The degree to which climate warming will stimulate soil organic carbon (SOC) losses via heterotrophic respiration remains uncertain, in part because different or even opposite microbial physiology and temperature relationships have been proposed in SOC models. We incorporated competing microbial carbon use efficiency (CUE)–mean annual temperature (MAT) and enzyme kinetic–MAT relationships into SOC models, and compared the simulated mass‐specific soil heterotrophic respiration rates with multiple published datasets of measured respiration. The measured data included 110 dryland soils globally distributed and two continental to global‐scale cross‐biome datasets. Model–data comparisons suggested that a positive CUE–MAT relationship best predic...
© The Author(s), 2017. This article is distributed under the terms of the Creative Commons Attributi...
The respiratory release of carbon dioxide (CO2) from soil is a major yet poorly understood flux in t...
Author Posting. © The Author(s), 2008. This is the author's version of the work. It is posted here ...
This is the author accepted manuscript. The final version is available from Nature Research via the ...
Global soil carbon (C) stocks are expected to decline with warming, and changes in microbial process...
The central objective of the proposed work was to develop a genomic approach (nucleic acid-based) th...
Soil contains a large amount of organic matter, which constitutes the largest terrestrial carbon poo...
Climate warming may stimulate microbial metabolism of soil carbon, causing a carbon cycle-climate fe...
Multiple lines of existing evidence suggest that increasing CO2 emission from soils in response to r...
Global soil carbon (C) stocks are expected to decline with warming, and changes in microbial process...
Soil microbial respiration is an important source of uncertainty in projecting future climate and ca...
Global ecosystem models may require microbial components to accurately predict feedbacks between cli...
Microbes are responsible for cycling carbon (C) through soils, and predicted changes in soil C stock...
Enhanced soil respiration in response to global warming may substantially increase atmospheric CO2 c...
Soil respiration, a process primarily driven by soil microbes, is the largest flux of carbon from te...
© The Author(s), 2017. This article is distributed under the terms of the Creative Commons Attributi...
The respiratory release of carbon dioxide (CO2) from soil is a major yet poorly understood flux in t...
Author Posting. © The Author(s), 2008. This is the author's version of the work. It is posted here ...
This is the author accepted manuscript. The final version is available from Nature Research via the ...
Global soil carbon (C) stocks are expected to decline with warming, and changes in microbial process...
The central objective of the proposed work was to develop a genomic approach (nucleic acid-based) th...
Soil contains a large amount of organic matter, which constitutes the largest terrestrial carbon poo...
Climate warming may stimulate microbial metabolism of soil carbon, causing a carbon cycle-climate fe...
Multiple lines of existing evidence suggest that increasing CO2 emission from soils in response to r...
Global soil carbon (C) stocks are expected to decline with warming, and changes in microbial process...
Soil microbial respiration is an important source of uncertainty in projecting future climate and ca...
Global ecosystem models may require microbial components to accurately predict feedbacks between cli...
Microbes are responsible for cycling carbon (C) through soils, and predicted changes in soil C stock...
Enhanced soil respiration in response to global warming may substantially increase atmospheric CO2 c...
Soil respiration, a process primarily driven by soil microbes, is the largest flux of carbon from te...
© The Author(s), 2017. This article is distributed under the terms of the Creative Commons Attributi...
The respiratory release of carbon dioxide (CO2) from soil is a major yet poorly understood flux in t...
Author Posting. © The Author(s), 2008. This is the author's version of the work. It is posted here ...