{"type": "FeatureCollection", "features": [{"id": "10.1007/s004420100656", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-27T16:14:50Z", "type": "Journal Article", "created": "2003-02-13", "title": "Fine-Root Biomass And Fluxes Of Soil Carbon In Young Stands Of Paper Birch And Trembling Aspen As Affected By Elevated Atmospheric Co2 And Tropospheric O3", "description": "Rising atmospheric CO2 may stimulate future forest productivity, possibly increasing carbon storage in terrestrial ecosystems, but how tropospheric ozone will modify this response is unknown. Because of the importance of fine roots to the belowground C cycle, we monitored fine-root biomass and associated C fluxes in regenerating stands of trembling aspen, and mixed stands of trembling aspen and paper birch at FACTS-II, the Aspen FACE project in Rhinelander, Wisconsin. Free-air CO2 enrichment (FACE) was used to elevate concentrations of CO2 (average enrichment concentration 535\u00a0\u00b5l l-1) and O3 (53\u00a0nl l-1) in developing forest stands in 1998 and 1999. Soil respiration, soil pCO2, and dissolved organic carbon in soil solution (DOC) were monitored biweekly. Soil respiration was measured with a portable infrared gas analyzer. Soil pCO2 and DOC samples were collected from soil gas wells and tension lysimeters, respectively, at depths of 15, 30, and 125\u00a0cm. Fine-root biomass averaged 263\u00a0g m-2 in control plots and increased 96% under elevated CO2. The increased root biomass was accompanied by a 39% increase in soil respiration and a 27% increase in soil pCO2. Both soil respiration and pCO2 exhibited a strong seasonal signal, which was positively correlated with soil temperature. DOC concentrations in soil solution averaged ~12\u00a0mg l-1 in surface horizons, declined with depth, and were little affected by the treatments. A simplified belowground C budget for the site indicated that native soil organic matter still dominated the system, and that soil respiration was by far the largest flux. Ozone decreased the above responses to elevated CO2, but effects were rarely statistically significant. We conclude that regenerating stands of northern hardwoods have the potential for substantially greater C input to soil due to greater fine-root production under elevated CO2. Greater fine-root biomass will be accompanied by greater soil C efflux as soil respiration, but leaching losses of C will probably be unaffected.", "keywords": ["0106 biological sciences", "Ecology and Evolutionary Biology", "Aspen-FACE-project", "root-", "USA-", "pollutants-", "Environmental-Sciences)", "tropospheric-ozone", "forest-productivity", "01 natural sciences", "biomass-", "northern-forests", "124-38-9: CARBON DIOXIDE", "soil-carbon-flux", "terrestrial-ecosystems", "populus-tremuloides", "Cellular and Developmental Biology", "soil-carbon", "7440-44-0: CARBON", "carbon-", "fine-root", "Bioenergetics- (Biochemistry-and-Molecular-Biophysics)", "Natural Resources and Environment", "04 agricultural and veterinary sciences", "GLOBAL-ECOLOGY", "North-America", "Nearctic-region)", "Rhinelander- (Wisconsin-", "carbon-sequestration", "atmosphere-", "biomass-production", "dissolved-organic-carbon [DOC-]", "Science", "respiration-", "carbon-dioxide-enrichment", "forest-plantations", "carbon-dioxide", "carbon-storage", "fine-root-biomass", "belowground-biomass", "United-States-Wisconsin-Rhinelander", "carbon-cycle", "Health Sciences", "ozone-", "soil-respiration", "air-pollution", "global-change", "atmospheric-carbon-dioxide", "biomass", "Molecular", "15. 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Climate action", "roots-", "Legacy", "Terrestrial-Ecology (Ecology-", "free-air-carbon-dioxide-enrichment [FREE-]: experimental-method", "0401 agriculture", " forestry", " and fisheries", "Northern Forests Global Change Carbon Sequestration Soil Respiration Dissolved Organic Carbon Soil PCO2"]}, "links": [{"href": "https://doi.org/10.1007/s004420100656"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Oecologia", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1007/s004420100656", "name": "item", "description": "10.1007/s004420100656", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1007/s004420100656"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2001-07-01T00:00:00Z"}}, {"id": "10.3389/fmicb.2022.859063", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-07-27T16:21:37Z", "type": "Journal Article", "created": "2022-05-17", "title": "Interacting Bioenergetic and Stoichiometric Controls on Microbial Growth", "description": "<p>Microorganisms function as open systems that exchange matter and energy with their surrounding environment. Even though mass (carbon and nutrients) and energy exchanges are tightly linked, there is a lack of integrated approaches that combine these fluxes and explore how they jointly impact microbial growth. Such links are essential to predicting how the growth rate of microorganisms varies, especially when the stoichiometry of carbon- (C) and nitrogen (N)-uptake is not balanced. Here, we present a theoretical framework to quantify the microbial growth rate for conditions of C-, N-, and energy-(co-) limitations. We use this framework to show how the C:N ratio and the degree of reduction of the organic matter (OM), which is also the electron donor, availability of electron acceptors (EAs), and the different sources of N together control the microbial growth rate under C, nutrient, and energy-limited conditions. We show that the growth rate peaks at intermediate values of the degree of reduction of OM under oxic and C-limited conditions, but not under N-limited conditions. Under oxic conditions and with N-poor OM, the growth rate is higher when the inorganic N (NInorg)-source is ammonium compared to nitrate due to the additional energetic cost involved in nitrate reduction. Under anoxic conditions, when nitrate is both EA and NInorg-source, the growth rates of denitrifiers and microbes performing the dissimilatory nitrate reduction to ammonia (DNRA) are determined by both OM degree of reduction and nitrate-availability. Consistent with the data, DNRA is predicted to foster growth under extreme nitrate-limitation and with a reduced OM, whereas denitrifiers are favored as nitrate becomes more available and in the presence of oxidized OM. Furthermore, the growth rate is reduced when catabolism is coupled to low energy yielding EAs (e.g., sulfate) because of the low carbon use efficiency (CUE). However, the low CUE also decreases the nutrient demand for growth, thereby reducing N-limitation. We conclude that bioenergetics provides a useful conceptual framework for explaining growth rates under different metabolisms and multiple resource-limitations.</p", "keywords": ["2. Zero hunger", "0301 basic medicine", "0303 health sciences", "denitrification", "660", "nitrogen limitation", "microbial growth", "Biological Sciences", "bioenergetics", "Microbiology", "QR1-502", "6. Clean water", "stoichiometry", "DNRA", "thermodynamics", "03 medical and health sciences", "Geovetenskap och relaterad milj\u00f6vetenskap", "Microbiology (Microbiology in the medical area to be 30109)", "13. Climate action", "Biologiska vetenskaper", "Bioenergy", "Earth and Related Environmental Sciences", "energy limitation"]}, "links": [{"href": "https://pub.epsilon.slu.se/28342/1/chakrawal-a-et-al-220615.pdf"}, {"href": "https://doi.org/10.3389/fmicb.2022.859063"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Frontiers%20in%20Microbiology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.3389/fmicb.2022.859063", "name": "item", "description": "10.3389/fmicb.2022.859063", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.3389/fmicb.2022.859063"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2022-05-17T00:00:00Z"}}, {"id": "10.1128/msystems.00495-19", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-27T16:19:55Z", "type": "Journal Article", "created": "2020-04-13", "title": "Energetic Basis of Microbial Growth and Persistence in Desert Ecosystems", "description": "<?xml version='1.0' encoding='UTF-8'?><article><p>Microbial life is surprisingly abundant and diverse in global desert ecosystems. In these environments, microorganisms endure a multitude of physicochemical stresses, including low water potential, carbon and nitrogen starvation, and extreme temperatures. In this review, we summarize our current understanding of the energetic mechanisms and trophic dynamics that underpin microbial function in desert ecosystems. Accumulating evidence suggests that dormancy is a common strategy that facilitates microbial survival in response to water and carbon limitation.</p></article>", "keywords": ["0301 basic medicine", "dormancy", "CYANOBACTERIAL EXOPOLYSACCHARIDES", "Trace gas", "Microbiology", "SOIL CRUSTS", "Energy reserve", "HIGH-AFFINITY", "03 medical and health sciences", "trace gas", "ATMOSPHERIC TRACE GASES", "Energetics", "energy reserve", "Dormancy", "SOR RONDANE MOUNTAINS", "Desert", "Photosynthesis", "106026 Ecosystem research", "CARBON-MONOXIDE", "desert", "ATACAMA DESERT", "energetics", "2. 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Climate action", "MOLECULAR-HYDROGEN", "106022 Microbiology", "Minireview"]}, "links": [{"href": "https://journals.asm.org/doi/pdf/10.1128/mSystems.00495-19"}, {"href": "https://doi.org/10.1128/msystems.00495-19"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/mSystems", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1128/msystems.00495-19", "name": "item", "description": "10.1128/msystems.00495-19", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1128/msystems.00495-19"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2020-04-28T00:00:00Z"}}, {"id": "10.1890/02-3005", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-27T16:20:42Z", "type": "Journal Article", "created": "2007-06-04", "title": "Co-2 Enrichment Reduces The Energetic Cost Of Biomass Construction In An Invasive Desert Grass", "description": "To examine how global change could influence species invasions, we compared the responses of energetic processes and growth of invasive and native grass species to atmospheric CO2 enrichment in an intact Mojave Desert ecosystem. Combined with its modest influence on photosynthetic activity, elevated atmospheric CO2 was associated with a significant reduction in the energetic cost of aboveground biomass construction in invasive Bromus madritensis spp. rubens (red brome) without a concurrent cost reduction in native Vulpia octoflora (six-weeks fescue). Consequently, the invasive grass species grew faster, grew bigger, and produced more seeds with atmospheric CO2 enrichment than the native grass species. As a physiological mechanism of invasive species success driven by CO2 enrichment, such alterations in biomass construction costs combined with increased photosynthetic activity could trigger a shift in the species composition of this ecosystem, and potentially that of other invaded ecosystems, toward increa...", "keywords": ["0106 biological sciences", "2. Zero hunger", "Bromus madritensis spp. rubens", "Invasive species", "Invasive grasses", "Red brome", "Systems Biology", "Plant Biology", "Native grasses", "NDFF", "Weed Science", "15. Life on land", "01 natural sciences", "Mojave Desert", "Vulpia octoflora", "Relative growth rate", "13. Climate action", "Energetics", "Six-weeks fescue", "Construction cost", "Elevated CO2", "Photosynthesis", "Nevada"]}, "links": [{"href": "https://doi.org/10.1890/02-3005"}, {"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": "10.1890/02-3005", "name": "item", "description": "10.1890/02-3005", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1890/02-3005"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2004-01-01T00:00:00Z"}}, {"id": "10.5281/zenodo.5547311", "type": "Feature", "geometry": null, "properties": {"license": "Embargo", "updated": "2026-07-27T16:24:29Z", "type": "Dataset", "title": "Energetic return on investment determines overall soil microbial activity.", "description": "<strong>Data</strong> and <strong>R codes</strong> used for the manuscript entitled ' <strong>Energetic return on investment determines overall soil microbial activity.'</strong>", "keywords": ["organic carbon", "community composition", "microorganisms", "bioenergetics", "microbial activity", "FT-ICR-MS", "calorimetry", "soil"], "contacts": [{"organization": "Dufour, Louis J.P., Herrmann, Anke M., Leloup, Julie, Przybylski, C\ufffd\ufffddric, Foti, Ludovic, Abbadie, Luc, Nunan, Naoise,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.5281/zenodo.5547311"}, {"rel": "self", "type": "application/geo+json", "title": "10.5281/zenodo.5547311", "name": "item", "description": "10.5281/zenodo.5547311", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.5281/zenodo.5547311"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2021-01-01T00:00:00Z"}}, {"id": "2263/74486", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-27T16:27:01Z", "type": "Journal Article", "created": "2020-04-13", "title": "Energetic Basis of Microbial Growth and Persistence in Desert Ecosystems", "description": "<?xml version='1.0' encoding='UTF-8'?><article><p>Microbial life is surprisingly abundant and diverse in global desert ecosystems. In these environments, microorganisms endure a multitude of physicochemical stresses, including low water potential, carbon and nitrogen starvation, and extreme temperatures. In this review, we summarize our current understanding of the energetic mechanisms and trophic dynamics that underpin microbial function in desert ecosystems. Accumulating evidence suggests that dormancy is a common strategy that facilitates microbial survival in response to water and carbon limitation.</p></article>", "keywords": ["0301 basic medicine", "dormancy", "CYANOBACTERIAL EXOPOLYSACCHARIDES", "Trace gas", "Microbiology", "SOIL CRUSTS", "Energy reserve", "HIGH-AFFINITY", "03 medical and health sciences", "trace gas", "ATMOSPHERIC TRACE GASES", "Energetics", "energy reserve", "Dormancy", "SOR RONDANE MOUNTAINS", "Desert", "Photosynthesis", "106026 Ecosystem research", "CARBON-MONOXIDE", "desert", "ATACAMA DESERT", "energetics", "2. Zero hunger", "106022 Mikrobiologie", "0303 health sciences", "photosynthesis", "COMMUNITY RESPONSE", "15. Life on land", "QR1-502", "106026 \u00d6kosystemforschung", "DRY SOIL", "13. Climate action", "MOLECULAR-HYDROGEN", "106022 Microbiology", "Minireview"]}, "links": [{"href": "https://journals.asm.org/doi/pdf/10.1128/mSystems.00495-19"}, {"href": "https://doi.org/2263/74486"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/mSystems", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "2263/74486", "name": "item", "description": "2263/74486", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/2263/74486"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2020-04-28T00:00:00Z"}}, {"id": "PMC9152356", "type": "Feature", "geometry": null, "properties": {"license": "Open Access", "updated": "2026-07-27T16:30:32Z", "type": "Journal Article", "created": "2022-05-17", "title": "Interacting Bioenergetic and Stoichiometric Controls on Microbial Growth", "description": "<p>Microorganisms function as open systems that exchange matter and energy with their surrounding environment. Even though mass (carbon and nutrients) and energy exchanges are tightly linked, there is a lack of integrated approaches that combine these fluxes and explore how they jointly impact microbial growth. Such links are essential to predicting how the growth rate of microorganisms varies, especially when the stoichiometry of carbon- (C) and nitrogen (N)-uptake is not balanced. Here, we present a theoretical framework to quantify the microbial growth rate for conditions of C-, N-, and energy-(co-) limitations. We use this framework to show how the C:N ratio and the degree of reduction of the organic matter (OM), which is also the electron donor, availability of electron acceptors (EAs), and the different sources of N together control the microbial growth rate under C, nutrient, and energy-limited conditions. We show that the growth rate peaks at intermediate values of the degree of reduction of OM under oxic and C-limited conditions, but not under N-limited conditions. Under oxic conditions and with N-poor OM, the growth rate is higher when the inorganic N (NInorg)-source is ammonium compared to nitrate due to the additional energetic cost involved in nitrate reduction. Under anoxic conditions, when nitrate is both EA and NInorg-source, the growth rates of denitrifiers and microbes performing the dissimilatory nitrate reduction to ammonia (DNRA) are determined by both OM degree of reduction and nitrate-availability. Consistent with the data, DNRA is predicted to foster growth under extreme nitrate-limitation and with a reduced OM, whereas denitrifiers are favored as nitrate becomes more available and in the presence of oxidized OM. Furthermore, the growth rate is reduced when catabolism is coupled to low energy yielding EAs (e.g., sulfate) because of the low carbon use efficiency (CUE). However, the low CUE also decreases the nutrient demand for growth, thereby reducing N-limitation. We conclude that bioenergetics provides a useful conceptual framework for explaining growth rates under different metabolisms and multiple resource-limitations.</p", "keywords": ["0301 basic medicine", "2. Zero hunger", "0303 health sciences", "denitrification", "660", "nitrogen limitation", "microbial growth", "Biological Sciences", "bioenergetics", "Microbiology", "QR1-502", "6. Clean water", "stoichiometry", "DNRA", "thermodynamics", "03 medical and health sciences", "Geovetenskap och relaterad milj\u00f6vetenskap", "Microbiology (Microbiology in the medical area to be 30109)", "13. 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