A positive soil carbon (C)\uffe2\uff80\uff90climate feedback is embedded into the climatic models of the IPCC. However, recent global syntheses indicate that the temperature sensitivity of soil respiration (RS) in drylands, the largest biome on Earth, is actually lower in warmed than in control plots. Consequently, soil C losses with future warming are expected to be low compared with other biomes. Nevertheless, the empirical basis for these global extrapolations is still poor in drylands, due to the low number of field experiments testing the pathways behind the long\uffe2\uff80\uff90term responses of soil respiration (RS) to warming. Importantly, global drylands are covered with biocrusts (communities formed by bryophytes, lichens, cyanobacteria, fungi, and bacteria), and thus,RSresponses to warming may be driven by both autotrophic and heterotrophic pathways. Here, we evaluated the effects of 8\uffe2\uff80\uff90year experimental warming onRS, and the different pathways involved, in a biocrust\uffe2\uff80\uff90dominated dryland in southern Spain. We also assessed the overall impacts on soil organic C (SOC) accumulation over time. Across the years and biocrust cover levels, warming reducedRSby 0.30\uffc2\uffa0\uffce\uffbcmol\uffc2\uffa0CO2\uffc2\uffa0m\uffe2\uff88\uff922\uffc2\uffa0s\uffe2\uff88\uff921(95% CI\uffc2\uffa0=\uffc2\uffa0\uffe2\uff88\uff920.24 to 0.84), although the negative warming effects were only significant after 3\uffc2\uffa0years of elevated temperatures in areas with low initial biocrust cover. We found support for different pathways regulating the warming\uffe2\uff80\uff90induced reduction inRSat areas with low (microbial thermal acclimation via reduced soil mass\uffe2\uff80\uff90specific respiration and \uffce\uffb2\uffe2\uff80\uff90glucosidase enzymatic activity) vs. high (microbial thermal acclimation jointly with a reduction in autotrophic respiration from decreased lichen cover) initial biocrust cover. Our 8\uffe2\uff80\uff90year experimental study shows a reduction in soil respiration with warming and highlights that biocrusts should be explicitly included in modeling efforts aimed to quantify the soil C\uffe2\uff80\uff93climate feedback in drylands. Ecology Letters (2011) 14: 187\uffe2\uff80\uff93194
AbstractThe degree to which rising atmospheric CO2 will be offset by carbon (C) sequestration in forests depends in part on the capacity of trees and soil microbes to make physiological adjustments that can alleviate resource limitation. Here, we show for the first time that mature trees exposed to CO2 enrichment increase the release of soluble C from roots to soil, and that such increases are coupled to the accelerated turnover of nitrogen (N) pools in the rhizosphere. Over the course of 3\uffe2\uff80\uff83years, we measured in situ rates of root exudation from 420 intact loblolly pine (Pinus taeda L.) roots. Trees fumigated with elevated CO2 (200 p.p.m.v. over background) increased exudation rates (\uffce\uffbcg\uffe2\uff80\uff83C\uffe2\uff80\uff83cm\uffe2\uff88\uff921\uffe2\uff80\uff83root\uffe2\uff80\uff83h\uffe2\uff88\uff921) by 55% during the primary growing season, leading to a 50% annual increase in dissolved organic inputs to fumigated forest soils. These increases in root\uffe2\uff80\uff90derived C were positively correlated with microbial release of extracellular enzymes involved in breakdown of organic N (R2\uffe2\uff80\uff83=\uffe2\uff80\uff830.66; P\uffe2\uff80\uff83=\uffe2\uff80\uff830.006) in the rhizosphere, indicating that exudation stimulated microbial activity and accelerated the rate of soil organic matter (SOM) turnover. In support of this conclusion, trees exposed to both elevated CO2 and N fertilization did not increase exudation rates and had reduced enzyme activities in the rhizosphere. Collectively, our results provide field\uffe2\uff80\uff90based empirical support suggesting that sustained growth responses of forests to elevated CO2 in low fertility soils are maintained by enhanced rates of microbial activity and N cycling fuelled by inputs of root\uffe2\uff80\uff90derived C. To the extent that increases in exudation also stimulate SOM decomposition, such changes may prevent soil C accumulation in forest ecosystems.
", "keywords": ["0106 biological sciences", "Nitrogen", "Plant Exudates", "Pinus taeda", "04 agricultural and veterinary sciences", "15. Life on land", "Carbon Dioxide", "01 natural sciences", "Plant Roots", "Carbon", "Trees", "Soil", "13. Climate action", "Rhizosphere", "North Carolina", "0401 agriculture", " forestry", " and fisheries", "Soil Microbiology"]}, "links": [{"href": "https://doi.org/10.1111/j.1461-0248.2010.01570.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.1461-0248.2010.01570.x", "name": "item", "description": "10.1111/j.1461-0248.2010.01570.x", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1111/j.1461-0248.2010.01570.x"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2010-12-22T00:00:00Z"}}, {"id": "10.1111/1462-2920.13678", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:18:33Z", "type": "Journal Article", "created": "2017-01-25", "title": "Bacterial, Fungal, And Plant Communities Exhibit No Biomass Or Compositional Response To Two Years Of Simulated Nitrogen Deposition In A Semiarid Grassland", "description": "SummaryNitrogen (N) deposition affects myriad aspects of terrestrial ecosystem structure and function, and microbial communities may be particularly sensitive to anthropogenic N inputs. However, our understanding of N deposition effects on microbial communities is far from complete, especially for drylands where data are comparatively rare. To address the need for an improved understanding of dryland biological responses to N deposition, we conducted a two\uffe2\uff80\uff90year fertilization experiment in a semiarid grassland on the Colorado Plateau in the southwestern United States. We evaluated effects of varied levels of N inputs on archaeal, bacterial, fungal and chlorophyte community composition within three microhabitats: biological soil crusts (biocrusts), soil below biocrusts, and the plant rhizosphere. Surprisingly, N addition did not affect the community composition or diversity of any of these microbial groups; however, microbial community composition varied significantly among sampling microhabitats. Further, while plant richness, diversity, and cover showed no response to N addition, there were strong linkages between plant properties and microbial community structure. Overall, these findings highlight the potential for some dryland communities to have limited biotic ability to retain augmented N inputs, possibly leading to large N losses to the atmosphere and to aquatic systems.
", "keywords": ["2. Zero hunger", "0301 basic medicine", "0303 health sciences", "Colorado", "Nitrogen", "Fungi", "15. Life on land", "Plants", "Archaea", "Grassland", "Soil", "03 medical and health sciences", "13. Climate action", "Rhizosphere", "Biomass", "Ecosystem", "Soil Microbiology"]}, "links": [{"href": "https://doi.org/10.1111/1462-2920.13678"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Environmental%20Microbiology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1111/1462-2920.13678", "name": "item", "description": "10.1111/1462-2920.13678", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1111/1462-2920.13678"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2017-03-13T00:00:00Z"}}, {"id": "10.1007/s12275-011-0421-x", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:15:19Z", "type": "Journal Article", "created": "2011-06-30", "title": "The Impacts Of Excessive Nitrogen Additions On Enzyme Activities And Nutrient Leaching In Two Contrasting Forest Soils", "description": "Nitrogen (N) deposition has increased dramatically worldwide, which may affect forest soils in various ways. In this study, we conducted a short-term manipulation experiment of N addition on two types of forest soils (urban and rural soils) found in Korea. N addition significantly decreased phenol oxidase activities in urban soil samples; however, it did not affect those in rural soils. Furthermore, N addition did not change \u03b2-glucosidase and N-acetylglucosaminidase activities, except for \u03b2-glucosidase activities in the O layer of rural soils. Changes in microbial biomass and general activity (dehydrogenase activity) were not induced by N addition, except for dehydrogenase in the A layer of urban soils. Although N addition did not change the extractable soil nutrients, organic matter, and water contents significantly, it enhanced nutrient leaching and resulted in lower pH leachate. These results suggest that excessive N addition to forest soils may induce nutrient leaching in the long-term. Overall results of our study also suggest that N addition may induce retardation of organic matter decomposition in soils; however, such a response may depend on the intensity of previous exposure to N deposition.", "keywords": ["2. Zero hunger", "Nitrogen", "04 agricultural and veterinary sciences", "Hydrogen-Ion Concentration", "15. Life on land", "6. Clean water", "Enzymes", "Trees", "Soil", "13. Climate action", "Republic of Korea", "11. Sustainability", "0401 agriculture", " forestry", " and fisheries", "Soil Microbiology"]}, "links": [{"href": "https://doi.org/10.1007/s12275-011-0421-x"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/The%20Journal%20of%20Microbiology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1007/s12275-011-0421-x", "name": "item", "description": "10.1007/s12275-011-0421-x", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1007/s12275-011-0421-x"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2011-06-01T00:00:00Z"}}, {"id": "10.1007/s12275-012-2409-6", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:15:19Z", "type": "Journal Article", "created": "2012-11-03", "title": "Characterization Of The Bacterial And Archaeal Communities In Rice Field Soils Subjected To Long-Term Fertilization Practices", "description": "The bacterial and archaeal communities in rice field soils subjected to different fertilization regimes for 57 years were investigated in two different seasons, a non-planted, drained season (April) and a rice-growing, flooded season (August), by performing soil dehydrogenase assay, real-time PCR assay and pyrosequencing analysis. All fertilization regimes increased the soil dehydrogenase activity while the abundances of bacteria and archaea increased in the plots receiving inorganic fertilizers plus compost and not in those receiving inorganic fertilizers only. Rice-growing and flooding decreased the soil dehydrogenase activity while they increased the bacterial diversity in rice field soils. The bacterial communities were dominated by Chloroflexi, Proteobacteria, and Actinobacteria and the archaeal communities by Crenarchaeota at the phylum level. In principal coordinates analysis based on the weighted Fast UniFrac metric, the bacterial and archaeal communities were separated primarily by season, and generally distributed along with soil pH, the variation of which had been caused by long-term fertilization. Variations in the relative abundance according to the season or soil pH were observed for many bacterial and archaeal groups. In conclusion, the microbial activity, prokaryotic abundance and diversity, and prokaryotic community structure in the rice field soils were changed by season and long-term fertilization.", "keywords": ["DNA", " Bacterial", "0301 basic medicine", "2. Zero hunger", "0303 health sciences", "Bacteria", "Molecular Sequence Data", "Agriculture", "Oryza", "15. Life on land", "Archaea", "6. Clean water", "Soil", "03 medical and health sciences", "RNA", " Ribosomal", " 16S", "Seasons", "Fertilizers", "Phylogeny", "Soil Microbiology"]}, "links": [{"href": "https://doi.org/10.1007/s12275-012-2409-6"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Journal%20of%20Microbiology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1007/s12275-012-2409-6", "name": "item", "description": "10.1007/s12275-012-2409-6", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1007/s12275-012-2409-6"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2012-10-01T00:00:00Z"}}, {"id": "10.1007/s12275-014-4129-6", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:15:19Z", "type": "Journal Article", "created": "2014-12-02", "title": "Effect Of Long-Term Different Fertilization On Bacterial Community Structures And Diversity In Citrus Orchard Soil Of Volcanic Ash", "description": "This study was conducted to assess bacterial species richness, diversity and community distribution according to different fertilization regimes for 16 years in citrus orchard soil of volcanic ash. Soil samples were collected and analyzed from Compost (cattle manure, 2,000 kg/10a), 1/2 NPK+compost (14-20-14+2,000 kg/10a), NPK+compost (28-40-28+2,000 kg/10a), NPK (28-40-28 kg/10a), 3 NPK (84-120-84 kg/10a), and Control (no fertilization) plot which have been managed in the same manners with compost and different amount of chemical fertilization. The range of pyrosequencing reads and OTUs were 4,687-7,330 and 1,790-3,695, respectively. Species richness estimates such as Ace, Chao1, and Shannon index were higher in 1/2 NPK+compost than other treatments, which were 15,202, 9,112, 7.7, respectively. Dominant bacterial groups at level of phylum were Proteobacteria, Acidobacteria, and Actinobacteria. Those were occupied at 70.9% in 1/2 NPK+compost. Dominant bacterial groups at level of genus were Pseudolabrys, Bradyrhizobium, and Acidobacteria. Those were distributed at 14.4% of a total of bacteria in Compost. Soil pH displayed significantly closely related to bacterial species richness estimates such as Ace, Chao1 (p<0.05) and Shannon index (p<0.01). However, it showed the negative correlation with exchangeable aluminum contents (p<0.05). In conclusion, diversity of bacterial community in citrus orchard soil was affected by fertilization management, soil pH changes and characteristics of volcanic ash.", "keywords": ["0301 basic medicine", "2. Zero hunger", "Citrus", "0303 health sciences", "Bacteria", "Agriculture", "Biodiversity", "Volcanic Eruptions", "15. Life on land", "Acidobacteria", "Actinobacteria", "Manure", "Soil", "03 medical and health sciences", "RNA", " Ribosomal", " 16S", "Proteobacteria", "Animals", "Cattle", "14. Life underwater", "Fertilizers", "Soil Microbiology", "Alphaproteobacteria"]}, "links": [{"href": "https://doi.org/10.1007/s12275-014-4129-6"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Journal%20of%20Microbiology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1007/s12275-014-4129-6", "name": "item", "description": "10.1007/s12275-014-4129-6", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1007/s12275-014-4129-6"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2014-11-29T00:00:00Z"}}, {"id": "10.1007/s11274-011-0809-0", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:15:13Z", "type": "Journal Article", "created": "2011-06-15", "title": "Soil Bacterial Community Composition And Diversity Respond To Cultivation In Karst Ecosystems", "description": "Soil microorganisms play vital roles in recovering and maintaining the health of ecosystems, particularly in fragile Karst ecosystems that are easily degraded after cultivation. We investigated the composition and diversity of soil bacterial communities, based on RFLP and 16S rDNA sequencing, in a cropland, a naturally revegetated land with former cultivation disturbance and a primeval forest in the subtropical Karst of southwest China. Our results illustrated that Proteobacteria accounted for 44.8% of the 600 tested clones, making it the most dominant phylum observed. This phylum was followed by Acidobacteria and Planctomycetes for the three Karst soils analyzed. Compared with the primeval forest soil, the proportions of Proteobacteria were decreased by 30.2 and 37.9%, while Acidobacteria increased by 93.9 and 87.9%, and the Shannon-Wiener diversity indices and the physicochemical parameters declined in the cropland and the revegetated land, respectively. Among the three soils, the proportion of dominant bacterial phyla and the diversity indices in the revegetated land were similar to the cropland, implying the bacterial community in the cropland was relatively stable, and the after-effects of cultivation were difficult to eliminate. However, similar distributions of the four Proteobacteria subphyla were observed between the revegetated land and the primeval forest soil. Furthermore, the proportion of Rhizobiales belonging to \u03b1-Proteobacteria was sharply decreased with cultivation compared to the primeval forest soil, while a small cluster of Rhizobiales recurred with vegetation recovery. These results indicated that although the subphyla of the dominant bacterial phylum had some positive responses to 20\u00a0years of vegetation recovery, it is a slow process. Our results suggest that priority should be given to conserve the primeval forest and inoculation of functional microorganisms on the basis of vegetation recovery may be more effective for the restoration of Karst ecosystems after cultivation.", "keywords": ["2. Zero hunger", "0301 basic medicine", "China", "0303 health sciences", "Bacteria", "Agriculture", "Biodiversity", "15. Life on land", "Trees", "RNA", " Bacterial", "Soil", "03 medical and health sciences", "RNA", " Ribosomal", " 16S", "Metagenome", "Ecosystem", "Phylogeny", "Polymorphism", " Restriction Fragment Length", "Soil Microbiology"], "contacts": [{"organization": "Xiangbi Chen, Ya-wei Wei, Wenxue Wei, Jinshui Wu, Yirong Su, Xunyang He,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.1007/s11274-011-0809-0"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/World%20Journal%20of%20Microbiology%20and%20Biotechnology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1007/s11274-011-0809-0", "name": "item", "description": "10.1007/s11274-011-0809-0", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1007/s11274-011-0809-0"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2011-06-15T00:00:00Z"}}, {"id": "10.1016/j.scitotenv.2019.01.095", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:16:47Z", "type": "Journal Article", "created": "2019-01-10", "title": "The Cover Crop Determines The Amf Community Composition In Soil And In Roots Of Maize After A Ten-Year Continuous Crop Rotation", "description": "Intensive agricultural practices are responsible for soil biological degradation. By stimulating indigenous arbuscular mycorrhizal fungi (AMF), cover cropping enhances soil health and promotes agroecosystem sustainability. Still, the legacy effects of cover crops (CCs) and the major factors driving the AM fungal community are not well known; neither is the influence of the specific CC. This work describes a field experiment established in Central Spain to test the effect of replacing winter fallow by barley (Hordeum vulgare L.) or vetch (Vicia sativa L.) during the intercropping of maize (Zea mays L.). We examined the community composition of the AMF in the roots and rhizosphere soil associated with the subsequent cash crop after 10\u202fyears of cover cropping, using Illumina technology. The multivariate analysis showed that the AMF communities under the barley treatment differed significantly from those under fallow, whereas no legacy effect of the vetch CC was detected. Soil organic carbon, electrical conductivity, pH, Ca and microbial biomass carbon were identified as major factors shaping soil AMF communities. Specific AMF taxa were found to play a role in plant uptake of P, Fe, Zn, Mn, and Cd, which may shed light on the functionality of these taxa. In our conditions, the use of barley as a winter CC appears to be an appropriate choice with respect to promotion of AMF populations and biological activity in agricultural soils with intercropping systems. However, more research on CC species and their legacy effect on the microbial community composition and functionality are needed to guide decisions in knowledge-based agriculture.", "keywords": ["Crops", " Agricultural", "2. Zero hunger", "Diversity", "Cover cropping", "Grass", "Arbuscular mycorrhizal fungi", "Agriculture", "Hordeum", "04 agricultural and veterinary sciences", "15. Life on land", "Plant Roots", "Zea mays", "Crop Production", "Legume", "Spain", "Long-term experiment", "Mycorrhizae", "Long-term experiments", "Rhizosphere", "0401 agriculture", " forestry", " and fisheries", "Illumina technology", "Mediterranean climate", "Soil Microbiology", "Mycobiome"]}, "links": [{"href": "https://doi.org/10.1016/j.scitotenv.2019.01.095"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Science%20of%20The%20Total%20Environment", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.scitotenv.2019.01.095", "name": "item", "description": "10.1016/j.scitotenv.2019.01.095", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.scitotenv.2019.01.095"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2019-04-01T00:00:00Z"}}, {"id": "10.1007/s11356-016-6927-3", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:15:14Z", "type": "Journal Article", "created": "2016-05-27", "title": "Crop Residue Management And Fertilization Effects On Soil Organic Matter And Associated Biological Properties", "description": "Returning crop residue may result in nutrient reduction in soil in the first few years. A two-year field experiment was conducted to assess whether this negative effect is alleviated by improved crop residue management (CRM). Nine treatments (3 CRM and 3\u00a0N fertilizer rates) were used. The CRM treatments were (1) R0: 100\u00a0% of the N using mineral fertilizer with no crop residues return; (2) R: crop residue plus mineral fertilizer as for the R0; and (3) Rc: crop residue plus 83\u00a0% of the N using mineral and 17\u00a0% manure fertilizer. Each CRM received N fertilizer rates at 270, 360, and 450\u00a0kg\u00a0N\u00a0ha(-1) year(-1). At the end of the experiment, soil NO3-N was reduced by 33\u00a0% from the R relative to the R0 treatment, while the Rc treatment resulted in a 21 to 44\u00a0% increase in occluded particulate organic C and N, and 80\u00a0\u00b0C extracted dissolved organic N, 19 to 32\u00a0% increase in microbial biomass C and protease activity, and higher monounsaturated phospholipid fatty acid (PLFA):saturated PLFA ratio from stimulating growth of indigenous bacteria when compared with the R treatment. Principal component analysis showed that the Biolog and PLFA profiles in the three CRM treatments were different from each other. Overall, these properties were not influenced by the used N fertilizer rates. Our results indicated that application of 17\u00a0% of the total N using manure in a field with crop residues return was effective for improving potential plant N availability and labile soil organic matter, primarily due to a shift in the dominant microorganisms.", "keywords": ["Crops", " Agricultural", "2. Zero hunger", "Soil organic matter", "Minerals", "Enzymatic activity", "550", "Bacteria", "Agriculture", "04 agricultural and veterinary sciences", "15. Life on land", "630", "6. Clean water", "Manure", "Soil", "Fertilizer rate", "Biolog", "PLFA", "0401 agriculture", " forestry", " and fisheries", "Biomass", "Fertilizers", "Soil Microbiology"]}, "links": [{"href": "https://doi.org/10.1007/s11356-016-6927-3"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Environmental%20Science%20and%20Pollution%20Research", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1007/s11356-016-6927-3", "name": "item", "description": "10.1007/s11356-016-6927-3", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1007/s11356-016-6927-3"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2016-05-28T00:00:00Z"}}, {"id": "10.1007/s11356-018-1397-4", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:15:14Z", "type": "Journal Article", "created": "2018-02-06", "title": "Impacts Of Earthworm Activity On The Fate Of Straw Carbon In Soil: A Microcosm Experiment", "description": "Earthworms not only facilitate carbon (C) stabilization, but also accelerate organic matter mineralization by enhancing microbial respiration. However, the fate (mineralization vs stabilization) of newly added C by straw returning in arable lands with earthworm activity is still unclear. In the present 40\u00a0days incubation study, we incorporated artificially 13C-labeled straw into soil with and without presence of earthworms (Metaphire guillelmi). Flux measurements of CO2 from soil (mineralization) were taken regularly, while straw-derived C remaining in the soil (stabilization) was measured at the end of the incubation. There was no significant difference of the cumulative CO2 emission between earthworm presence and absence treatment. However, earthworm presence significantly decreased straw-derived cumulative CO2-C emission when compared with the treatment without earthworm. Besides, earthworm incubation led to a significantly low light fraction organic carbon (LFOC) content and straw-derived LFOC proportion. Relative to the non-earthworm treatment, straw-derived C content significantly decreased in micro-aggregates (<\u20090.25\u00a0mm), but increased in large macro-aggregates (>\u20092\u00a0mm) in the earthworm treatment. In total, only 3.8% of added straw C was assimilated by earthworm within 40\u00a0days, while most of the straw C remained in the soil. Earthworms decreased straw-derived CO2-C emission from 10.0 to 8.1% when compared with the non-earthworm treatment. In the present short period incubation experiment, compared with the soil without earthworms, the presence of Metaphire guillelmi (1) resulted a higher soil CO2 emissions, which may mainly evolved from the older SOC, and (2) stabilized more residue-derived C in the soil aggregates. We therefore propose that Metaphire guillelmi may increase soil organic carbon pool turnover rates in the short term after straw returning by replacement of older SOC with newly added straw C.", "keywords": ["2. Zero hunger", "Soil", "13. Climate action", "Animals", "0401 agriculture", " forestry", " and fisheries", "04 agricultural and veterinary sciences", "Oligochaeta", "15. Life on land", "Carbon", "Soil Microbiology"]}, "links": [{"href": "https://doi.org/10.1007/s11356-018-1397-4"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Environmental%20Science%20and%20Pollution%20Research", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1007/s11356-018-1397-4", "name": "item", "description": "10.1007/s11356-018-1397-4", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1007/s11356-018-1397-4"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2018-02-06T00:00:00Z"}}, {"id": "10.1016/j.scitotenv.2019.03.176", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:16:47Z", "type": "Journal Article", "created": "2019-03-13", "title": "Effect of digestate application on microbial respiration and bacterial communities' diversity during bioremediation of weathered petroleum hydrocarbons contaminated soils", "description": "Digestate is an organic by-product of biogas production via anaerobic digestion processes and has a great potential as soil fertilizer due to concentrated nutrients. In this study, we examined digestate as a potential nutrient and microbial seeding for bioremediation of weathered (aged) petroleum hydrocarbon contaminated soils. We analysed 6 different treatments in microcosm using two industrial soils having different textures: a clay rich soil and a sandy soil. After 30\u202fdays of incubation, the highest total petroleum hydrocarbons (TPH) removal was observed in microcosms containing digestate together with bulking agent (17.8% and 12.7% higher than control in clay rich soil and sandy soil, respectively) or digestate together with immobilized bacteria (13.4% and 9% higher than control in clay rich soil and sandy soil, respectively). After digestate application microbial respiration was enhanced in sandy soil and inhibited in clay rich soil due to aggregates formation. After bulking agent addition to clay rich soil aggregates size was reduced and oxygen uptake was improved. Application of digestate to soil resulted in the development of distinct microbial groups in amended and non-amended soils. Genera containing species able to degrade TPH like Acinetobacter and Mycobacterium were abundant in digestate and in soil amended with digestate. Quantification of alkB genes, encoding alkane monoxygenase, revealed high concentration of these genes in digestate bacterial community. After application of digestate, the level of alkB genes significantly increased in soils and remained high until the end of the treatment. The study revealed great potential of digestate as a nutrient and bacteria source for soil bioremediation.", "keywords": ["[SDE] Environmental Sciences", "TPH removal", "550", "Soil remediation", "0211 other engineering and technologies", "alkB genes; Organic fertilizers; qPCR; Soil remediation; TPH removal; Biodegradation", " Environmental; Environmental Restoration and Remediation; Hydrocarbons; Petroleum; Petroleum Pollution; Soil; Soil Pollutants; Soil Microbiology", "02 engineering and technology", "01 natural sciences", "7. Clean energy", "630", "Organic fertilizers", "Environmental", "Soil", "alkB genes", "Soil Pollutants", "Petroleum Pollution", "Environmental Restoration and Remediation", "Soil Microbiology", "0105 earth and related environmental sciences", "2. Zero hunger", "[SDE.IE]Environmental Sciences/Environmental Engineering", "15. Life on land", "Hydrocarbons", "6. Clean water", "qPCR", "Biodegradation", " Environmental", "Petroleum", "[SDE]Environmental Sciences", "Biodegradation", "[SDE.IE] Environmental Sciences/Environmental Engineering"]}, "links": [{"href": "https://doi.org/10.1016/j.scitotenv.2019.03.176"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Science%20of%20The%20Total%20Environment", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.scitotenv.2019.03.176", "name": "item", "description": "10.1016/j.scitotenv.2019.03.176", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.scitotenv.2019.03.176"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2019-06-01T00:00:00Z"}}, {"id": "10.1038/s41586-024-07274-7", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:17:44Z", "type": "Journal Article", "created": "2024-04-17", "title": "Environmental drivers of increased ecosystem respiration in a warming tundra", "description": "AbstractArctic and alpine tundra ecosystems are large reservoirs of organic carbon1,2. Climate warming may stimulate ecosystem respiration and release carbon into the atmosphere3,4. The magnitude and persistency of this stimulation and the environmental mechanisms that drive its variation remain uncertain5\uffe2\uff80\uff937. This hampers the accuracy of global land carbon\uffe2\uff80\uff93climate feedback projections7,8. Here we synthesize 136 datasets from 56 open-top chamber in situ warming experiments located at 28 arctic and alpine tundra sites which have been running for less than 1\uffe2\uff80\uff89year up to 25\uffe2\uff80\uff89years. We show that a mean rise of 1.4\uffe2\uff80\uff89\uffc2\uffb0C [confidence interval (CI) 0.9\uffe2\uff80\uff932.0\uffe2\uff80\uff89\uffc2\uffb0C] in air and 0.4\uffe2\uff80\uff89\uffc2\uffb0C [CI 0.2\uffe2\uff80\uff930.7\uffe2\uff80\uff89\uffc2\uffb0C] in soil temperature results in an increase in growing season ecosystem respiration by 30% [CI 22\uffe2\uff80\uff9338%] (n\uffe2\uff80\uff89=\uffe2\uff80\uff89136). Our findings indicate that the stimulation of ecosystem respiration was due to increases in both plant-related and microbial respiration (n\uffe2\uff80\uff89=\uffe2\uff80\uff899) and continued for at least 25\uffe2\uff80\uff89years (n\uffe2\uff80\uff89=\uffe2\uff80\uff89136). The magnitude of the warming effects on respiration was driven by variation in warming-induced changes in local soil conditions, that is, changes in total nitrogen concentration and pH and by context-dependent spatial variation in these conditions, in particular total nitrogen concentration and the carbon:nitrogen ratio. Tundra sites with stronger nitrogen limitations and sites in which warming had stimulated plant and microbial nutrient turnover seemed particularly sensitive in their respiration response to warming. The results highlight the importance of local soil conditions and warming-induced changes therein for future climatic impacts on respiration.traditional>conventional, highlighting the importance of integrative biomarker-based strategies for the development of the trace metal 'footprint' in Andosols.", "keywords": ["2. Zero hunger", "beta-Glucosidase", "Agriculture", "04 agricultural and veterinary sciences", "15. Life on land", "01 natural sciences", "6. Clean water", "Soil", "Metals", "13. Climate action", "Soil Pollutants", "0401 agriculture", " forestry", " and fisheries", "Biomass", "Oxidoreductases", "Soil Microbiology", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://orca.cardiff.ac.uk/id/eprint/102750/1/Parelho%202016.pdf"}, {"href": "https://doi.org/10.1016/j.ecoenv.2016.03.019"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Ecotoxicology%20and%20Environmental%20Safety", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.ecoenv.2016.03.019", "name": "item", "description": "10.1016/j.ecoenv.2016.03.019", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.ecoenv.2016.03.019"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2016-07-01T00:00:00Z"}}, {"id": "10072/428410", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-01T16:24:22Z", "type": "Journal Article", "created": "2023-10-18", "title": "Community composition and physiological plasticity control microbial carbon storage across natural and experimental soil fertility gradients", "description": "Abstract
Many microorganisms synthesise carbon (C)-rich compounds under resource deprivation. Such compounds likely serve as intracellular C-storage pools that sustain the activities of microorganisms growing on stoichiometrically imbalanced substrates, making them potentially vital to the function of ecosystems on infertile soils. We examined the dynamics and drivers of three putative C-storage compounds (neutral lipid fatty acids [NLFAs], polyhydroxybutyrate [PHB], and trehalose) across a natural gradient of soil fertility in eastern Australia. Together, NLFAs, PHB, and trehalose corresponded to 8.5\uffe2\uff80\uff9340% of microbial C and 0.06\uffe2\uff80\uff930.6% of soil organic C. When scaled to \uffe2\uff80\uff9cstructural\uffe2\uff80\uff9d microbial biomass (indexed by polar lipid fatty acids; PLFAs), NLFA and PHB allocation was 2\uffe2\uff80\uff933-times greater in infertile soils derived from ironstone and sandstone than in comparatively fertile basalt- and shale-derived soils. PHB allocation was positively correlated with belowground biological phosphorus (P)-demand, while NLFA allocation was positively correlated with fungal PLFA : bacterial PLFA ratios. A complementary incubation revealed positive responses of respiration, storage, and fungal PLFAs to glucose, while bacterial PLFAs responded positively to PO43-. By comparing these results to a model of microbial C-allocation, we reason that NLFA primarily served the \uffe2\uff80\uff9creserve\uffe2\uff80\uff9d storage mode for C-limited taxa (i.e., fungi), while the variable portion of PHB likely served as \uffe2\uff80\uff9csurplus\uffe2\uff80\uff9d C-storage for P-limited bacteria. Thus, our findings reveal a convergence of community-level processes (i.e., changes in taxonomic composition that underpin reserve-mode storage dynamics) and intracellular mechanisms (e.g., physiological plasticity of surplus-mode storage) that drives strong, predictable community-level microbial C-storage dynamics across gradients of soil fertility and substrate stoichiometry.