The temperature response of soil microbial efficiency and its feedback to climate
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Social dynamics within decomposer communities lead to nitrogen retention and organic matter build-up in soils.Managing uncertainty in soil carbon feedbacks to climate changeSoil Functional Zone Management: A Vehicle for Enhancing Production and Soil Ecosystem Services in Row-Crop Agroecosystems.Labile compounds in plant litter reduce the sensitivity of decomposition to warming and altered precipitation.Investigating the long-term legacy of drought and warming on the soil microbial community across five European shrubland ecosystems.Model systems for a no-analog future: species associations and climates during the last deglaciation.Climate change and mammals: evolutionary versus plastic responses.Plant litter chemistry and microbial priming regulate the accrual, composition and stability of soil carbon in invaded ecosystems.Soil respiration under climate warming: differential response of heterotrophic and autotrophic respiration.Microbial dormancy improves development and experimental validation of ecosystem modelSoil respiration response to climate change in Pacific Northwest prairies is mediated by a regional Mediterranean climate gradient.Are there links between responses of soil microbes and ecosystem functioning to elevated CO2, N deposition and warming? A global perspective.Modeling adaptation of carbon use efficiency in microbial communitiesMicrobial models with data-driven parameters predict stronger soil carbon responses to climate change.Long-term forest soil warming alters microbial communities in temperate forest soilsTerrestrial and marine perspectives on modeling organic matter degradation pathways.Two decades of warming increases diversity of a potentially lignolytic bacterial community.Biofuel intercropping effects on soil carbon and microbial activity.Neurospora discreta as a model to assess adaptation of soil fungi to warmingSoil Respiration and Bacterial Structure and Function after 17 Years of a Reciprocal Soil Transplant ExperimentChanges in the Size of the Active Microbial Pool Explain Short-Term Soil Respiratory Responses to Temperature and Moisture.Elevated CO2 and temperature increase soil C losses from a soybean-maize ecosystem.Flexible Carbon-Use Efficiency across Litter Types and during Decomposition Partly Compensates Nutrient Imbalances-Results from Analytical Stoichiometric Models.Microbial community composition explains soil respiration responses to changing carbon inputs along an Andes-to-Amazon elevation gradient.Microbial carbon mineralization in tropical lowland and montane forest soils of Peru.Does agricultural crop diversity enhance soil microbial biomass and organic matter dynamics? A meta-analysis.Short-term precipitation exclusion alters microbial responses to soil moisture in a wet tropical forest.Compositional differences in simulated root exudates elicit a limited functional and compositional response in soil microbial communities.Microbial profiling of South African acid mine water samples using next generation sequencing platform.Plant community and soil chemistry responses to long-term nitrogen inputs drive changes in alpine bacterial communities.Shifts in microbial trophic strategy explain different temperature sensitivity of CO2 flux under constant and diurnally varying temperature regimes.Alpine soil carbon is vulnerable to rapid microbial decomposition under climate cooling.Accelerated soil carbon turnover under tree plantations limits soil carbon storageDirect evidence for microbial-derived soil organic matter formation and its ecophysiological controlsOffsetting global warming-induced elevated greenhouse gas emissions from an arable soil by biochar application.Modelling the dynamic physical protection of soil organic carbon: Insights into carbon predictions and explanation of the priming effect.Temperature sensitivity and enzymatic mechanisms of soil organic matter decomposition along an altitudinal gradient on Mount Kilimanjaro.Uncertain future soil carbon dynamics under global change predicted by models constrained by total carbon measurements.Use of 13 C- and phosphate 18 O-labeled substrate for studying phosphorus and carbon cycling in soils: a proof of concept.Mycorrhiza-mediated competition between plants and decomposers drives soil carbon storage.
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The temperature response of soil microbial efficiency and its feedback to climate
description
article
@en
im Januar 2013 veröffentlichter wissenschaftlicher Artikel
@de
wetenschappelijk artikel
@nl
наукова стаття, опублікована в січні 2013
@uk
name
The temperature response of soil microbial efficiency and its feedback to climate
@en
The temperature response of soil microbial efficiency and its feedback to climate
@nl
type
label
The temperature response of soil microbial efficiency and its feedback to climate
@en
The temperature response of soil microbial efficiency and its feedback to climate
@nl
prefLabel
The temperature response of soil microbial efficiency and its feedback to climate
@en
The temperature response of soil microbial efficiency and its feedback to climate
@nl
P2093
P2860
P356
P1476
The temperature response of soil microbial efficiency and its feedback to climate
@en
P2093
Jerry M. Melillo
Serita D. Frey
P2860
P2888
P304
P356
10.1038/NCLIMATE1796
P50
P577
2013-01-20T00:00:00Z