Rising global temperatures may increase the rates of soil organic matter decomposition by heterotrophic microorganisms, potentially accelerating climate change further by releasing additional carbon dioxide (CO2 ) to the atmosphere. However, the possibility that microbial community responses to prolonged warming may modify the temperature sensitivity of soil respiration creates large uncertainty in the strength of this positive feedback. Both compensatory responses (decreasing temperature sensitivity of soil respiration in the long-term) and enhancing responses (increasing temperature sensitivity) have been reported, but the mechanisms underlying these responses are poorly understood. In this study, microbial biomass, community structure an...
types: Journal Article; Research Support, Non-U.S. Gov'tThis a post-print, author-produced version o...
Understanding the mechanisms by which soil respiration responds to climate change is critical to p...
Author Posting. © The Author(s), 2008. This is the author's version of the work. It is posted here ...
Rising global temperatures may increase the rates of soil organic matter decomposition by heterotrop...
Rising global temperatures may increase the rates of soil organic matter decomposition by heterotrop...
Rising global temperatures may increase the rates of soil organic matter decomposition by heterotrop...
Rising global temperatures may increase the rates of soil organic matter decomposition by heterotrop...
Microbes are responsible for cycling carbon (C) through soils, and predicted changes in soil C stock...
Microbes are responsible for cycling carbon (C) through soils, and predicted changes in soil C stock...
Microbes are responsible for cycling carbon (C) through soils, and predicted changes in soil C stock...
Microbes are responsible for cycling carbon (C) through soils, and predicted changes in soil C stock...
Microbes are responsible for cycling carbon (C) through soils, and predicted changes in soil C stock...
Soil microbial respiration and methanogenesis are key sources of atmospheric carbon. Conflicting evi...
The central objective of the proposed work was to develop a genomic approach (nucleic acid-based) th...
AbstractSoil microbial communities mediate the decomposition of soil organic matter (SOM). The amoun...
types: Journal Article; Research Support, Non-U.S. Gov'tThis a post-print, author-produced version o...
Understanding the mechanisms by which soil respiration responds to climate change is critical to p...
Author Posting. © The Author(s), 2008. This is the author's version of the work. It is posted here ...
Rising global temperatures may increase the rates of soil organic matter decomposition by heterotrop...
Rising global temperatures may increase the rates of soil organic matter decomposition by heterotrop...
Rising global temperatures may increase the rates of soil organic matter decomposition by heterotrop...
Rising global temperatures may increase the rates of soil organic matter decomposition by heterotrop...
Microbes are responsible for cycling carbon (C) through soils, and predicted changes in soil C stock...
Microbes are responsible for cycling carbon (C) through soils, and predicted changes in soil C stock...
Microbes are responsible for cycling carbon (C) through soils, and predicted changes in soil C stock...
Microbes are responsible for cycling carbon (C) through soils, and predicted changes in soil C stock...
Microbes are responsible for cycling carbon (C) through soils, and predicted changes in soil C stock...
Soil microbial respiration and methanogenesis are key sources of atmospheric carbon. Conflicting evi...
The central objective of the proposed work was to develop a genomic approach (nucleic acid-based) th...
AbstractSoil microbial communities mediate the decomposition of soil organic matter (SOM). The amoun...
types: Journal Article; Research Support, Non-U.S. Gov'tThis a post-print, author-produced version o...
Understanding the mechanisms by which soil respiration responds to climate change is critical to p...
Author Posting. © The Author(s), 2008. This is the author's version of the work. It is posted here ...