00eda; y de pastizales a agroforester\u00eda. A nivel mundial, los factores medios de cambio de stock SOC (\u00b1 intervalos de confianza) se estimaron en 1,25 \u00b1 0,04, 0,89 \u00b1 0,07 y 1,19 \u00b1 0,10, para los tres LUC principales, respectivamente. Sin embargo, estos coeficientes promedio ocultan enormes disparidades entre y dentro de diferentes climas, regiones y tipos de sistemas agroforestales, lo que destaca la necesidad de adoptar los coeficientes m\u00e1s desagregados que se proporcionan en este documento. Alentamos a los gobiernos nacionales a sintetizar datos de experimentos de campo locales para generar factores espec\u00edficos de cada pa\u00eds para una estimaci\u00f3n m\u00e1s s\u00f3lida de la biomasa y el almacenamiento de COS.", "keywords": ["emission factor", "Carbon sequestration", "Biomass (ecology)", "F08 - Syst\u00e8mes et modes de culture", "Environmental technology. Sanitary engineering", "climate change mitigation", "Agricultural and Biological Sciences", "Climate change mitigation", "http://aims.fao.org/aos/agrovoc/c_7427", "Agroforestry Systems and Biodiversity Enhancement", "Soil water", "11. Sustainability", "Climate change", "GE1-350", "TD1-1066", "http://aims.fao.org/aos/agrovoc/c_35657", "agroforesterie", "2. Zero hunger", "changement climatique", "Global and Planetary Change", "Geography", "Ecology", "Physics", "Q", "Life Sciences", "Forestry", "Agriculture", "04 agricultural and veterinary sciences", "Soil carbon", "http://aims.fao.org/aos/agrovoc/c_207", "s\u00e9questration du carbone", "http://aims.fao.org/aos/agrovoc/c_926", "Archaeology", "http://aims.fao.org/aos/agrovoc/c_4182", "Physical Sciences", "Ecosystem Functioning", "mati\u00e8re organique du sol", "P33 - Chimie et physique du sol", "land use change", "P40 - M\u00e9t\u00e9orologie et climatologie", "Science", "QC1-999", "stockage", "Soil Science", "utilisation des terres", "Environmental science", "biomasse", "Ecosystem services", "http://aims.fao.org/aos/agrovoc/c_1666", "http://aims.fao.org/aos/agrovoc/c_1301", "Agroforestry", "Soil Carbon Sequestration", "Biology", "Land use", " land-use change and forestry", "Ecosystem", "Soil science", "15. Life on land", "http://aims.fao.org/aos/agrovoc/c_331583", "carbon sequestration", "Agronomy", "Environmental sciences", "Carbon dioxide", "13. Climate action", "FOS: Biological sciences", "Environmental Science", "Land use", "0401 agriculture", " forestry", " and fisheries", "carbone", "Soil Carbon Dynamics and Nutrient Cycling in Ecosystems", "Drivers and Impacts of Tropical Deforestation"]}, "links": [{"href": "https://doi.org/10.1088/1748-9326/aaeb5f"}, {"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/aaeb5f", "name": "item", "description": "10.1088/1748-9326/aaeb5f", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1088/1748-9326/aaeb5f"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2018-12-14T00:00:00Z"}}, {"id": "10.1111/cobi.13930", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-04-04T16:18:55Z", "type": "Journal Article", "created": "2022-05-05", "title": "Challenges of and opportunities for protecting European soil biodiversity", "description": "Abstract<p>Soil biodiversity and related ecosystem functions are neglected in most biodiversity assessments and nature conservation actions. We examined how society, and particularly policy makers, have addressed these factors worldwide with a focus on Europe and explored the role of soils in nature conservation in Germany as an example. We reviewed past and current global and European policies, compared soil ecosystem functioning in\uffe2\uff80\uff90 and outside protected areas, and examined the role of soils in nature conservation management via text analyses. Protection and conservation of soil biodiversity and soil ecosystem functioning have been insufficient. Soil\uffe2\uff80\uff90related policies are unenforceable and lack soil biodiversity conservation goals, focusing instead on other environmental objectives. We found no evidence of positive effects of current nature conservation measures in multiple soil ecosystem functions in Europe. In German conservation management, soils are considered only from a limited perspective (e.g., as physicochemical part of the environment and as habitat for aboveground organisms). By exploring policy, evidence, and management as it relates to soil ecosystems, we suggest an integrative perspective to move nature conservation toward targeting soil ecosystems directly (e.g., by setting baselines, monitoring soil threats, and establishing a soil indicator system).</p>", "keywords": ["0301 basic medicine", "570", "Conservation of Natural Resources", "0303 health sciences", "nature conservation", "soil biodiversity", "Biodiversity", "belowground", "Europe", "Soil", "03 medical and health sciences", "Biowissenschaften; Biologie", "Germany", "soil ecosystem functioning", "protected areas", "soil policy", "Ecosystem"]}, "links": [{"href": "https://onlinelibrary.wiley.com/doi/pdf/10.1111/cobi.13930"}, {"href": "https://doi.org/10.1111/cobi.13930"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Conservation%20Biology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1111/cobi.13930", "name": "item", "description": "10.1111/cobi.13930", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1111/cobi.13930"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2022-07-19T00:00:00Z"}}, {"id": "10.1111/j.1365-2486.2009.01970.x", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-04-04T16:19:11Z", "type": "Journal Article", "created": "2009-05-08", "title": "Solar Uvb And Warming Affect Decomposition And Earthworms In A Fen Ecosystem In Tierra Del Fuego, Argentina", "description": "Abstract<p>Combined effects of co\uffe2\uff80\uff90occurring global climate changes on ecosystem responses are generally poorly understood. Here, we present results from a 2\uffe2\uff80\uff90year field experiment in aCarexfen ecosystem on the southernmost tip of South America, where we examined the effects of solar ultraviolet B (UVB, 280\uffe2\uff80\uff93315\uffe2\uff80\uff83nm) and warming on above\uffe2\uff80\uff90 and belowground plant production, C\uffe2\uff80\uff83:\uffe2\uff80\uff83N ratios, decomposition rates and earthworm population sizes. Solar UVB radiation was manipulated using transparent plastic filter films to create a near\uffe2\uff80\uff90ambient (90% of ambient UVB) or a reduced solar UVB treatment (15% of ambient UVB). The warming treatment was imposed passively by wrapping the same filter material around the plots resulting in a mean air and soil temperature increase of about 1.2\uffe2\uff80\uff83\uffc2\uffb0C. Aboveground plant production was not affected by warming, and marginally reduced at near\uffe2\uff80\uff90ambient UVB only in the second season. Aboveground plant biomass also tended to have a lower C\uffe2\uff80\uff83:\uffe2\uff80\uff83N ratio under near\uffe2\uff80\uff90ambient UVB and was differently affected at the two temperatures (marginal UVB \uffc3\uff97 temperature interaction). Leaf decomposition of one dominant sedge species (Carex curta) tended to be faster at near\uffe2\uff80\uff90ambient UVB than at reduced UVB. Leaf decomposition of a codominant species (Carex decidua) was significantly faster at near\uffe2\uff80\uff90ambient UVB; root decomposition of this species tended to be lower at increased temperature and interacted with UVB. We found, for the first time in a field experiment that epigeic earthworm density and biomass was 36% decreased by warming but remained unaffected by UVB radiation. Our results show that present\uffe2\uff80\uff90day solar UVB radiation and modest warming can adversely affect ecosystem functioning and engineers of this fen. However, results on plant biomass production also showed that treatment manipulations of co\uffe2\uff80\uff90occurring global change factors can be overridden by the local climatic situation in a given study year.</p>", "keywords": ["DECOMPOSITION", "EARTHWORMS", "0106 biological sciences", "CAREX CURTA", "ECOSYSTEM FUNCTIONING", "04 agricultural and veterinary sciences", "15. Life on land", "BIOMASS PRODUCTION", "SOIL HETEROTROPHS", "01 natural sciences", "CAREX DECIDUA", "13. Climate action", "DENDROBAENA OCTAEDRA", "https://purl.org/becyt/ford/1.6", "0401 agriculture", " forestry", " and fisheries", "GLOBAL WARMING", "GLOBAL CHANGE", "OZONE DEPLETION", "https://purl.org/becyt/ford/1"]}, "links": [{"href": "https://doi.org/10.1111/j.1365-2486.2009.01970.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": "10.1111/j.1365-2486.2009.01970.x", "name": "item", "description": "10.1111/j.1365-2486.2009.01970.x", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1111/j.1365-2486.2009.01970.x"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2009-09-04T00:00:00Z"}}, {"id": "10.1111/j.1461-0248.2009.01352.x", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-04-04T16:19:15Z", "type": "Journal Article", "created": "2009-07-23", "title": "Shrub Encroachment Can Reverse Desertification In Semi-Arid Mediterranean Grasslands", "description": "Abstract<p>The worldwide phenomenon of shrub encroachment in grass\uffe2\uff80\uff90dominated dryland ecosystems is commonly associated with desertification. Studies of the purported desertification effects associated with shrub encroachment are often restricted to relatively few study areas, and document a narrow range of possible impacts upon biota and ecosystem processes. We conducted a study in degraded Mediterranean grasslands dominated by Stipa tenacissima to simultaneously evaluate the effects of shrub encroachment on the structure and composition of multiple biotic community components, and on various indicators of ecosystem function. Shrub encroachment enhanced vascular plant richness, biomass of fungi, actinomycetes and other bacteria, and was linked with greater soil fertility and N mineralization rates. While shrub encroachment may be a widespread phenomenon in drylands, an interpretation that this is an expression of desertification is not universal. Our results suggest that shrub establishment may be an important step in the reversal of desertification processes in the Mediterranean region.</p>", "keywords": ["0106 biological sciences", "2. Zero hunger", "Mediterranean Region", "Shrub encroachment", "Mediterranean", "15. Life on land", "01 natural sciences", "Soil", "Stipa tenacissima", "Semi-arid", "13. Climate action", "Ecosystem functioning", "Desert Climate", "Plant successional dynamics", "Global change", "Desertification", "Ecosystem", "Plant Physiological Phenomena"]}, "links": [{"href": "https://doi.org/10.1111/j.1461-0248.2009.01352.x"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Ecology%20Letters", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1111/j.1461-0248.2009.01352.x", "name": "item", "description": "10.1111/j.1461-0248.2009.01352.x", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1111/j.1461-0248.2009.01352.x"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2009-08-13T00:00:00Z"}}, {"id": "10.14279/depositonce-15380", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-04T16:19:53Z", "type": "Journal Article", "created": "2022-02-24", "title": "Decoupling between ecosystem photosynthesis and transpiration: a last resort against overheating", "description": "Abstract                <p>Ecosystems are projected to face extreme high temperatures more frequently in the near future. Various biotic coping strategies exist to prevent heat stress. Controlled experiments have recently provided evidence for continued transpiration in woody plants during high air temperatures, even when photosynthesis is inhibited. Such a decoupling of photosynthesis and transpiration would represent an effective strategy (\uffe2\uff80\uff98known as leaf or canopy cooling\uffe2\uff80\uff99) to prevent lethal leaf temperatures. At the ecosystem scale, continued transpiration might dampen the development and propagation of heat extremes despite further desiccating soils. However, at the ecosystem scale, evidence for the occurrence of this decoupling is still limited. Here, we aim to investigate this mechanism using eddy-covariance data of thirteen woody ecosystems located in Australia and a causal graph discovery algorithm. Working at half-hourly time resolution, we find evidence for a decoupling of photosynthesis and transpiration in four ecosystems which can be classified as Mediterranean woodlands. The decoupling occurred at air temperatures above 35 \uffe2\uff88\uff98C. At the nine other investigated woody sites, we found that vegetation CO2 exchange remained coupled to transpiration at the observed high air temperatures. Ecosystem characteristics suggest that the canopy energy balance plays a crucial role in determining the occurrence of a decoupling. Our results highlight the value of causal-inference approaches for the analysis of complex physiological processes. With regard to projected increasing temperatures and especially extreme events in future climates, further vegetation types might be pushed to threatening canopy temperatures. Our findings suggest that the coupling of leaf-level photosynthesis and stomatal conductance, common in land surface schemes, may need be re-examined when applied to high-temperature events.</p>", "keywords": ["heat wave", "570", "AUSTRALIA", "Science", "QC1-999", "UNCERTAINTY", "Environmental technology. Sanitary engineering", "01 natural sciences", "transpiration", "FLUX TOWER", "ddc:570", "GE1-350", "TOLERANCE", "TEMPERATURE", "TD1-1066", "0105 earth and related environmental sciences", "photosynthesis", "CONDUCTANCE", "Physics", "Q", "04 agricultural and veterinary sciences", "15. Life on land", "WATER-USE", "MODEL", "Environmental sciences", "13. Climate action", "Earth and Environmental Sciences", "ecosystem functioning", "PINUS-TAEDA", "0401 agriculture", " forestry", " and fisheries", "ELEVATED CO2", "570 Biowissenschaften; Biologie"]}, "links": [{"href": "https://doi.org/10.14279/depositonce-15380"}, {"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": "10.14279/depositonce-15380", "name": "item", "description": "10.14279/depositonce-15380", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.14279/depositonce-15380"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2022-03-14T00:00:00Z"}}, {"id": "10.1371/journal.pone.0087975", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-04-04T16:19:51Z", "type": "Journal Article", "created": "2014-02-03", "title": "Nitrogen Deposition Enhances Carbon Sequestration By Plantations In Northern China", "description": "Open Access\u062d\u0638\u064a \u062a\u0631\u0633\u0628 \u0627\u0644\u0646\u064a\u062a\u0631\u0648\u062c\u064a\u0646 \u0648\u0622\u062b\u0627\u0631\u0647 \u0627\u0644\u0628\u064a\u0626\u064a\u0629 \u0639\u0644\u0649 \u0627\u0644\u0646\u0638\u0645 \u0627\u0644\u0625\u064a\u0643\u0648\u0644\u0648\u062c\u064a\u0629 \u0644\u0644\u063a\u0627\u0628\u0627\u062a \u0628\u0627\u0647\u062a\u0645\u0627\u0645 \u0639\u0627\u0644\u0645\u064a. \u062a\u0644\u0639\u0628 \u0627\u0644\u0645\u0632\u0627\u0631\u0639 \u062f\u0648\u0631\u064b\u0627 \u0645\u0647\u0645\u064b\u0627 \u0641\u064a \u0627\u0644\u062a\u062e\u0641\u064a\u0641 \u0645\u0646 \u062a\u063a\u064a\u0631 \u0627\u0644\u0645\u0646\u0627\u062e 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\u0630\u0627\u062a\u064a \u0627\u0644\u062a\u063a\u0630\u064a\u0629 (AR) \u0648\u0644\u0643\u0646 \u062a\u0646\u0641\u0633 \u063a\u064a\u0631\u064a \u0627\u0644\u062a\u063a\u0630\u064a\u0629 (HR) \u0627\u0646\u062e\u0641\u0636 \u0641\u064a N \u0639\u0627\u0644\u064a\u0629 \u0645\u0642\u0627\u0631\u0646\u0629 \u0628\u0645\u062e\u0637\u0637\u0627\u062a N \u0627\u0644\u0645\u062a\u0648\u0633\u0637\u0629\u060c \u0639\u0644\u0649 \u0627\u0644\u0631\u063a\u0645 \u0645\u0646 \u0623\u0646 HR \u0641\u064a \u0645\u062e\u0637\u0637\u0627\u062a N \u0639\u0627\u0644\u064a\u0629 \u0648\u0645\u062a\u0648\u0633\u0637\u0629 \u0644\u0645 \u062a\u062e\u062a\u0644\u0641 \u0627\u062e\u062a\u0644\u0627\u0641\u064b\u0627 \u0643\u0628\u064a\u0631\u064b\u0627 \u0639\u0646 \u062a\u0644\u0643 \u0627\u0644\u0645\u0648\u062c\u0648\u062f\u0629 \u0641\u064a \u0627\u0644\u062a\u062d\u0643\u0645. \u0642\u062f \u062a\u0646\u0628\u0639 \u0632\u064a\u0627\u062f\u0629 \u0627\u0644\u0648\u0627\u0642\u0639 \u0627\u0644\u0645\u0639\u0632\u0632 \u0645\u0646 \u0627\u0644\u062a\u0646\u0641\u0633 \u0627\u0644\u0641\u0637\u0631\u064a \u0627\u0644\u062c\u0630\u0631\u064a \u0648\u0627\u0644\u062a\u0646\u0641\u0633 \u0627\u0644\u0645\u064a\u0643\u0631\u0648\u0628\u064a \u0627\u0644\u062c\u0630\u0631\u060c \u0648\u0644\u064a\u0633 \u062a\u0646\u0641\u0633 \u0627\u0644\u062c\u0630\u0631 \u0627\u0644\u062d\u064a\u060c \u0644\u0623\u0646 \u0627\u0644\u0643\u062a\u0644\u0629 \u0627\u0644\u062d\u064a\u0648\u064a\u0629 \u0644\u0644\u062c\u0630\u0631 \u0627\u0644\u0646\u0627\u0639\u0645 \u0648\u062a\u0631\u0643\u064a\u0632\u0627\u062a N \u0644\u0645 \u062a\u0638\u0647\u0631 \u0623\u064a \u0627\u062e\u062a\u0644\u0627\u0641\u0627\u062a \u0643\u0628\u064a\u0631\u0629. \u0639\u0644\u0649 \u0627\u0644\u0631\u063a\u0645 \u0645\u0646 \u0642\u0645\u0639 \u0627\u0644\u0645\u0648\u0627\u0631\u062f \u0627\u0644\u0628\u0634\u0631\u064a\u0629 \u0628\u0634\u0643\u0644 \u0643\u0628\u064a\u0631 \u0641\u064a \u0627\u0644\u0645\u0624\u0627\u0645\u0631\u0627\u062a \u0639\u0627\u0644\u064a\u0629 \u0627\u0644\u0646\u064a\u062a\u0631\u0648\u062c\u064a\u0646\u060c \u0625\u0644\u0627 \u0623\u0646 \u0627\u0644\u0643\u062a\u0644\u0629 \u0627\u0644\u062d\u064a\u0648\u064a\u0629 \u0627\u0644\u0645\u064a\u0643\u0631\u0648\u0628\u064a\u0629 \u0644\u0644\u062a\u0631\u0628\u0629 \u0623\u0648 \u062a\u0643\u0648\u064a\u0646\u0647\u0627 \u0623\u0648 \u0646\u0634\u0627\u0637 \u0627\u0644\u0625\u0646\u0632\u064a\u0645\u0627\u062a \u062e\u0627\u0631\u062c \u0627\u0644\u062e\u0644\u064a\u0629 \u0644\u0645 \u062a\u062a\u063a\u064a\u0631 \u0628\u0634\u0643\u0644 \u0643\u0628\u064a\u0631. \u0643\u0645\u0627 \u0623\u0646 \u0627\u0646\u062e\u0641\u0627\u0636 \u062f\u0631\u062c\u0629 \u0627\u0644\u062d\u0645\u0648\u0636\u0629 \u0645\u0639 \u0627\u0644\u0625\u062e\u0635\u0627\u0628 \u0644\u0627 \u064a\u0645\u0643\u0646 \u0623\u0646 \u064a\u0641\u0633\u0631 \u0646\u0645\u0637 \u0627\u0644\u0645\u0648\u0627\u0631\u062f \u0627\u0644\u0628\u0634\u0631\u064a\u0629. \u0642\u062f \u064a\u0643\u0648\u0646 \u0627\u0646\u062e\u0641\u0627\u0636 \u0627\u0644\u0645\u0648\u0627\u0631\u062f \u0627\u0644\u0628\u0634\u0631\u064a\u0629 \u0645\u0631\u062a\u0628\u0637\u064b\u0627 \u0628\u0643\u0641\u0627\u0621\u0629 \u0627\u0644\u0627\u0633\u062a\u062e\u062f\u0627\u0645 \u0627\u0644\u0645\u064a\u0643\u0631\u0648\u0628\u064a \u0627\u0644\u0645\u062a\u063a\u064a\u0631 C. \u062a\u0645 \u062a\u0639\u0632\u064a\u0632 \u0627\u0644\u0633\u064a\u0627\u0633\u0629 \u0627\u0644\u0627\u0642\u062a\u0635\u0627\u062f\u064a\u0629 \u0627\u0644\u062c\u062f\u064a\u062f\u0629 \u0628\u0634\u0643\u0644 \u0643\u0628\u064a\u0631 \u0645\u0646 \u062e\u0644\u0627\u0644 \u0625\u0636\u0627\u0641\u0629 N\u060c \u0645\u0646 149 \u0625\u0644\u0649 426.6\u062c\u0645 \u0645\u0643\u0639\u0628\u0644\u0643\u0644 \u0633\u0646\u0629. \u0642\u062f \u062a\u0624\u062f\u064a \u0625\u0636\u0627\u0641\u0629 N \u0642\u0635\u064a\u0631\u0629 \u0627\u0644\u0623\u062c\u0644 \u0625\u0644\u0649 \u062a\u0639\u0632\u064a\u0632 \u062f\u0648\u0631 \u0627\u0644\u0645\u0632\u0627\u0631\u0639 \u0628\u0634\u0643\u0644 \u0643\u0628\u064a\u0631 \u0643\u0645\u063a\u0633\u0644\u0629 C \u0645\u0647\u0645\u0629.", "keywords": ["Biomass (ecology)", "Carbon sequestration", "0106 biological sciences", "Organic chemistry", "Carbon Dynamics in Peatland Ecosystems", "Plant Roots", "01 natural sciences", "Agricultural and Biological Sciences", "Soil", "Biomass", "2. Zero hunger", "Global and Planetary Change", "Ecology", "Primary production", "Respiration", "Q", "R", "Life Sciences", "Agriculture", "Soil respiration", "Chemistry", "Physical Sciences", "Heterotroph", "Environmental chemistry", "Medicine", "Seasons", "Nitrogen Deposition", "Ecosystem Functioning", "Research Article", "Carbon Sequestration", "Autotroph", "Nitrogen", "Science", "Cell Respiration", "Soil Science", "Plant litter", "Environmental science", "Litter", "Genetics", "Soil Carbon Sequestration", "Biology", "Ecosystem", "Bacteria", "Global Forest Drought Response and Climate Change", "Botany", "Carbon Dioxide", "15. Life on land", "Agronomy", "13. Climate action", "FOS: Biological sciences", "Environmental Science", "Soil Carbon Dynamics and Nutrient Cycling in Ecosystems", "Animal science"], "contacts": [{"organization": "Zhenmin Du, Wei Wang, Wenjing Zeng, Hui Zeng,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.1371/journal.pone.0087975"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/PLoS%20ONE", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1371/journal.pone.0087975", "name": "item", "description": "10.1371/journal.pone.0087975", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1371/journal.pone.0087975"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2014-02-03T00:00:00Z"}}, {"id": "10.1371/journal.pone.0092985", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-04-04T16:19:51Z", "type": "Journal Article", "created": "2014-03-25", "title": "Comparison Of Seasonal Soil Microbial Process In Snow-Covered Temperate Ecosystems Of Northern China", "description": "Open AccessMore than half of the earth's terrestrial surface currently experiences seasonal snow cover and soil frost. Winter compositional and functional investigations in soil microbial community are frequently conducted in alpine tundra and boreal forest ecosystems. However, little information on winter microbial biogeochemistry is known from seasonally snow-covered temperate ecosystems. As decomposer microbes may differ in their ability/strategy to efficiently use soil organic carbon (SOC) within different phases of the year, understanding seasonal microbial process will increase our knowledge of biogeochemical cycling from the aspect of decomposition rates and corresponding nutrient dynamics. In this study, we measured soil microbial biomass, community composition and potential SOC mineralization rates in winter and summer, from six temperate ecosystems in northern China. Our results showed a clear pattern of increased microbial biomass C to nitrogen (N) ratio in most winter soils. Concurrently, a shift in soil microbial community composition occurred with higher fungal to bacterial biomass ratio and gram negative (G-) to gram positive (G+) bacterial biomass ratio in winter than in summer. Furthermore, potential SOC mineralization rate was higher in winter than in summer. Our study demonstrated a distinct transition of microbial community structure and function from winter to summer in temperate snow-covered ecosystems. Microbial N immobilization in winter may not be the major contributor for plant growth in the following spring.", "keywords": ["Biomass (ecology)", "Atmospheric Science", "Microbial population biology", "Decomposer", "Nutrient cycle", "Physical Phenomena", "Agricultural and Biological Sciences", "Soil", "Terrestrial ecosystem", "Snow", "Soil water", "Biomass", "Phospholipids", "Soil Microbiology", "Minerals", "Glucan 1", "4-beta-Glucosidase", "Ecology", "Geography", "Mineralization (soil science)", "Q", "R", "Life Sciences", "04 agricultural and veterinary sciences", "Biogeochemistry", "16. Peace & justice", "Earth and Planetary Sciences", "Physical Sciences", "Medicine", "Seasons", "Ecosystem Functioning", "Research Article", "China", "Nitrogen", "Science", "Soil Science", "Biogeochemical cycle", "Environmental science", "Meteorology", "Genetics", "Arctic Permafrost Dynamics and Climate Change", "Tundra", "Biology", "Ecosystem", "Soil science", "Bacteria", "Fungi", "Microbial Diversity in Antarctic Ecosystems", "15. Life on land", "Carbon", "Temperate climate", "13. Climate action", "FOS: Biological sciences", "Environmental Science", "0401 agriculture", " forestry", " and fisheries", "Soil Carbon Dynamics and Nutrient Cycling in Ecosystems"], "contacts": [{"organization": "Xinyue Zhang, Wei Wang, Weile Chen, Naili Zhang, Hui Zeng,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.1371/journal.pone.0092985"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/PLoS%20ONE", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1371/journal.pone.0092985", "name": "item", "description": "10.1371/journal.pone.0092985", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1371/journal.pone.0092985"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2014-03-25T00:00:00Z"}}, {"id": "10.5061/dryad.9ghx3ffpz", "type": "Feature", "geometry": null, "properties": {"license": "unspecified", "updated": "2026-04-04T16:21:55Z", "type": "Dataset", "created": "2023-10-24", "title": "The functional significance of tree species diversity in European forests - the FunDivEUROPE dataset", "description": "unspecifiedGeneral design  The FunDivEUROPE project,  short for 'Functional Significance of Forest Biodiversity in  Europe,' aimed at exploring the intricate relationships between  forest biodiversity and ecosystem functioning, focusing specifically on  European forests (Baeten et al., 2019; Baeten et al., 2013; Ratcliffe et  al., 2017; van der Plas et al., 2016a; van der Plas et al., 2016b; van der  Plas et al., 2018). In total, 209 mature forest plots measuring 30 x 30  meters were located in six European countries, ranging from boreal to  Mediterranean zones, and with each representing a major European forest  type: Finland (28 plots, boreal forest), Poland (43 plots, hemiboreal  forest), Germany (38 plots, temperate deciduous forest), Romania (28  plots, mountainous deciduous forest), Italy (36 plots, thermophilous  deciduous forest), and Spain (36 plots, Mediterranean mixed forest). These  plots were primarily established to investigate the role of the richness  of regionally common and economically important \u2018target\u2019 species on  ecosystem functioning and were hence selected to differ as much as  possible in the richness of these. Plot selection was aimed at mimicking  the design of a biodiversity experiment, in which variation in environment  is minimized and diversity is not confounded with composition, as in most  observational studies of diversity. Hence, plots were carefully selected  so that correlations between tree species richness and community  composition, topography (slope, altitude), and potentially confounding  soil factors (texture, depth, pH) were minimized, thus ensuring robust  tests of diversity-ecosystem function relationships (comparative study  design). Most forest plots were historically used for timber production  but are now managed by low-frequency thinning or with minimal  intervention. Hence, species compositions and diversity patterns in  forests are predominantly management-driven and/or are the result of  random species assembly, from the regional species pool. All sites are  considered as mature forests. In total, there were 15 target  species across all 209 plots, and plots were selected so that almost all  possible combinations of these target species were realized. Target  species contributed to more than 90% of the tree biomass in the plots and  therefore we expected them to be most important for ecosystem functioning.  Richness levels of one, two, three, four, and five target species were  replicated 56, 67, 54, 29, and 3 times, respectively, across countries,  and most possible target species compositions were realized. For the  majority of species combinations, we included two or more \u201crealizations\u201d  (not strict replicates, because species abundances differ), which allows  for comparing the importance of species diversity with that of species  composition for this subset of plots. At each richness level, each target  tree species was present in at least one plot, allowing us to  statistically test for the effects of presence/absence of species on  ecosystem functioning. Since species evenness might also affect ecosystem  functioning, all plots were selected to have target species with similar  abundances (with Pielou\u2019s evenness values above 0.6 in &gt; 91% of the  plots). To reach this goal, we <em>a priori</em> decided to  exclude locally rare target species (&lt;2 individuals per plot) in  richness measures. To describe community composition and to estimate  biomass values of each tree in each plot, we identified all stems \u22657.5 cm  in diameter to species and permanently marked them (12,939 stems in  total). More details about the design of the FunDivEUROPE plot network can  be found in Baeten et al. (2013). We determined a high number of basic  data for each of the 209 plots, describing geographic and  geomorphological, as well as soil and bedrock characteristics, see also  Ratcliffe et al (2017). Soil pH was determined in the same samples used  for C and N determination (see below) with a 0.01M  CaCl<sub>2</sub> solution at a ratio of 1:2.5 using a 827 pH  labs Metrohm AG, Herisau, Switzerland; see details in Dawud et al. (2017).  For each plot, we extracted mean annual temperature, temperature  seasonality (standard deviation of mean monthly temperatures), annual  precipitation, and precipitation seasonality (standard deviation of mean  monthly precipitation) from the WorldClim dataset (interpolated from  measurements taken between 1960 and to 1990 and at a spatial resolution of  one square kilometer) and the slope from the GTOPO30\u2014digital elevation  model with a spatial resolution of one square kilometer (data available  from the U.S. Geological Survey); see details in Kambach et al. (2019). We  further quantified several measures of tree diversity, based on the  initial inventory made in each plot, see Baeten et al. (2013). Short  description of all these variables are available in the \u201cMetadata\u201d sheet  of the data file. Ecosystem functions  methodology A major strength of the FunDivEUROPE  project was the general philosophy to measure all ecosystem functions in  all plots, following the same protocol by the same observers across the  six forest types. Measurements are thus directly comparable across plots  and show high coverage. In each of the 209 plots, 27  ecosystem functions were measured. The functions were <em>a  priori</em> classified into six groups reflecting basic ecological  processes (groups 1 to 5 below), and which have established links to  supporting, provisioning, regulating, or cultural ecosystem services.  These functions were also used in Chao et al. (in press): Hill-Chao  numbers allow decomposing gamma-multifunctionality into alpha and beta  components. Ecology Letters. In addition, we quantified timber quality as  an additional ecosystem service. \u00a0 In the  following, we describe the methodology for each measured ecosystem  function/service. (For more details, see also Baeten et al., 2019;  Ratcliffe et al., 2017; van der Plas et al., 2016a; van der Plas et al.,  2016b; van der Plas et al., 2018), and other FunDivEUROPE publications  that focus on specific ecosystem properties and functions. Additional  datasets are stored in the FunDivEUROPE data portal  (https://data.botanik.uni-halle.de/fundiveurope/, logon required to view  most data; all metadata is publicly available). 1.  Nutrient and carbon cycling-related drivers (header in the data table in  parentheses): a.\u00a0\u00a0\u00a0\u00a0\u00a0\u00a0 Earthworm biomass: \u00a0Biomass of all earthworms [g m<sup>-2</sup>] (earthworm_biomass) Earthworm sampling was carried out in spring 2012 in Italy, Germany, and Finland, and in autumn 2012 in Poland, Romania, and Spain. Plots were divided in nine (10 x 10) m subplots. One sample per plot was taken in the center subplot. Sampling close to tree stems was avoided and whenever possible performed, in between multiple, different tree species. At each sampling point, earthworms were sampled by means of a combined method. First litter was handsorted over an area of (25 x 25) cm<sup>2</sup>. After litter removal over an enlarged area of 0.5 m\u00b2, ethological extraction using a mustard suspension was applied. Finally, hand sorting of a soil sample of (25 \u00d7 25) cm<sup>2</sup> and 20 cm depth was performed in the middle of the 0.5 m\u00b2 area. Earthworms were preserved in ethanol (70%) for two weeks, and transferred to a 5% formaldehyde solution for fixation (until constant weight), after which they were transferred to ethanol (70%) again for further preservation and identification. All worms were individually weighed, including gut content, and identified to species level. \u00a0Results per unit area of the three sampling techniques were summed to determine the total earthworm biomass per m\u00b2. For details on earthworm biomass measurements, we refer to De Wandeler et al. (2018; 2016). b.\u00a0\u00a0\u00a0\u00a0\u00a0 Fine woody debris: Number of snags and standing dead trees shorter than 1.3 m and thinner than 5 cm DBH, and all stumps and other dead wood pieces lying on the forest floor (fine_woody_debris) Fine woody debris (FWD) was measured in two circular subplots (radius of 7 m) located in the opposite corners of each plot. All standing dead trees thinner than 5 cm diameter at breast height and snags shorter than 1.3 m, and all stumps and other dead wood pieces lying on the forest floor, were surveyed. In this study, we used the number of FWD pieces in each plot. c.\u00a0\u00a0\u00a0\u00a0\u00a0\u00a0 Microbial biomass: Mineral soil (0\u20135cm layer) microbial biomass carbon [mg C kg<sup>-1</sup>] (microbial_biomass_mineral) For soil sampling, each of the 209 plots was divided into nine 10x10m subplots. A soil sample was taken from five of the nine subplots and mixed to obtain one representative composite sample from each plot. Forest floor and mineral soil horizons (0-5 cm) were sampled separately. Soils were sieved fresh (4mm), stored at 4\u00b0C and analyzed within two weeks. Sampling was performed in spring 2012 in Italy, Germany, and Finland, and in autumn 2012 in Poland, Romania, and Spain. No forest floor was collected from the plots in Germany. Soil microbial biomass C was determined by the chloroform fumigation extraction method, of 10g and 15g (organic and mineral soil, respectively) soil, followed by 0.5 M K<sub>2</sub>SO<sub>4</sub> extraction of both fumigated and unfumigated soils (soil:solution ratio, 1:5). Fumigations were carried out for three days in vacuum desiccators with alcohol-free chloroform. Extracts were filtered (Whatman n\u00b0 42), and dissolved organic carbon in fumigated and unfumigated extracts was measured with a Total Organic Carbon analyser (Labtoc, Pollution and Process Monitoring Limited, UK). Soil microbial biomass C was calculated by dividing the difference of total extract between fumigated and unfumigated samples with a kEC (extractable part of microbial biomass C after fumigation) of 0.45 for biomass C (Joergensen and Mueller, 1996). d.\u00a0\u00a0\u00a0\u00a0\u00a0 Soil carbon stocks: \u00a0Total soil carbon stock in forest floor and 0\u201310 cm mineral soil layer combined [Mg ha<sup>-1</sup>] (soil_c_ff_10) Soil sampling was carried out from May 2012 to October 2012 (i.e. Poland in May 2012, Spain in June 2012, Finland and Germany in August 2012, Romania in September 2012 and Italy in October 2012). Nine forest floor samples and nine cores of mineral soil were collected from each plot and these were subsequently pooled into one sample per plot by each soil layer, i.e. forest floor, 0\u201310cm and 10\u201320cm depths for samples from Germany, Finland, Italy, and Romania. For Poland, the fixed depth was extended to 20\u201330cm and 30\u201340 cm whereas for Spain it was only possible to sample up to the 0\u201310cm layer due to the stoniness of the site. We oven-dried the samples at 55\u00b0C to constant weight, sorted out stones and other materials, ground the forest floor first with a heavy-duty SM 2000-Retsch cutting mill, and we then took subsamples and ground it further into finer particles with a planetary ball mill (PM 400-Retsch) for six minutes at 280rpm. The mineral soil samples were sieved through 2mm diameter mesh. We carried out carbonate removal treatments for those soil samples whose pH value exceeded the threshold point and proved presence of carbonates when tested with a 4N HCl fizz test. We used 6% (w/v) H<sub>2</sub>SO<sub>3</sub> solution and followed the carbonate removal procedure described by\u00a0(Skjemstad and Baldock, 2007). We took subsamples and further ground it into finer particles with a planetary ball mill (PM 400-Retsch) for six minutes at 280 rpm before analyzing soil organic carbon (SOC) with a Thermo Scientific FLASH 2000 soil CN analyzer. Soil organic C stocks were estimated by multiplying the SOC concentrations with soil bulk density, relative root volume and relative stone volume using the formula described in Vesterdal et al., (2008). We also determined the moisture content of the soil samples by oven-dried subsamples at 105\u00b0C and the reported SOC stock is thus on 105\u00b0C dry weight basis.\u00a0 2. Nutrient cycling related processes a.\u00a0\u00a0\u00a0\u00a0\u00a0\u00a0 Litter decomposition: Decomposition of leaf litter using the litterbag methodology [% daily rate] (litter_decomp_day) Litter collection and litterbag construction Leaf litter from all target tree species of the cross-region exploratory platform was collected at tree species-specific peak leaf litter fall between October 2011 and November 2012. Except for the Finnish forests, where freshly fallen leaf litter was collected from the forest floor, litter was collected using suspended litter traps, which were regularly harvested at one to two-week intervals. In all cases, litter was collected nearby, but not within the experimental plots. Litter was then air-dried and stored until the preparation of the litterbags. Litterbags (15 x 15 cm) were constructed using polyethylene fabrics of two different mesh sizes. For the bottom side of the litterbags, we used a small mesh width of 0.5 x 0.5 mm in order to minimize losses of litter fragments, while for the upper side, we used a large mesh width of 5 x 8 mm to allow soil macrofauna access to the litter within bags. Litterbags were filled with 10 g of litter. For litter mixtures, litterbags were filled with equivalent proportion of each litter species. Subsamples of all litter species were weighed, dried at 65\u00b0C for 48 h and reweighed to get a 65\u00b0C dry mass correction factor. Litterbag incubation Within each experimental plot, three litterbags with the plot-specific litter type (either single litter species or specific mixtures) were placed on bare soil after the natural litter layer had been removed, and fixed to the soil by placing chicken wire on top of it. The litterbags were removed from the field when 50\u201360% of the initial litter mass of the region\u2019s fastest decomposing species was remaining (evaluated with an extra set of litterbags that were harvested regularly). As a consequence, the duration of litter decomposition varied among regions. This procedure ensured that litter was sampled at similar decomposition stages across all sites, facilitating meaningful comparisons of litter diversity effects. Litter processing Harvested litterbags were sent to Montpellier where they were dried at 65\u00b0C. Litter was cleaned of pieces of wood, stones or other foreign material that occasionally got into the litterbags. Litter was then weighed, ground to a particle size of 1 mm with a Cyclotec Sample Mill (Tecator, H\u00f6gan\u00e4s, Sweden). To correct for potential soil contamination during decomposition in the field, we determined the ash content of initial and final litter material on all samples and expressed litter mass loss on ash-free litter mass.\u00a0 Litter mass loss was expressed as the percentage of mass lost from each litterbag, calculated as followed: Mass Loss = 100 x (Initial (ash free) mass \u2013 Final (ash free) mass)/Initial (ash free) mass. For details on litter decomposition measurements, we refer to Joly et al. (2017; 2023). b.\u00a0\u00a0\u00a0\u00a0\u00a0 Nitrogen resorption efficiency: Difference in N content between green and senescent leaves divided by N content of green leaves [%] (nutrient_resorption_efficiency) In each plot, fresh leaf and needle samples were collected from the south-exposed sun crown of all dominant tree species during the growing season (June to August) of 2012 and 2013. Twigs with leaves and needles were cut down from six trees per species in the monocultures and from three trees per species in the mixtures. Depending on the local conditions, tree loppers, tree climbers, or ruffles were used for this purpose. The selected material was placed in paper bags and was either oven-dried or air-dried, depending on the facilities available. Furthermore, collection of leaves from the litter traps, as representative of senescent leaves, has been conducted at periods of maximum litterfall during 2012 and 2013. For this purpose, five litter traps per plot were established and the collected litter was separated into the different species it originated from (see \u201cLitter production\u201d below). All samples were ground and analysed for nitrogen and calcium content by means of Near Infra Red Spectroscopy (NIRS) as described in detail by Pollastrini et al. (2016a). For the calibration of the NIRS spectra for the Ca analysis, a subset of samples was analysed with an atom absorption spectrometer (AAS, iCE 3000 series, ThermoScientific, China). Nitrogen resorption efficiency was calculated as follows, taking into account the N content of green and senescent leaves: NRE(%) = 100 x ((N green leaves - N senescent leaves)/(N green leaves)) Furthermore, the estimated NRE was corrected in order to take into account the leaf mass loss occurring during senescence. Thus, NRE was corrected based on the Ca foliar concentration, since Ca is rather immobile and is not resorbed during senescence (Van Heerwaarden et al., 2003). To validate the correction of NRE based on Ca concentrations, the Mass Loss Correction Factors (MLCF) suggested by Vergutz et al. (2012) have also been used. c.\u00a0\u00a0\u00a0\u00a0\u00a0\u00a0 Soil C/N ratio: Soil C/N ratio in forest floor and 0\u201310 cm mineral soil layer combined (soil_cn_ff_10) Soil sampling was carried out between May 2012 and October 2012 in all the regions.\u00a0Nine forest floor samples were collected using a 25 x 25 cm wooden frame, and the mineral soil (0-10 cm layer) was sampled, after forest floor removal, using a cylindrical metal corer. Total soil carbon and nitrogen concentrations were measured with a Thermo Scientific FLASH 2000 soil CN analyser on the forest floor and 0-10 cm layer samples. For full details on soil carbon and nitrogen methodology see Dawud et al. (2017). d.\u00a0\u00a0\u00a0\u00a0\u00a0 Wood decomposition: Decomposition of flat wooden sticks placed on forest floor [% daily rate] (wood_decomp_day) Flat wooden sticks (wooden tongue depressors made of <em>Betula pendula</em> wood) were placed to decompose at each plot of the exploratory platform. Each wooden stick was initially weighed (average of 2.5 g). As the weighing was done on air-dry sticks, subsamples were weighed, dried at 65\u00b0C for 48 h and reweighed to get a 65\u00b0C dry mass correction factor. Within each plot, three wooden sticks were placed on the bare soil after the natural litter layer had been locally removed, and fixed to the soil by placing chicken wire on top of it. The wooden sticks stayed in the field for different durations among regions depending on the mass loss of the region\u2019s fastest decomposing litter species (target of 50 to 60 % mass remaining), that was placed in the field at the same time as the wooden sticks.\u00a0 After field exposure wooden sticks were harvested, dried at 65\u00b0C, and weighed. Mass loss of wooden sticks was expressed as the percentage of initial mass lost, calculated as followed: Mass Loss = 100 x (Initial mass \u2013 Final mass)/Initial mass. For details on wood decomposition measurements, we refer to Joly et al. (2017; 2023). 3. Primary production a.\u00a0\u00a0\u00a0\u00a0\u00a0\u00a0 Fine root biomass: Total biomass of living fine roots in forest floor and 0-10 mineral soil layer combined [g m<sup>-2</sup>] (root_biomass) On each plot for determining fine root biomass, nine soil samples were taken from a predefined grid. The sampling was done in the six countries during May-October 2012. The forest floor was sampled using a wooden frame of size 25 cm x 25 cm, and thereafter the mineral soil was sampled using a cylindrical metal corer with 36 mm of inside diameter. The mineral soil was sampled down to 20 cm, except for the plots in Poland (down to 40 cm) and in Spain (down to 10 cm). Samples were pooled by layer and plot into one sample. Living fine roots (diameter \u2264 2 mm) were separated from the soil samples by hand to two categories, tree roots and ground vegetation roots. After separation, the roots were washed with water to remove adhering soil. Subsequently, the roots were dried at 40\u00b0C until constant mass and weighed for biomass. The root biomass was corrected with a correction factor for soil stoniness (CFstones= 100-(% stones)/100), where the respective volumetric stoniness was estimated with the metal rod method (Tamminen and Starr, 1994) on each plot. For this study, total tree fine root biomass for each plot was calculated (g m<sup>-2</sup>) for the sampled soil layer (forest floor + sampled mineral soil). For further details, see also Fin\u00e9r et al. (2017). b.\u00a0\u00a0\u00a0\u00a0\u00a0 Leaf mass: Leaf Area Index (lai) As a proxy for the leaf mass of each plot, we used the Leaf Area Index (LAI), which is the projected leaf area per unit of ground area. Five measurements of LAI in each plot were carried out at two time points, either early in the morning (shortly before sunrise) or late in the evening (shortly after sunset) in order to work in the presence of diffuse solar radiation and thus reduce the effect of scattered blue light in the canopy. LAI measurements were carried out in early September 2012, before the beginning of leaf shedding, using a Plant Canopy Analyzer LAI-2000 (LI-Cor Inc., Nebraska). With the LAI-2000, the incident light above the canopy and the light transmission below the canopy were measured using one sensor with five fisheye light sensors (lenses), with central zenith angle of 7\u00b0,23\u00b0, 38\u00b0, 53\u00b0 and 68\u00b0 (LAI-2000 manual, Li-Cor). The protocol used in each plot consisted of five measurements within the plots (light transmission below the canopy), and five measurements outside the forest (as proxy of the light incidence above the canopy), in an open space that was in close proximity of the sampled plots. LAI data were processed using Li-Cor\u2019s FV2200 software (LI-COR Biogeosciences, Inc. 2010). The light transmittance measurements of the fifth ring were removed to minimise the boundary effects on LAI. The LAI value per plot was the mean value of the five measurements for each plot. \u00a0For full details of the LAI measurement, see Pollastrini et al., (2016a) c.\u00a0\u00a0\u00a0\u00a0\u00a0\u00a0 Litter production: Annual production of foliar litter dry mass [g] (leaf_litter_production) In each of the 209 plots, five geodetic litter traps of 0.5m\u00b2 collection surface were installed in a regular grid. The sampling period covered a whole year and litters were collected several times. Sampling frequency was irregular and depended on working capacity within a region and seasonality of litter production. The litter was pooled per plot, and stored in plastic bags for transportation from the field site to the local laboratories. After air-drying, litter samples were sorted by species and by different fractions for dry weighing and chemical analysis. The following fractions were used: foliar litter (leaves or needles), woody litter (twigs, branches, bark parts), reproductive litter (flowers, cones, fruits, seeds, fruit capsules, etc.), other (e.g. bud scales, indefinable or small parts). Here, only the foliar litter is reported. A subsample of all litter types per species and region was dried at 65\u00b0C to constant weight to determine the conversion factor from air-dried to oven-dried values of litter dry mass (g). d.\u00a0\u00a0\u00a0\u00a0\u00a0 Photosynthetic efficiency: Chlorophyll fluorescence methodology [ChlF] (photo_eff_tot) Photosynthetic efficiency was measured using chlorophyll fluorescence (ChlF). ChlF measurements were replicated on eight randomly chosen leaves per tree from both the top and the bottom of the crown. The measurements were done on the twigs after the dark adaptation (i.e. after a minimum of 4 hours in a black plastic bag, at ambient temperature). In evergreen conifers, chlorophyll fluorescence measurements were taken in the current year\u2019s needles (i.e. needles sprouted in 2012). For full details of the ChlF measurement see Pollastrini et al. (2016b). e.\u00a0\u00a0\u00a0\u00a0\u00a0\u00a0 Tree productivity: Annual aboveground wood production [Mg C ha<sup>-1</sup> yr<sup>-1</sup>] (tree_growth) Wood cores Tree ring data were used to reconstruct the past annually resolved wood production. Between March and October of 2012, bark-to-pith increment cores (5 mm in diameter) were collected for a subset of trees in each plot following a size-stratified random sampling approach (Jucker et al., 2014a). We cored 12 trees per plot in monocultures and six trees per species in mixtures (except in Poland, where only five cores per species were taken in all plots due to restrictions imposed by park authorities), for a total of 3138 cored trees. Short of coring all trees within a stand, this approach has been shown to provide the most reliable estimates of plot-level productivity when using tree ring data, as it ensured that the size distribution of each plot is adequately represented by the subsample. Wood cores were stored in polycarbonate sheeting and allowed to air dry before being mounted on wooden boards and sanded with progressively finer grit sizes. A high-resolution flatbed scanner (2400 dpi optical resolution) was then used to image the cores. \u00a0From tree rings to aboveground wood production We followed a four-step approach (i\u2013iv) to estimate temporal trends in aboveground wood production (AWP, in MgC ha<sup>-1</sup> yr<sup>-1</sup>) from tree ring data (Jucker et al., 2014a). i.\u00a0\u00a0\u00a0\u00a0\u00a0\u00a0\u00a0 Measuring growth increments from wood cores We measured yearly radial growth increments (mm yr<sup>-1</sup>) for each cored tree from the scanned images. To minimize measurement errors associated with incorrectly placed ring boundaries, we crossdated each sample against a species-level reference curve obtained by averaging all ring-width chronologies belonging to a given species from a given site. In this process, 188 cores which showed poor agreement with reference curves were excluded from further analysis, giving a final total of 2950 tree ring chronologies. Both radial growth measurements and crossdating were performed using CDendro (Cybis Elektronik &amp; Data, Saltsj\u00f6baden, Sweden). Here we report data from the five-year period between 2007 and 2011. ii. Converting diameter increments into biomass growth We combined radial increments and allometric functions to express the growth rate of individual trees in units of biomass. We calculated the average yearly biomass growth between 2007\u20132011 (G, kgC yr<sup>-1</sup>) of cored trees as G = (AGBt<sub>2</sub> \u2013 AGBt<sub>1</sub>)/ \u0394t, where AGBt<sub>2</sub> is the tree\u2019s biomass, estimated with equations presented in Jucker et al. (2014b) in the most recent time period (i.e., end of 2011) and AGBt<sub>1</sub> is its biomass at the previous time step (i.e., end of 2006), \u0394t and is the elapsed time (i.e., five years). AGBt<sub>1</sub> was estimated by replacing current diameter and height measurements used to fit biomass equations with past values. Past diameters were reconstructed directly from wood core samples by progressively subtracting each year\u2019s diameter increment. Height growth was estimated by using height-diameter functions to predict the past height of a tree based on its past diameter. iii. Modelling individual tree biomass growth We modelled the biomass growth of each species as a function of tree size, competition for light, species richness, and a random plot effect: log(G<sub>i</sub>) = \u03b1<sub>j[i]</sub> + \u03b2<sub>1</sub> x log(D<sub>i</sub>) + \u03b2<sub>2</sub> x CI<sub>i</sub> + \u03b2<sub>3</sub> x SR<sub>j</sub> + \u03b5<sub>i</sub>\u00a0 where G<sub>i</sub>, D<sub>i</sub> and CI<sub>i</sub> are, respectively, the biomass growth, stem diameter and crown illumination index of tree i growing in plot j; SR<sub>j</sub> is the species richness of plot j; \u03b1<sub>j</sub> is a species\u2019 intrinsic growth rate for a tree growing in plot j; \u03b2<sub>1-3</sub> are, respectively, a species\u2019 growth response to size, light availability and species richness; and \u03b5<sub>i</sub> is the residual error. The structure of the growth model is adapted from Jucker et al. (2014b) and was fitted using the lmer function in R. Model robustness was assessed both visually, by comparing plots of predicted vs observed growth, and through a combination of model selection and goodness-of-fit tests (AIC model comparison and R<sup>2</sup>). Across all species, individual growth models explained much of the variation in growth among trees (Jucker et al., 2014a). iv. Scaling up to plot-level AWP To quantify AWP at the plot level, we used the fitted growth models to estimate the biomass growth of all trees that had not been cored. For each plot, we then summed the biomass growth of all standing trees to obtain an estimate of AWP. Growth estimates were generated using the predict.lmer function in R. f.\u00a0\u00a0\u00a0\u00a0\u00a0\u00a0\u00a0 Tree biomass: Aboveground biomass of all trees [Mg C ha<sup>-1</sup>] (tree_biomass) In each plot, the aboveground biomass (AGB, Mg C ha<sup>-1</sup>) of all the individual trees was estimated using tree diameter and height measurements in combination with species-specific biomass functions (see above). Biomass estimates of the individual trees were then summed to quantify the plot-level tree biomass. g.\u00a0\u00a0\u00a0\u00a0\u00a0 Understorey biomass: Dry weight of all understorey vegetation in a quadrant [g] (total_understorey_weight) In three subplots in each plot (upper right, central, lower left), a quadrant of 5 m x 5 m was marked for identification and estimation of cover of understorey vascular plant species (both woody and non-woody). Within each quadrant, all understorey vegetation was identified to species and afterwards clipped in a zone of 0.5 m x 0.5 m, where vegetation was relatively abundant and the composition was representative of the whole quadrant. The biomass samples (g) were dried for 48 h at 70\u00b0C before weighing. 4 4.\u00a0Regeneration a.\u00a0\u00a0\u00a0\u00a0\u00a0\u00a0 Sapling growth: Growth of saplings up to 1.60 m tall [cm] (sapling_growth) Sapling growth measurements (cm) were taken in 2012 on a total of 30 saplings per species wherever possible. Saplings (up to 1.60 m tall) of all tree species in the regional species pool were selected in a subplot of 4x4 m located in the central part of the main plot. Sapling growth was quantified as the distance between the bud scars (internodes) along the main stem of the last five years (i.e. from 2007 to 2011), without considering the shoot of the current growing season. For details on the methodology, see Bastias et al. (2019). b.\u00a0\u00a0\u00a0\u00a0\u00a0 Tree seedling regeneration: Number of saplings up to 1.60 m tall (regeneration_seedlings) Field sampling for tree seedling regeneration was carried out at the same time and in the same subplot as the tree juvenile regeneration (see below). Tree seedling regeneration was quantified as the number of tree seedlings (i.e. less than a year old) of all tree species in the regional species pool. For details on the methodology, see Bastias et al. (2019). c.\u00a0\u00a0\u00a0\u00a0\u00a0\u00a0 Tree juvenile regeneration: Number of tree seedlings less than a year old (regeneration_juveniles) Field sampling to quantify regeneration was carried out in 2012, from April to late August, in a subplot of 4x4m (16m2) delimited in the central part of the main plot. Tree juvenile regeneration was quantified as the number of sapling trees of tree species in the regional species pool over one year old and up to 1.60 m tall. For details on the methodology, see Bastias et al. (2019). 5 5.\u00a0Resistance to disturbance a.\u00a0\u00a0\u00a0\u00a0\u00a0\u00a0 Resistance to drought: Difference in carbon isotope composition in wood cores between dry and wet years [\u2030] (wue) For each plot, we randomly selected six trees among the 12 largest ones (i.e. largest diameter at breast height, DBH). For the mixed plots, three trees per species were randomly selected among the six largest trees of each species. This selection was conducted as to only select dominant and/or co-dominant trees in order to avoid confounding factors related to light interception. From each selected tree, a wood core was extracted at breast height during the summers of 2012 and 2013. For each site, we selected two years with contrasting climatic conditions during the growing season (dry vs. wet year) during the 1997-2010 period, see Grossiord et al. (2014) for full details. Latewood samples from these two years were carefully extracted from each wood core. The late wood sections from a given year and a given species in a given plot were bulked and analyzed for their carbon isotope composition (\u03b4<sup>13</sup>C, \u2030) with a mass spectrometer. By only selecting latewood sections, we characterized the functioning of the trees during the second part of the growing season and avoided potential effects related to the remobilization of stored carbohydrates from the previous growing season or to a favorable spring climate. Plot-level \u03b4<sup>13</sup>C was calculated as the basal-area weighted average value of species-level \u03b4<sup>13</sup>C measurements. Soil drought exposure in each forest stand was calculated as the stand-level increase in carbon isotope composition of late wood from the wet to the dry year (\u0394\u03b4<sup>13</sup>CS). For more details on resistance to drought measurements, we refer to Grossiord et al. 2014 (2014). b.\u00a0\u00a0\u00a0\u00a0\u00a0 Resistance to insect damage: Foliage not damaged by insects [%] (resistance_insects) As for fungal pathogens sampling (see below), we estimated insect herbivory on six trees per species in monocultures and three trees per focal species in mixed forests. The herbivory assessment was done once, from late spring to early summer (see periods on fungal pathogens protocol below). The insect herbivory protocol was derived from the ICP Forests manual. It was adapted to better account for total insect damage by observing the whole tree crown, instead of the \u201cassessable crown\u201d only. Damage on the crown exposed to sunlight and in the shade was recorded separately, as foliar loss may be also due to competition for light or natural pruning in the shaded part, particularly in heliophilous tree species. We considered damage as leaf area loss or shoot mortality i.e. defoliation. To estimate herbivore impact, we compared the sampled trees to a \u201creference tree\u201d, i.e. a healthy tree with intact foliage in its vicinity. Using binoculars, we estimated the proportion of defoliation in the living crown (i.e. the crown excluding the dead branches) in both parts of the crown (sunlight-exposed PDL and in the shade PDS) and put the estimates in one out of seven percentage classes: 0%, 0.5-1%, 1-12.5%, 12.5-25%, 25-50%, 50-75% and &gt; 75% damage. The assessment was done from at least two sides of the crown to account for all damage. When a different score was attributed from different sides to a focal tree, the mean of damage class median was used. The total percent of defoliation was calculated as the natural logarithm of the sum of PDL and PDS. For further details on the methodology, see Guyot et al. (2016). c.\u00a0\u00a0\u00a0\u00a0\u00a0\u00a0 Resistance to mammal browsing: Twigs not damaged by browsers [%] (lack_browsing) All plots were sampled using four 5m x 5m subplots located in the same areas of each plot.\u00a0 Within each of the four 5x5m subplots each woody species individual was visually inspected for browsing damage (bitten twigs).\u00a0 When browsing was found, the species was recorded, an estimation of the percentage of twigs browsed (between a height of 0.5\u20132 m) was made (biomass removed), and the stem diameter (at the base) and upper and lower limits of browsing were recorded. With these data, a plot-level average of the percentage of twigs browsed was calculated, and resistance to mammal browsing was defined as 100 - % of twigs browsed. d.\u00a0\u00a0\u00a0\u00a0\u00a0 Resistance to pathogen damage: Foliage not damaged by pathogens [%] (no_pathogen_damage) Fungal pathogen damage was assessed over a two-week period at each plot during the growing period, over two years. Foliage was collected from Italy (June-July 2012), Germany (July 2012), Finland (August 2012), Spain (June 2013), Romania (July 2013), and Poland (July-August 2013). In each plot, the six trees with the largest DBH per species were selected for trees within monoculture plots, and three trees with the largest DBH per species for trees within mixture plots. Foliage (leaves and shoots) samples were collected from branches from two levels of the tree canopy (25-60 leaves and 10 current-year shoots per branch) for each focal tree species. The number of leaves sampled from each focal tree and the number of plots within each tree species richness levels are enumerated in Table S8 in van der Plas et al. (2016a).\u00a0 Visual assessments for fungal pathogen damages were conducted on fresh leaves within one day of sampling. Leaves and shoots were assessed for four classes of fungal damages: oak powdery mildew and leaf spots for the broadleaved tree species, and rust and needle cast for the conifer species. The number of leaves or shoots with the respective damages per tree was recorded, as well as the number of leaves and shoots free from fungal pathogen damage, i.e. healthy foliage. To obtain a value of healthy foliage at the plot level, the sum of all healthy foliage for all trees within the plot was calculated and this was divided by the total number of foliage replicates to acquire a plot-level proportion of healthy foliage. All assessments were conducted by one person to avoid observer bias. For details on the sampling effort, we refer to Nguyen et al.(2016). e.\u00a0\u00a0\u00a0\u00a0\u00a0\u00a0 Tree growth recovery: Ratio between post-drought growth and growth during the respective drought period (tree_growth_recovery) Following Lloret et al. (Lloret et al., 2011), growth recovery was defined as the ability to recover growth rates (see tree productivity section) after a decline in growth experienced during the low-growth period (see growth resistance section). It corresponds to the ratio between the average post-drought growth in the five years after a drought year and the growth during the respective low-growth year. Values less than 1 indicate a decline in growth after the drought year, while values greater than one indicate (partial) recovery. f.\u00a0\u00a0\u00a0\u00a0\u00a0\u00a0\u00a0 Tree growth resilience: Ratio between growth after and before the drought period (tree_growth_resilience) Following Lloret et al. (Lloret et al., 2011), growth resilience was defined as the capacity of the forest stand to return to pre-drought growth (see tree productivity section) levels after a drought and is estimated as the ratio between average growth in the five years after and before the low-growth period (see growth resistance section). g.\u00a0\u00a0\u00a0\u00a0\u00a0 Tree growth resistance: Ratio of tree growth during a drought period and growth during the previous five-year high-growth period (tree_growth_resistance) Following Lloret et al. (Lloret et al., 2011), growth resistance was quantified by comparing tree growth in a low-growth year to the mean growth in the preceding five years. The year with the lowest growth across the regions was 2003, with the exception of Germany and Spain, where the lowest growth was in 1998 and 2005, respectively. 1998 and 2003 were known as drought years across Europe, with the exception of Spain where 2005 was even drier. Growth resistance was defined as the reversal of the reduction in growth (methodology described in the tree productivity section) during the drought: as the ratio of growth during the low-growth year and the growth during the previous five-year high-growth period. The larger the value, the greater the resistance of tree growth to drought. h.\u00a0\u00a0\u00a0\u00a0\u00a0 Tree growth stability: Mean annual tree growth divided by standard deviation in annual tree growth between 1992 and 2011 (tree_growth_stability) Using the annual aboveground wood production (AWP, see tree productivity section above), for each plot the growth stability was calculated as: mean(AWP) / <em>sd(AWP)</em> where mean(AWP) is the temporal mean AWP and <em>sd(AWP)</em> is the standard deviation in AWP between 1992 and 2011. See Jucker <em>et al.</em> (2014) for more details. 6 6.\u00a0Timber quality a.\u00a0\u00a0\u00a0\u00a0\u00a0\u00a0 Stem quality: Mean plot silvicultural quality assessment based on stem characteristics (timber_quality) For timber quality measurements, in each plot, dendrometric data and externally visible stem characteristics were recorded. The silvicultural quality assessment was based on stem characteristics that can be measured and evaluated non-destructively and rapidly along with a measurement of potentially influencing factors at the tree- and stand-level. For each tree within a plot, total height, height of the crown base, height of the lowest dead branch (&gt; 1 cm diameter), and type of fork (or steeply angled branch) were measured. In addition, the presence of the following stem quality parameters was recorded: curving, stem lean, epicormic branching, coppicing, pathogenic, and other defects. Due to the multiple factors constituting stem quality and wood quality, a four-class stem quality grading scheme was used to aggregate all stem quality parameters collected for each tree into an appropriate stem quality score, allowing for the analysis of a single response variable across all regions, species diversity levels and compositions; see Table 1 in Benneter et al (2018), with quality class D=1 being the lowest, and class A=4 being the highest quality class. The assessment of stem quality parameters was limited to the butt log of the tree, which represented the lowest 5 meters of the stem for broadleaved tree species and a maximum of 10 meters from the stem base for conifers. Multiples of the 5-meter section were only considered if the second log showed at least quality class C=2, but only if the green crown base was above the section considered. It has been estimated that for most commercial species in Europe, these butt logs comprise up to 50-70 % (softwood) and 80-95 % (hardwood) of the total commercial tree value. Plot-level timber quality was then calculated as the average timber quality of all the individual trees. For further details, see Benneter et al. (2018). We further quantified the diversity of several forest-associated taxonomic groups (bats, birds, spiders, insects, earthworms, fungal pathogens, soil microbes, understorey plants, and their multi-diversity and multi-abundance/-activity indices) and many aspects of habitat quality (tree functional and structural diversity), in each plot; the respective data can be found here: Allan, E. et al. (2019). Tree diversity is key for promoting the diversity and abundance of forest\u2010associated taxa in Europe [Dataset]. Dryad. https://doi.org/10.5061/dryad.sf7m0cg22. See also: Ampoorter, E. et al. (2020) Tree diversity is key for promoting the diversity and abundance of forest-associated taxa in Europe. Oikos 129, 133-146. In addition, detailed measurements on soil fauna, properties, and functions have been quantified within the SoilForEUROPE project, see https://websie.cefe.cnrs.fr/soilforeurope/. References Baeten, L. et al., 2019. Identifying the tree species compositions that maximize ecosystem functioning in European forests. Journal of Applied Ecology, 56(3): 733-744. Baeten, L. et al., 2013. A novel comparative research platform designed to determine the functional significance of tree species diversity in European forests. Perspect Plant Ecol, 15: 281-291. Bastias, C.C., Mor\u00e1n-L\u00f3pez, T., Valladares, F. and Benavides, R., 2019. Seed size underlies the uncoupling in species composition between canopy and recruitment layers in European forests. Forest Ecol Manag, 449: 117471. Benneter, A., Forrester, D.I., Bouriaud, O., Dormann, C.F. and Bauhus, J., 2018. Tree species diversity does not compromise stem quality in major European forest types. Forest Ecol Manag, 422: 323-337. Dawud, S.M. et al., 2017. Tree species functional group is a more important driver of soil properties than tree species diversity across major European forest types. Functional Ecology, 31: 1153-1162. De Wandeler, H. et al., 2018. Tree identity rather than tree diversity drives earthworm communities in European forests. Pedobiologia, 67: 16-25. De Wandeler, H. et al., 2016. Drivers of earthworm incidence and abundance across European forests. Soil Biology and Biochemistry, 99: 167-178. Fin\u00e9r, L. et al., 2017. Conifer proportion explains fine root biomass more than tree species diversity and site factors in major European forest types. Forest Ecol Manag, 406(Supplement C): 330-350. Grossiord, C. et al., 2014. Tree diversity does not always improve resistance of forest ecosystems to drought. Proceedings of the National Academy of Sciences, 111(41): 14812-14815. Guyot, V., Castagneyrol, B., Vialatte, A., Deconchat, M. and Jactel, H., 2016. Tree diversity reduces pest damage in mature forests across Europe. Biology Letters, 12(4): 20151037. Joergensen, R.G. and Mueller, T., 1996. The fumigation-extraction method to estimate soil microbial biomass: Calibration of the kEN value. Soil Biology and Biochemistry, 28(1): 33-37. Joly, F.-X. et al., 2017. Tree species diversity affects decomposition through modified micro-environmental conditions across European forests. New Phytologist, 214: 1281-1293. Joly, F.-X., Scherer-Lorenzen, M. and H\u00e4ttenschwiler, S., 2023. Resolving the intricate role of climate in litter decomposition. Nature Ecology &amp; Evolution, 7(2): 214-223. Jucker, T., Bouriaud, O., Avacaritei, D. and Coomes, D.A., 2014a. Stabilizing effects of diversity on aboveground wood production in forest ecosystems: linking patterns and processes. Ecol Lett, 17(12): 1560\u20131569. Jucker, T. et al., 2014b. Competition for light and water play contrasting roles in driving diversity\u2013productivity relationships in Iberian forests. J Ecol, 102: 1202\u20131213. Kambach, S. et al., 2019. How do trees respond to species mixing in experimental compared to observational studies? Ecology and Evolution, 9(19): 11254-11265. Lloret, F., Keeling, E.G. and Sala, A., 2011. Components of tree resilience: Effects of successive low-growth episodes in old ponderosa pine forests. Oikos 120: 1909\u20131920. Nguyen, D. et al., 2016. Fungal disease incidence along tree diversity gradients depends on latitude in European forests. Ecology and Evolution, 6(8): 2426-2438. Pollastrini, M. et al., 2016a. Physiological significance of forest tree defoliation: results from a survey in a mixed forest in Tuscany (central Italy). Forest Ecology and Management 361: 170-178. Pollastrini, M. et al., 2016b. Taxonomic and ecological relevance of the chlorophyll a fluorescence signature of tree species in mixed European forests. New Phytologist, 212(1): 51-65. Ratcliffe, S. et al., 2017. Biodiversity and ecosystem functioning relations in European forests depend on environmental context. Ecol Lett, 20: 1414-1426. Skjemstad, J.O. and Baldock, J.A., 2007. Total and organic carbon. Soil sampling and methods of analysis. CRC Press, Boca Raton, FL. Tamminen, P. and Starr, M., 1994. Bulk density of forested mineral soils. Silva Fennica 28 (1): article id 5528. van der Plas, F. et al., 2016a. Jack-of-all-trades effects drive biodiversity-ecosystem multifunctionality relationships in European forests. Nature Communications, 7: 11109. van der Plas, F. et al., 2016b. Biotic homogenization can decrease landscape-scale forest multifunctionality. Proceedings of the National Academy of Sciences, 113(13): 3557-3562. van der Plas, F. et al., 2018. Continental mapping of forest ecosystem functions reveals a high but unrealised potential for forest multifunctionality. Ecol Lett, 21(1): 31-42. Van Heerwaarden, L.M., Toet, S. and Aerts, R., 2003. Current measures of nutrient resorption efficiency lead to a substantial underestimation of real resorption efficiency: facts and solutions. Oikos 101: 664-669. Vergutz, L., Manzoni, S., Porporato, A., Novais, R.F. and Jackson, R.B., 2012. Global resorption efficiencies and concentrations of carbon and nutrients in leaves of terrestrial plants. Ecological Monographs 82: 205-220. Vesterdal, L., Schmidt, I.K., Callesen, I., Nilsson, L.O. and Gundersen, P., 2008. Carbon and nitrogen in forest floor and mineral soil under six common European tree species. Forest Ecol Manag, 255(1): 35-48.", "keywords": ["Ecology", "FunDivEUROPE", "Biodiversity", "FOS: Earth and related environmental sciences", "15. Life on land", "6. Clean water", "multifunctionality", "13. Climate action", "FOS: Biological sciences", "11. Sustainability", "Ecosystem functioning", "14. Life underwater", "Ecology", " Evolution", " Behavior and Systematics", "Nature and Landscape Conservation"], "contacts": [{"organization": "Scherer-Lorenzen, Michael, Allan, Eric, Ampoorter, Evy, Avacaritiei, Daniel, Baeten, Lander, Barnoaiea, Ionut, Bastias, Cristina C., Bauhus, J\u00fcrgen, Benavides, Raquel, Benneter, Adam, Berger, Sigrid, Bonal, Damien, Bouriaud, Olivier, Bruelheide, Helge, Bussotti, Filippo, Carnol, Monique, Castagneyrol, Bastien, Che\u0107ko, Ewa, Coomes, David, Coppi, Andrea, Cosofret, Cosmin, Danila, Iulian, Dawud, Seid Muhie, De Wandeler, Hans, Domisch, Timo, Duduman, Gabriel, Fin\u00e9r, Leena, Fischer, Markus, Fotelli, Mariangela, Gessler, Arthur, Gimeno, Teresa E., Grossiord, Charlotte, Guyot, Virginie, H\u00e4ttenschwiler, Stephan, Jactel, Herv\u00e9, Jaroszewicz, Bogdan, Joly, Fran\u00e7ois\u2010Xavier, Jucker, Tommaso, Koricheva, Julia, L\u00f3pez-Quiroga, David, Milligan, Harriet, M\u00fcller, Sandra, Muys, Bart, Nguyen, Diem, Pollastrini, Martina, Rabasa, Sonia G., Radoglou, Kalliopi, Ratcliffe, Sophia, Raulund\u2010Rasmussen, Karsten, Ruiz\u2010Benito, Paloma, Seidl, Rupert, Seiferling, Ian, Selvi, Federico, Smerczy\u0144ski, Ireneusz, Stenlid, Jan, Valladares, Fernando, van der Plas, Fons, Verheyen, Kris, Vesterdal, Lars, von Wilpert, Klaus, Wirth, Christian, Zavala, Miguel A.,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.5061/dryad.9ghx3ffpz"}, {"rel": "self", "type": "application/geo+json", "title": "10.5061/dryad.9ghx3ffpz", "name": "item", "description": "10.5061/dryad.9ghx3ffpz", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.5061/dryad.9ghx3ffpz"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2023-11-06T00:00:00Z"}}, {"id": "10.5194/bg-12-5537-2015", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-04T16:22:06Z", "type": "Journal Article", "created": "2015-09-29", "title": "Responses Of Soil Microbial Communities And Enzyme Activities To Nitrogen And Phosphorus Additions In Chinese Fir Plantations Of Subtropical China", "description": "<p>Abstract. Nitrogen (N) and phosphorus (P) additions to forest ecosystems are known to influence various above-ground properties, such as plant productivity and composition, and below-ground properties, such as soil nutrient cycling. However, our understanding of how soil microbial communities and their functions respond to nutrient additions in subtropical plantations is still not complete. In this study, we added N and P to Chinese fir plantations in subtropical China to examine how nutrient additions influenced soil microbial community composition and enzyme activities. The results showed that most soil microbial properties were responsive to N and/or P additions, but responses often varied depending on the nutrient added and the quantity added. For instance, there were more than 30 % greater increases in the activities of \uffce\uffb2-glucosidase (\uffce\uffb2G) and N-acetyl-\uffce\uffb2-D-glucosaminidase (NAG) in the treatments that received nutrient additions compared to the control plot, whereas acid phosphatase (aP) activity was always higher (57 and 71 %, respectively) in the P treatment. N and P additions greatly enhanced the phospholipid fatty acids (PLFAs) abundance especially in the N2P (100 kg ha\uffe2\uff88\uff921 yr\uffe2\uff88\uff921 of N +50 kg ha\uffe2\uff88\uff921 yr\uffe2\uff88\uff921 of P) treatment; the bacterial PLFAs (bacPLFAs), fungal PLFAs (funPLFAs) and actinomycic PLFAs (actPLFAs) were about 2.5, 3 and 4 times higher, respectively, than in the CK (control). Soil enzyme activities were noticeably higher in November than in July, mainly due to seasonal differences in soil moisture content (SMC). \uffce\uffb2G or NAG activities were significantly and positively correlated with microbial PLFAs. These findings indicate that \uffce\uffb2G and NAG would be useful tools for assessing the biogeochemical transformation and metabolic activity of soil microbes. We recommend combined additions of N and P fertilizer to promote soil fertility and microbial activity in this kind of plantation.                     </p>", "keywords": ["Biogeochemical Cycling of Nutrients in Aquatic Ecosystems", "Microbial population biology", "Nitrogen", "Soil Science", "Organic chemistry", "Carbon Dynamics in Peatland Ecosystems", "Biochemistry", "Nutrient cycle", "Agricultural and Biological Sciences", "Life", "QH501-531", "Genetics", "Environmental Chemistry", "Biology", "QH540-549.5", "Ecosystem", "2. Zero hunger", "QE1-996.5", "Ecology", "Bacteria", "Nutrient Cycling", "Life Sciences", "Geology", "Phosphorus", "04 agricultural and veterinary sciences", "15. Life on land", "Agronomy", "6. Clean water", "Chemistry", "Phos", "Subtropics", "FOS: Biological sciences", "Environmental Science", "Physical Sciences", "0401 agriculture", " forestry", " and fisheries", "Soil Carbon Dynamics and Nutrient Cycling in Ecosystems", "Ecosystem Functioning", "Animal science", "Nutrient"], "contacts": [{"organization": "Wenyi Dong, X. Y. Zhang, X. Y. Liu, Xiaoli Fu, F. S. Chen, H. M. Wang, Xiaoming Sun, Xuefa Wen,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.5194/bg-12-5537-2015"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Biogeosciences", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.5194/bg-12-5537-2015", "name": "item", "description": "10.5194/bg-12-5537-2015", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.5194/bg-12-5537-2015"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2015-07-08T00:00:00Z"}}, {"id": "10.5194/gmd-10-3745-2017", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-04T16:22:16Z", "type": "Journal Article", "created": "2017-10-12", "title": "A representation of the phosphorus cycle for ORCHIDEE (revision\u00a04520)", "description": "<p>Abstract. Land surface models rarely incorporate the terrestrial phosphorus cycle and its interactions with the carbon cycle, despite the extensive scientific debate about the importance of nitrogen and phosphorus supply for future land carbon uptake. We describe a representation of the terrestrial phosphorus cycle for the ORCHIDEE land surface model, and evaluate it with data from nutrient manipulation experiments along a\uffc2\uffa0soil formation chronosequence in Hawaii.  ORCHIDEE accounts for the influence of the nutritional state of vegetation on tissue nutrient concentrations, photosynthesis, plant growth, biomass allocation, biochemical (phosphatase-mediated) mineralization, and biological nitrogen fixation. Changes in the nutrient content (quality) of litter affect the carbon use efficiency of decomposition and in return the nutrient availability to vegetation. The model explicitly accounts for root zone depletion of phosphorus as a function of root phosphorus uptake and phosphorus transport from the soil to the root surface.  The model captures the observed differences in the foliage stoichiometry of vegetation between an early (300-year) and a late (4.1\uffe2\uff80\uffafMyr) stage of soil development. The contrasting sensitivities of net primary productivity to the addition of either nitrogen, phosphorus, or both among sites are in general reproduced by the model. As observed, the model simulates a preferential stimulation of leaf level productivity when nitrogen stress is alleviated, while leaf level productivity and leaf area index are stimulated equally when phosphorus stress is alleviated. The nutrient use efficiencies in the model are lower than observed primarily due to biases in the nutrient content and turnover of woody biomass.  We conclude that ORCHIDEE is able to reproduce the shift from nitrogen to phosphorus limited net primary productivity along the soil development chronosequence, as well as the contrasting responses of net primary productivity to nutrient addition.                     </p>", "keywords": ["Biomass (ecology)", "Chronosequence", "Organic chemistry", "chronos\u00e9quence", "Plant Science", "mod\u00e8le", "Nitrogen cycle", "01 natural sciences", "Nutrient cycle", "Agricultural and Biological Sciences", "Soil water", "Pathology", "2. Zero hunger", "QE1-996.5", "Global and Planetary Change", "Orchidee", "Ecology", "Physics", "Life Sciences", "Geology", "Phosphorus", "Carbon cycle", "Chemistry", "nutrition", "Physical Sciences", "Medicine", "[SDU.STU.GP] Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph]", "Ecosystem Functioning", "Vegetation (pathology)", "cycle du carbone", "570", "[SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph]", "Nitrogen", "hawai", "Soil Science", "mod\u00e8le orchid\u00e9e", "Environmental science", "vegetation", "phosphore du sol", "Biology", "Ecosystem", "0105 earth and related environmental sciences", "Soil science", "Soil Fertility", "ddc:550", "Global Forest Drought Response and Climate Change", "surface terrestre", "Plant Nutrient Uptake and Signaling Pathways", "15. Life on land", "Agronomy", "hawaii", "13. Climate action", "FOS: Biological sciences", "Environmental Science", "Soil Carbon Dynamics and Nutrient Cycling in Ecosystems", "Nutrient"]}, "links": [{"href": "https://gmd.copernicus.org/articles/10/3745/2017/gmd-10-3745-2017.pdf"}, {"href": "https://doi.org/10.5194/gmd-10-3745-2017"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Geoscientific%20Model%20Development", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.5194/gmd-10-3745-2017", "name": "item", "description": "10.5194/gmd-10-3745-2017", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.5194/gmd-10-3745-2017"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2017-10-12T00:00:00Z"}}, {"id": "1959.7/uws:44389", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-04-04T16:25:44Z", "type": "Journal Article", "created": "2017-08-24", "title": "Alleviating Nitrogen Limitation in Mediterranean Maquis Vegetation Leads to Ecological Degradation", "description": "Abstract<p>Soils are being degraded at an alarming rate and thereby also crucial ecosystem goods and services. Nitrogen (N) enrichment is a major driver of this degradation. While the negative impacts of N enrichment on vegetation are well known globally, those on various ecological interactions, and on ecosystem functioning, remain largely unknown. Because Mediterranean ecosystems are N limited, they are good model systems for evaluating how N enrichment impacts not only vegetation but also ecological partnerships and ecosystem functioning. Using a 7\uffe2\uff80\uff90year N\uffe2\uff80\uff90manipulation (dose and form) field experiment running in a Mediterranean Basin maquis located in a region with naturally low ambient N deposition (&lt;4\uffc2\uffa0kg\uffc2\uffa0N\uffc2\uffa0ha\uffe2\uff88\uff921\uffc2\uffa0y\uffe2\uff88\uff921), we assessed the impacts of the N additions on (i) the dominant plant species (photosynthetic N\uffe2\uff80\uff90use efficiency); (ii) plant\uffe2\uff80\uff93soil ecological partnerships with ectomycorrhiza and N\uffe2\uff80\uff90fixing bacteria; and (iii) ecosystem degradation (plant\uffe2\uff80\uff93soil cover, biological mineral weathering and soil N fixation). N additions significantly disrupted plant\uffe2\uff80\uff93soil cover, plant\uffe2\uff80\uff93soil biotic interactions, and ecosystem functioning compared with ambient N deposition conditions. However, the higher the ammonium dose (alone or with nitrate), the more drastic these disruptions were. We report a critical threshold at 20\uffe2\uff80\uff9340\uffc2\uffa0kg ammonium ha\uffe2\uff88\uff921\uffc2\uffa0y\uffe2\uff88\uff921 whereby severe ecosystem degradation can be expected. These observations are critical to help explain the mechanisms behind ecosystem degradation, to describe the collective loss of organisms and multifunction in the landscape, and to predict potential fragmentation of Mediterranean maquis under conditions of unrelieved N enrichment. Copyright \uffc2\uffa9 2017 John Wiley &amp; Sons, Ltd.</p", "keywords": ["2. Zero hunger", "0106 biological sciences", "plant\u2013soil ecological partnerships", "04 agricultural and veterinary sciences", "Mediterranean", "15. Life on land", "01 natural sciences", "nitrogen", "ammonium", "soil degradation", "13. Climate action", "ecosystem functioning", "XXXXXX - Unknown", "Plant-soil ecological partnerships", "Ecosystem functioning", "ecosystem degradation", "0401 agriculture", " forestry", " and fisheries", "Ecosystem degradation", "ecosystems", "Ammonium"]}, "links": [{"href": "https://onlinelibrary.wiley.com/doi/pdf/10.1002/ldr.2784"}, {"href": "https://doi.org/1959.7/uws:44389"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Land%20Degradation%20%26amp%3B%20Development", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "1959.7/uws:44389", "name": "item", "description": "1959.7/uws:44389", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/1959.7/uws:44389"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2017-09-12T00:00:00Z"}}, {"id": "10138/576497", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-04-04T16:25:03Z", "type": "Journal Article", "title": "Soil BON Earthworm - A global initiative on earthworm distribution, traits, and spatiotemporal diversity patterns", "description": "Open AccessPeer reviewed", "keywords": ["2. Zero hunger", "temporal dynamics", "500", "soil biodiversity", "earthworms", "time-series data", "15. Life on land", "Traits", "Microbiology", "630", "QR1-502", "[SDE.BE] Environmental Sciences/Biodiversity and Ecology", "QL1-991", "Ecology", " evolutionary biology", "global collaboration", "ecosystem functioning", "citizen science", "Community ecology", "functional traits", "14. Life underwater", "[SDE.BE]Environmental Sciences/Biodiversity and Ecology", "Zoology", "community ecology"]}, "links": [{"href": "https://doi.org/10138/576497"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Soil%20Organisms", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10138/576497", "name": "item", "description": "10138/576497", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10138/576497"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2024-01-01T00:00:00Z"}}, {"id": "10141/623078", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-04-04T16:25:03Z", "type": "Journal Article", "created": "2022-11-12", "title": "Frontiers in soil ecology\u2014Insights from the World Biodiversity Forum 2022", "description": "Abstract<p>Global change is affecting soil biodiversity and functioning across all terrestrial ecosystems. Still, much is unknown about how soil biodiversity and function will change in the future in response to simultaneous alterations in climate and land use, as well as other environmental drivers. It is crucial to understand the direct, indirect\uffc2\uffa0and interactive effects of global change drivers on soil communities and ecosystems across environmental contexts, not only today but also in the near future. This is particularly relevant for international efforts to tackle climate change like the Paris Agreement, and considering the failure to achieve the 2020 biodiversity targets, especially the target of halting soil degradation. Here, we outline the main frontiers related to soil ecology that were presented and discussed at the thematic sessions of the World Biodiversity Forum 2022 in Davos, Switzerland. We highlight multiple frontiers of knowledge associated with data integration, causal inference, soil biodiversity and function scenarios, critical soil biodiversity facets, underrepresented drivers, global collaboration, knowledge application and transdisciplinarity, as well as policy and public communication. These identified research priorities are not only of immediate interest to the scientific community but may also be considered in research priority programmes and calls for funding.</p", "keywords": ["[SDE] Environmental Sciences", "0301 basic medicine", "570", "Agriculture (General)", "577", "soil biodiversity", "scenario modelling", "580 Plants (Botany)", "S1-972", "03 medical and health sciences", "10126 Department of Plant and Microbial Biology", "11. Sustainability", "Life Science", "GE1-350", "10211 Zurich-Basel Plant Science Center", "Biology", "soil macroecology", "Biodiversity change", "2. Zero hunger", "Soil macroecology", "0303 health sciences", "15. Life on land", "Scenario modelling", "Soil biodiversity", "6. Clean water", "Environmental sciences", "biodiversity change", "13. Climate action", "ecosystem functioning", "[SDE]Environmental Sciences", "Ecosystem functioning", "ta1181"]}, "links": [{"href": "https://onlinelibrary.wiley.com/doi/pdf/10.1002/sae2.12031"}, {"href": "https://doi.org/10141/623078"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Journal%20of%20Sustainable%20Agriculture%20and%20Environment", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10141/623078", "name": "item", "description": "10141/623078", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10141/623078"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2022-11-11T00:00:00Z"}}, {"id": "1959.7/uws:63733", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-04-04T16:25:45Z", "type": "Journal Article", "created": "2018-02-27", "title": "Temperature and aridity regulate spatial variability of soil multifunctionality in drylands across the globe", "description": "Abstract<p>The relationship between the spatial variability of soil multifunctionality (i.e., the capacity of soils to conduct multiple functions; SVM) and major climatic drivers, such as temperature and aridity, has never been assessed globally in terrestrial ecosystems. We surveyed 236 dryland ecosystems from six continents to evaluate the relative importance of aridity and mean annual temperature, and of other abiotic (e.g., texture) and biotic (e.g., plant cover) variables as drivers of SVM, calculated as the averaged coefficient of variation for multiple soil variables linked to nutrient stocks and cycling. We found that increases in temperature and aridity were globally correlated to increases in SVM. Some of these climatic effects on SVM were direct, but others were indirectly driven through reductions in the number of vegetation patches and increases in soil sand content. The predictive capacity of our structural equation\uffc2\uffa0modelling was clearly higher for the spatial variability of N\uffe2\uff80\uff90 than for C\uffe2\uff80\uff90 and P\uffe2\uff80\uff90related soil variables. In the case of N cycling, the effects of temperature and aridity were both direct and indirect via changes in soil properties. For C and P, the effect of climate was mainly indirect via changes in plant attributes. These results suggest that future changes in climate may decouple the spatial availability of these elements for plants and microbes in dryland soils. Our findings significantly advance our understanding of the patterns and mechanisms driving SVM in drylands across the globe, which is critical for predicting changes in ecosystem functioning in response to climate change.</p", "keywords": ["Abiotic component", "Atmospheric sciences", "Physical geography", "Arid", "Climate Change", "Soil Science", "Spatial variability", "Environmental science", "Agricultural and Biological Sciences", "Soil", "Biodiversity Conservation and Ecosystem Management", "Soil texture", "Aridity index", "XXXXXX - Unknown", "Soil water", "FOS: Mathematics", "Pathology", "Climate change", "Biology", "Ecosystem", "Nature and Landscape Conservation", "Soil science", "2. Zero hunger", "Global and Planetary Change", "Soil Fertility", "Ecology", "Geography", "Global Forest Drought Response and Climate Change", "Statistics", "Temperature", "Life Sciences", "Cycling", "Geology", "FOS: Earth and related environmental sciences", "04 agricultural and veterinary sciences", "Plants", "15. Life on land", "Archaeology", "13. Climate action", "FOS: Biological sciences", "Environmental Science", "Physical Sciences", "Medicine", "0401 agriculture", " forestry", " and fisheries", "Soil Carbon Dynamics and Nutrient Cycling in Ecosystems", "Ecosystem Functioning", "Vegetation (pathology)", "Mathematics"]}, "links": [{"href": "https://eprints.whiterose.ac.uk/128150/8/Dur-n_et_al-2018-Ecology.pdf"}, {"href": "https://esajournals.onlinelibrary.wiley.com/doi/pdf/10.1002/ecy.2199"}, {"href": "https://doi.org/1959.7/uws:63733"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Ecology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "1959.7/uws:63733", "name": "item", "description": "1959.7/uws:63733", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/1959.7/uws:63733"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2018-05-01T00:00:00Z"}}, {"id": "1959.7/uws:77720", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-04-04T16:25:47Z", "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/1959.7/uws:77720"}, {"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": "1959.7/uws:77720", "name": "item", "description": "1959.7/uws:77720", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/1959.7/uws:77720"}, {"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": "20.500.11815/1261", "type": "Feature", "geometry": null, "properties": {"updated": "2026-04-04T16:25:53Z", "type": "Journal Article", "created": "2018-10-24", "title": "Using research networks to create the comprehensive datasets needed to assess nutrient availability as a key determinant of terrestrial carbon cycling", "description": "Open AccessA wide range of research shows that nutrient availability strongly influences terrestrial carbon (C) cycling and shapes ecosystem responses to environmental changes and hence terrestrial feedbacks to climate. Nonetheless, our understanding of nutrient controls remains far from complete and poorly quantified, at least partly due to a lack of informative, comparable, and accessible datasets at regional-to-global scales. A growing research infrastructure of multi-site networks are providing valuable data on C fluxes and stocks and are monitoring their responses to global environmental change and measuring responses to experimental treatments. These networks thus provide an opportunity for improving our understanding of C-nutrient cycle interactions and our ability to model them. However, coherent information on how nutrient cycling interacts with observed C cycle patterns is still generally lacking. Here, we argue that complementing available C-cycle measurements from monitoring and experimental sites with data characterizing nutrient availability will greatly enhance their power and will improve our capacity to forecast future trajectories of terrestrial C cycling and climate. Therefore, we propose a set of complementary measurements that are relatively easy to conduct routinely at any site or experiment and that, in combination with C cycle observations, can provide a robust characterization of the effects of nutrient availability across sites. In addition, we discuss the power of different observable variables for informing the formulation of models and constraining their predictions. Most widely available measurements of nutrient availability often do not align well with current modelling needs. This highlights the importance to foster the interaction between the empirical and modelling communities for setting future research priorities.", "keywords": ["Global vegetation models", "550", "manipulation experiments", "Terrestrial-Aquatic Linkages", "Kolefni", "01 natural sciences", "Nutrient cycle", "Agricultural and Biological Sciences", "Terrestrial ecosystem", "SDG 13 - Climate Action", "Climate change", "Jar\u00f0vegur", "Environmental resource management", "Global change", "General Environmental Science", "SDG 15 - Life on Land", "Carbon-nutrient cycle interactions", "2. Zero hunger", "Data syntheses", "Global and Planetary Change", "Ecology", "Geography", "Physics", "Life Sciences", "Application of Stable Isotopes in Trophic Ecology", "Cycling", "Carbon cycle", "04 agricultural and veterinary sciences", "Chemistry", "ORGANIC-MATTER", "Archaeology", "Physical Sciences", "Nutrient availability", "NET PRIMARY PRODUCTIVITY", "Ecosystem Functioning", "570", "LAND", "TROPICAL RAIN-FOREST", "carbon-nutrient cycle interactions", "data syntheses", "Soil Science", "Environmental science", "[SDU] Sciences of the Universe [physics]", "SOIL-PHOSPHORUS AVAILABILITY", "global vegetation models", "SDG 3 - Good Health and Well-being", "nutrients", "USE EFFICIENCY", "SDG 7 - Affordable and Clean Energy", "GLOBAL CHANGE", "Key (lock)", "Biology", "Ecosystem", "Manipulation experiments", "0105 earth and related environmental sciences", "Renewable Energy", " Sustainability and the Environment", "Ecosystem Structure", "Public Health", " Environmental and Occupational Health", "Nutrients", "15. Life on land", "Computer science", "[SDU]Sciences of the Universe [physics]", "13. Climate action", "ECOSYSTEM RESPONSES", "FOS: Biological sciences", "Global Methane Emissions and Impacts", "Environmental Science", "0401 agriculture", " forestry", " and fisheries", "NITROGEN-FIXATION", "Soil Carbon Dynamics and Nutrient Cycling in Ecosystems", "Nutrient Limitation", "ELEVATED CO2", "Nutrient"]}, "links": [{"href": "https://doi.org/20.500.11815/1261"}, {"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": "20.500.11815/1261", "name": "item", "description": "20.500.11815/1261", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/20.500.11815/1261"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2018-12-07T00:00:00Z"}}, {"id": "20.500.14352/94922", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-04-04T16:26:00Z", "type": "Journal Article", "created": "2018-09-22", "title": "Cascading effects from plants to soil microorganisms explain how plant species richness and simulated climate change affect soil multifunctionality", "description": "Abstract<p>Despite their importance, how plant communities and soil microorganisms interact to determine the capacity of ecosystems to provide multiple functions simultaneously (multifunctionality) under climate change is poorly known. We conducted a common garden experiment using grassland species to evaluate how plant functional structure and soil microbial (bacteria and protists) diversity and abundance regulate soil multifunctionality responses to joint changes in plant species richness (one, three and six species) and simulated climate change (3\uffc2\uffb0C warming and 35% rainfall reduction). The effects of species richness and climate on soil multifunctionality were indirectly driven via changes in plant functional structure and their relationships with the abundance and diversity of soil bacteria and protists. More specifically, warming selected for the larger and most productive plant species, increasing the average size within communities and leading to reductions in functional plant diversity. These changes increased the total abundance of bacteria that, in turn, increased that of protists, ultimately promoting soil multifunctionality. Our work suggests that cascading effects between plant functional traits and the abundance of multitrophic soil organisms largely regulate the response of soil multifunctionality to simulated climate change, and ultimately provides novel experimental insights into the mechanisms underlying the effects of biodiversity and climate change on ecosystem functioning.</p", "keywords": ["[SDE] Environmental Sciences", "0106 biological sciences", "570", "[SDV]Life Sciences [q-bio]", "Nutrientcycles", "Climate Change", "Edafolog\u00eda (Biolog\u00eda)", "Bacterial Physiological Phenomena", "biotic communities", "01 natural sciences", "631.4", "climatic changes", "Soil", "XXXXXX - Unknown", "Climate change", "14. Life underwater", "species richness", "bacteria", "Ecosystem", "Plant Physiological Phenomena", "Soil Microbiology", "biodiversity", "580", "2. Zero hunger", "species diversity", "Bacteria", "Protist", "2417.13 Ecolog\u00eda Vegetal", "nutrient cycles", "environmental filtering", "Biodiversity", "15. Life on land", "[SDV] Life Sciences [q-bio]", "climate change", "13. Climate action", "ecosystem functioning", "[SDE]Environmental Sciences", "Ecosystem functioning", "2511.02 Biolog\u00eda de Suelos", "protist", "Environmental filtering", "Species richness"]}, "links": [{"href": "https://onlinelibrary.wiley.com/doi/pdf/10.1111/gcb.14440"}, {"href": "https://doi.org/20.500.14352/94922"}, {"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": "20.500.14352/94922", "name": "item", "description": "20.500.14352/94922", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/20.500.14352/94922"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2018-10-09T00:00:00Z"}}, {"id": "21.11116/0000-0000-F094-9", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-04-04T16:26:03Z", "type": "Journal Article", "created": "2018-09-27", "title": "GOLUM-CNP v1.0: a data-driven modeling of carbon, nitrogen and phosphorus cycles in major terrestrial biomes", "description": "<?xml version='1.0' encoding='UTF-8'?><article><p>Abstract. Global terrestrial nitrogen (N) and phosphorus (P) cycles are coupled to the global carbon (C) cycle for net primary production (NPP), plant C allocation, and decomposition of soil organic matter, but N and P have distinct pathways of inputs and losses. Current C-nutrient models exhibit large uncertainties in their estimates of pool sizes, fluxes, and turnover rates of nutrients, due to a lack of consistent global data for evaluating the models. In this study, we present a new model\u2013data fusion framework called the Global Observation-based Land-ecosystems Utilization Model of Carbon, Nitrogen and Phosphorus (GOLUM-CNP) that combines the CARbon DAta MOdel fraMework (CARDAMOM) data-constrained C-cycle analysis with spatially explicit data-driven estimates of N and P inputs and losses and with observed stoichiometric ratios. We calculated the steady-state N- and P-pool sizes and fluxes globally for large biomes. Our study showed that new N inputs from biological fixation and deposition supplied &gt;20\u2009% of total plant uptake in most forest ecosystems but accounted for smaller fractions in boreal forests and grasslands. New P inputs from atmospheric deposition and rock weathering supplied a much smaller fraction of total plant uptake than new N inputs, indicating the importance of internal P recycling within ecosystems to support plant growth. Nutrient-use efficiency, defined as the ratio of gross primary production (GPP) to plant nutrient uptake, were diagnosed from our model results and compared between biomes. Tropical forests had the lowest N-use efficiency and the highest P-use efficiency of the forest biomes. An analysis of sensitivity and uncertainty indicated that the NPP-allocation fractions to leaves, roots, and wood contributed the most to the uncertainties in the estimates of nutrient-use efficiencies. Correcting for biases in NPP-allocation fractions produced more plausible gradients of N- and P-use efficiencies from tropical to boreal ecosystems and highlighted the critical role of accurate measurements of C allocation for understanding the N and P cycles.</p></article>", "keywords": ["Atmospheric sciences", "550", "Organic chemistry", "Carbon Dynamics in Peatland Ecosystems", "Deposition (geology)", "01 natural sciences", "Nutrient cycle", "Agricultural and Biological Sciences", "Terrestrial ecosystem", "Biome", "Taiga", "2. Zero hunger", "QE1-996.5", "Ecology", "Primary production", "Nutrient Cycling", "Life Sciences", "Phosphorus", "Geology", "Carbon cycle", "Nitrogen Cycle", "[SDU.ENVI] Sciences of the Universe [physics]/Continental interfaces", " environment", "Chemistry", "Physical Sciences", "environment", "Ecosystem Functioning", "Biogeochemical Cycling of Nutrients in Aquatic Ecosystems", "Nitrogen", "Soil Science", "Environmental science", "Environmental Chemistry", "New production", "Soil Carbon Sequestration", "Biology", "Ecosystem", "0105 earth and related environmental sciences", "[SDU.OCEAN]Sciences of the Universe [physics]/Ocean", "Atmosphere", "[SDU.OCEAN] Sciences of the Universe [physics]/Ocean", " Atmosphere", "ddc:550", "Nitrogen Dynamics", "Paleontology", "FOS: Earth and related environmental sciences", "15. Life on land", "13. Climate action", "FOS: Biological sciences", "Environmental Science", "Phytoplankton", "Sediment", "[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces", "Soil Carbon Dynamics and Nutrient Cycling in Ecosystems", "Nutrient"]}, "links": [{"href": "https://gmd.copernicus.org/articles/11/3903/2018/gmd-11-3903-2018.pdf"}, {"href": "https://doi.org/21.11116/0000-0000-F094-9"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Geoscientific%20Model%20Development", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "21.11116/0000-0000-F094-9", "name": "item", "description": "21.11116/0000-0000-F094-9", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/21.11116/0000-0000-F094-9"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2018-03-22T00:00:00Z"}}, {"id": "21.11116/0000-0000-F096-7", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-04-04T16:26:03Z", "type": "Journal Article", "created": "2018-09-27", "title": "GOLUM-CNP v1.0: a data-driven modeling of carbon, nitrogen and phosphorus cycles in major terrestrial biomes", "description": "<?xml version='1.0' encoding='UTF-8'?><article><p>Abstract. Global terrestrial nitrogen (N) and phosphorus (P) cycles are coupled to the global carbon (C) cycle for net primary production (NPP), plant C allocation, and decomposition of soil organic matter, but N and P have distinct pathways of inputs and losses. Current C-nutrient models exhibit large uncertainties in their estimates of pool sizes, fluxes, and turnover rates of nutrients, due to a lack of consistent global data for evaluating the models. In this study, we present a new model\u2013data fusion framework called the Global Observation-based Land-ecosystems Utilization Model of Carbon, Nitrogen and Phosphorus (GOLUM-CNP) that combines the CARbon DAta MOdel fraMework (CARDAMOM) data-constrained C-cycle analysis with spatially explicit data-driven estimates of N and P inputs and losses and with observed stoichiometric ratios. We calculated the steady-state N- and P-pool sizes and fluxes globally for large biomes. Our study showed that new N inputs from biological fixation and deposition supplied &gt;20\u2009% of total plant uptake in most forest ecosystems but accounted for smaller fractions in boreal forests and grasslands. New P inputs from atmospheric deposition and rock weathering supplied a much smaller fraction of total plant uptake than new N inputs, indicating the importance of internal P recycling within ecosystems to support plant growth. Nutrient-use efficiency, defined as the ratio of gross primary production (GPP) to plant nutrient uptake, were diagnosed from our model results and compared between biomes. Tropical forests had the lowest N-use efficiency and the highest P-use efficiency of the forest biomes. An analysis of sensitivity and uncertainty indicated that the NPP-allocation fractions to leaves, roots, and wood contributed the most to the uncertainties in the estimates of nutrient-use efficiencies. Correcting for biases in NPP-allocation fractions produced more plausible gradients of N- and P-use efficiencies from tropical to boreal ecosystems and highlighted the critical role of accurate measurements of C allocation for understanding the N and P cycles.                     </p></article>", "keywords": ["Atmospheric sciences", "550", "Organic chemistry", "Carbon Dynamics in Peatland Ecosystems", "Deposition (geology)", "01 natural sciences", "Nutrient cycle", "Agricultural and Biological Sciences", "Terrestrial ecosystem", "Biome", "Taiga", "2. Zero hunger", "QE1-996.5", "Ecology", "Primary production", "Nutrient Cycling", "Life Sciences", "Phosphorus", "Geology", "Carbon cycle", "Nitrogen Cycle", "[SDU.ENVI] Sciences of the Universe [physics]/Continental interfaces", " environment", "Chemistry", "Physical Sciences", "environment", "Ecosystem Functioning", "Biogeochemical Cycling of Nutrients in Aquatic Ecosystems", "Nitrogen", "Soil Science", "Environmental science", "Environmental Chemistry", "New production", "Soil Carbon Sequestration", "Biology", "Ecosystem", "0105 earth and related environmental sciences", "[SDU.OCEAN]Sciences of the Universe [physics]/Ocean", "Atmosphere", "[SDU.OCEAN] Sciences of the Universe [physics]/Ocean", " Atmosphere", "ddc:550", "Nitrogen Dynamics", "Paleontology", "FOS: Earth and related environmental sciences", "15. Life on land", "13. Climate action", "FOS: Biological sciences", "Environmental Science", "Phytoplankton", "Sediment", "[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces", "Soil Carbon Dynamics and Nutrient Cycling in Ecosystems", "Nutrient"]}, "links": [{"href": "https://gmd.copernicus.org/articles/11/3903/2018/gmd-11-3903-2018.pdf"}, {"href": "https://doi.org/21.11116/0000-0000-F096-7"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Geoscientific%20Model%20Development", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "21.11116/0000-0000-F096-7", "name": "item", "description": "21.11116/0000-0000-F096-7", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/21.11116/0000-0000-F096-7"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2018-03-22T00:00:00Z"}}, {"id": "2440/106807", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-04-04T16:26:15Z", "type": "Journal Article", "created": "2017-06-13", "title": "Circular linkages between soil biodiversity, fertility and plant productivity are limited to topsoil at the continental scale", "description": "Summary<p>   <p>The current theoretical framework suggests that tripartite positive feedback relationships between soil biodiversity, fertility and plant productivity are universal. However, empirical evidence for these relationships at the continental scale and across different soil depths is lacking.</p>  <p>We investigate the continental\uffe2\uff80\uff90scale relationships between the diversity of microbial and invertebrate\uffe2\uff80\uff90based soil food webs, fertility and above\uffe2\uff80\uff90ground plant productivity at 289 sites and two soil depths, that is 0\uffe2\uff80\uff9310 and 20\uffe2\uff80\uff9330\uffc2\uffa0cm, across Australia.</p>  <p>Soil biodiversity, fertility and plant productivity are strongly positively related in surface soils. Conversely, in the deeper soil layer, the relationships between soil biodiversity, fertility and plant productivity weaken considerably, probably as a result of a reduction in biodiversity and fertility with depth. Further modeling suggested that strong positive associations among soil biodiversity\uffe2\uff80\uff93fertility and fertility\uffe2\uff80\uff93plant productivity are limited to the upper soil layer (0\uffe2\uff80\uff9310\uffc2\uffa0cm), after accounting for key factors, such as distance from the equator, altitude, climate and physicochemical soil properties.</p>  <p>These findings highlight the importance of surface soil biodiversity for soil fertility, and suggest that any loss of surface soil could potentially break the links between soil biodiversity\uffe2\uff80\uff93fertility and/or fertility\uffe2\uff80\uff93plant productivity, which can negatively impact nutrient cycling and food production, upon which future generations depend.</p>  </p", "keywords": ["0301 basic medicine", "Eukaryotes", "Climate", "Plant Development", "soil biodiversity", "Terrestrial ecosystems", "Soil", "03 medical and health sciences", "eukaryotes", "1110 Plant Science", "XXXXXX - Unknown", "plant productivity", "bacteria", "Ecosystem functionality", "Soil Microbiology", "2. Zero hunger", "0303 health sciences", "Bacteria", "Australia", "terrestrial ecosystems", "1314 Physiology", "Biodiversity", "15. Life on land", "Soil biodiversity", "ecosystem functionality", "Fertility", "ecosystems", "Plant productivity"]}, "links": [{"href": "https://nph.onlinelibrary.wiley.com/doi/pdf/10.1111/nph.14634"}, {"href": "https://doi.org/2440/106807"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/New%20Phytologist", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "2440/106807", "name": "item", "description": "2440/106807", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/2440/106807"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2017-06-13T00:00:00Z"}}, {"id": "2893251307", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-04-04T16:26:24Z", "type": "Journal Article", "created": "2018-09-22", "title": "Cascading effects from plants to soil microorganisms explain how plant species richness and simulated climate change affect soil multifunctionality", "description": "Abstract<p>Despite their importance, how plant communities and soil microorganisms interact to determine the capacity of ecosystems to provide multiple functions simultaneously (multifunctionality) under climate change is poorly known. We conducted a common garden experiment using grassland species to evaluate how plant functional structure and soil microbial (bacteria and protists) diversity and abundance regulate soil multifunctionality responses to joint changes in plant species richness (one, three and six species) and simulated climate change (3\uffc2\uffb0C warming and 35% rainfall reduction). The effects of species richness and climate on soil multifunctionality were indirectly driven via changes in plant functional structure and their relationships with the abundance and diversity of soil bacteria and protists. More specifically, warming selected for the larger and most productive plant species, increasing the average size within communities and leading to reductions in functional plant diversity. These changes increased the total abundance of bacteria that, in turn, increased that of protists, ultimately promoting soil multifunctionality. Our work suggests that cascading effects between plant functional traits and the abundance of multitrophic soil organisms largely regulate the response of soil multifunctionality to simulated climate change, and ultimately provides novel experimental insights into the mechanisms underlying the effects of biodiversity and climate change on ecosystem functioning.</p", "keywords": ["[SDE] Environmental Sciences", "0106 biological sciences", "570", "[SDV]Life Sciences [q-bio]", "Nutrientcycles", "Climate Change", "Edafolog\u00eda (Biolog\u00eda)", "Bacterial Physiological Phenomena", "biotic communities", "01 natural sciences", "631.4", "climatic changes", "Soil", "XXXXXX - Unknown", "Climate change", "14. Life underwater", "species richness", "bacteria", "Ecosystem", "Plant Physiological Phenomena", "Soil Microbiology", "biodiversity", "580", "2. 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