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Labile Carbon Addition Shifts Wetland Soil Microbes Towards R-Strategists and Increases Temperature Sensitivity of Microbial Respiration
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Outgoing claims: the papers this work cites, builds on, or argues with.
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Responses of microbial activity to carbon, nitrogen, and phosphorus additions in forest mineral soils differing in organic carbon content
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The priming effect dynamics are driven by microbial activation and growth and constrained by the relative availability of input C and soil N
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An evaluation of plant-available soil nitrogen in selected sandy soils by electro-ultrafiltration, KCl, and CaCl 2 extraction methods
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Effect of soil CO 2 concentration on microbial biomass
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Labile substrate availability controls temperature sensitivity of organic carbon decomposition at different soil depths
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Response of microbial activity and community structure to decreasing soil osmotic and matric potential
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Contrasting effects of increased carbon input on boreal SOM decomposition with and without presence of living root system of Pinus sylvestris L.
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The sensitivity of soil microbial respiration declined due to crop straw addition but did not depend on the type of crop straw
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Land use change exerts a strong impact on deep soil C stabilization in subtropical forests
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Analytical approaches to the characterization of samples of microbial communities using patterns of potential C source utilization
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Priming effects in Chernozem induced by glucose and N in relation to microbial growth strategies
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Labile carbon addition alters soil organic carbon mineralization but not its temperature sensitivity in a freshwater marsh of Northeast China
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Ammonia nitrogen and dissolved organic carbon regulate soil microbial gene abundances and enzyme activities in wetlands under different vegetation types
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The temperature sensitivity of organic carbon mineralization is affected by exogenous carbon inputs and soil organic carbon content
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Microbial biomass and ecoenzymatic stoichiometries vary in response to nutrient availability in an arable soil
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How nutrient loads influence microbial-derived carbon accumulation in wetlands: A new insight from microbial metabolic investment strategies
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Deep soil microbial carbon metabolic function is important but often neglected: a study on the Songnen Plain reed wetland, Northeast China
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Priming effects in soils after combined and repeated substrate additions
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Effects of carbon input quality and timing on soil microbe mediated processes
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Response of soil nitrogen mineralization to warming temperatures depends on soil management history
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Widespread asymmetric response of soil heterotrophic respiration to warming and cooling
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Microbial assemblies associated with temperature sensitivity of soil respiration along an altitudinal gradient
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Catalytic efficiency of soil enzymes explains temperature sensitivity: Insights from physiological theory
inferredcites →https://doi.org/10.1016/j.soilbio.2004.09.014openalex-snapshot
Responses of extracellular enzymes to simple and complex nutrient inputs
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Interactions between plants, litter and microbes in cycling of nitrogen and phosphorus in the arctic
inferredcites →https://doi.org/10.1016/j.soilbio.2010.04.003openalex-snapshot
Priming effects: Interactions between living and dead organic matter
inferredcites →https://doi.org/10.1016/j.soilbio.2013.08.024openalex-snapshot
Active microorganisms in soil: Critical review of estimation criteria and approaches
inferredcites →https://doi.org/10.1016/j.soilbio.2013.09.007openalex-snapshot
Reduced substrate supply limits the temperature response of soil organic carbon decomposition
inferredcites →https://doi.org/10.1016/j.soilbio.2014.04.033openalex-snapshot
Rhizosphere priming effects on soil carbon and nitrogen mineralization
inferredcites →https://doi.org/10.1016/j.soilbio.2014.09.005openalex-snapshot
Biochemistry of hexose and pentose transformations in soil analyzed by position-specific labeling and 13C-PLFA
inferredcites →https://doi.org/10.1016/j.soilbio.2015.07.021openalex-snapshot
Sugars in soil and sweets for microorganisms: Review of origin, content, composition and fate
inferredcites →https://doi.org/10.1016/j.soilbio.2016.01.004openalex-snapshot
Large amounts of easily decomposable carbon stored in subtropical forest subsoil are associated with r-strategy-dominated soil microbes
inferredcites →https://doi.org/10.1016/j.soilbio.2017.08.031openalex-snapshot
Adaptation of microbial resource allocation affects modelled long term soil organic matter and nutrient cycling
inferredcites →https://doi.org/10.1016/j.soilbio.2019.06.006openalex-snapshot
Microbial utilization of simple carbon substrates in boreal peat soils at low temperatures
inferredcites →https://doi.org/10.1016/j.soilbio.2019.107561openalex-snapshot
Peatland microbial community response to altered climate tempered by nutrient availability
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Carbon and nitrogen recycling from microbial necromass to cope with C:N stoichiometric imbalance by priming
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inferredcites →https://doi.org/10.1016/j.soilbio.2022.108589openalex-snapshot
Short-term effects of labile organic C addition on soil microbial response to temperature in a temperate steppe
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Stoichiometric regulation of priming effects and soil carbon balance by microbial life strategies
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Linkages between the temperature sensitivity of soil respiration and microbial life strategy are dependent on sampling season
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Modeling ecosystem-scale carbon dynamics in soil: The microbial dimension
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Review of mechanisms and quantification of priming effects
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The dependence of soil CO2 efflux on temperature
inferredcites →https://doi.org/10.1016/s0038-0717(01)00020-7openalex-snapshot
Soil microbial biomass is triggered into activity by trace amounts of substrate
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The priming effect of organic matter: a question of microbial competition?
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Corn cob biochar increases soil culturable bacterial abundance without enhancing their capacities in utilizing carbon sources in Biolog Eco-plates
inferredcites →https://doi.org/10.1029/2008gb003327openalex-snapshot
Soil organic carbon pools in the northern circumpolar permafrost region
inferredcites →https://doi.org/10.1038/nature04514openalex-snapshot
Temperature sensitivity of soil carbon decomposition and feedbacks to climate change
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Temperature sensitivity of soil respiration rates enhanced by microbial community response
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Widespread coupling between the rate and temperature sensitivity of organic matter decay
inferredcites →https://doi.org/10.1038/nrmicro1643openalex-snapshot
The role of ecological theory in microbial ecology
inferredcites →https://doi.org/10.1038/nrmicro2439openalex-snapshot
Microorganisms and climate change: terrestrial feedbacks and mitigation options
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Soil microbial respiration adapts to ambient temperature in global drylands
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Cross-biome patterns in soil microbial respiration predictable from evolutionary theory on thermal adaptation
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Temperature fluctuation promotes the thermal adaptation of soil microbial respiration
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Structure and function of the global topsoil microbiome
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The diversity and biogeography of soil bacterial communities
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Shifts in microbial trophic strategy explain different temperature sensitivity of CO2 flux under constant and diurnally varying temperature regimes
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Higher temperature sensitivity for stable than for labile soil organic carbon – Evidence from incubations of long‐term bare fallow soils
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Soil C and N availability determine the priming effect: microbial N mining and stoichiometric decomposition theories
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Functional genomic analysis of corals from natural CO 2 ‐seeps reveals core molecular responses involved in acclimatization to ocean acidification
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Carbon input by roots into the soil: Quantification of rhizodeposition from root to ecosystem scale
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Temperature adaptation of soil microbial respiration in alpine, boreal and tropical soils: An application of the square root (Ratkowsky) model
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High microbial diversity stabilizes the responses of soil organic carbon decomposition to warming in the subsoil on the Tibetan Plateau
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Elevated CO 2 shifts soil microbial communities from K ‐ to r ‐strategists
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Effects of substrate availability on the temperature sensitivity of soil organic matter decomposition
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Stimulation of microbial extracellular enzyme activities by elevated CO 2 depends on soil aggregate size
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Temperature and soil organic matter decomposition rates - synthesis of current knowledge and a way forward
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Summer warming accelerates sub‐arctic peatland nitrogen cycling without changing enzyme pools or microbial community structure
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Size and functional diversity of microbe populations control plant persistence and long‐term soil carbon accumulation
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Thermal adaptation of soil microbial respiration to elevated temperature
inferredcites →https://doi.org/10.1111/mec.15773openalex-snapshot
Winter warming rapidly increases carbon degradation capacities of fungal communities in tundra soil: Potential consequences on carbon stability
inferredcites →https://doi.org/10.1128/aem.02874-09openalex-snapshot
Soil Microbial Community Responses to Multiple Experimental Climate Change Drivers
inferredcites →https://doi.org/10.1371/journal.pone.0109161openalex-snapshot
New Insights into How Increases in Fertility Improve the Growth of Rice at the Seedling Stage in Red Soil Regions of Subtropical China
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Vulnerability of Permafrost Carbon to Climate Change: Implications for the Global Carbon Cycle
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NUTRIENT SUBSIDIES TO BELOWGROUND MICROBES IMPACT ABOVEGROUND FOOD WEB INTERACTIONS
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TOWARD AN ECOLOGICAL CLASSIFICATION OF SOIL BACTERIA
inferredcites →https://doi.org/10.1890/10-2028.1openalex-snapshot
Substrate concentration and enzyme allocation can affect rates of microbial decomposition
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ATMOSPHERIC NITRATE DEPOSITION AND ENHANCED DISSOLVED ORGANIC CARBON LEACHING
inferredcites →https://doi.org/10.2307/3060891openalex-snapshot
Response of CO 2 and CH 4 Emissions from Peatlands to Warming and Water Table Manipulation
inferredcites →https://doi.org/10.3389/fmicb.2022.1093487openalex-snapshot
Soil CO2 and N2O emissions and microbial abundances altered by temperature rise and nitrogen addition in active-layer soils of permafrost peatland
inferredcites →https://doi.org/10.3390/microorganisms10010131openalex-snapshot
Water Level Has Higher Influence on Soil Organic Carbon and Microbial Community in Poyang Lake Wetland Than Vegetation Type
inferredcites →https://doi.org/10.3390/microorganisms10071329openalex-snapshot
Warming-Induced Labile Carbon Change Soil Organic Carbon Mineralization and Microbial Abundance in a Northern Peatland
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