Temperature and substrate availability are among the key factors controlling microbial metabolism. Therelative importance of these two drivers on soil organic matter turnover is, however, hotly debated. Inthis study, we investigated the effect of temperature changes on the potential enzyme activities involvedin C (phenol-oxidase) and N (protease and amidase) cycling by incubating peat soils collected in winterand summer at the two typical temperatures recorded in the field during these two distinct periods (4and 19 C, respectively). In addition, to evaluate the effect of substrate limitations, we also compared therespiration rates of the thermally adapted soils with and without plant litter additions. Results showedthat both collection seas...
As earth\u27s climate continues to warm, it is important to understand how the capacity of terrestri...
Thermal adaptations of soil microorganisms could mitigate or facilitate global warming effects on so...
Rising global temperatures may increase the rates of soil organic matter decomposition by heterotrop...
Temperature and substrate availability are among the key factors controlling microbial metabolism. T...
Northern peatlands constitute an important component of the global carbon (C) cycle due to their lon...
Northern peatlands constitute an important component of the global carbon (C) cycle due to their lon...
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...
Biological processes in soils are regulated in part by soil temperature, and there is currently cons...
The activities of extracellular enzymes, the proximate agents of decomposition in soils, are known t...
Rising global temperatures may increase the rates of soil organic matter decomposition by heterotrop...
Peatlands store vast amounts of carbon (C) within the global terrestrial biosphere. Drainage and cul...
Temperature acclimation of soil organic matter (SOM) decomposition is one of the major uncertainties...
Rising global temperatures may increase the rates of soil organic matter decomposition by heterotrop...
Microbial enzyme activities are the direct agents of organic matter decomposition, and thus play a c...
As earth\u27s climate continues to warm, it is important to understand how the capacity of terrestri...
Thermal adaptations of soil microorganisms could mitigate or facilitate global warming effects on so...
Rising global temperatures may increase the rates of soil organic matter decomposition by heterotrop...
Temperature and substrate availability are among the key factors controlling microbial metabolism. T...
Northern peatlands constitute an important component of the global carbon (C) cycle due to their lon...
Northern peatlands constitute an important component of the global carbon (C) cycle due to their lon...
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...
Biological processes in soils are regulated in part by soil temperature, and there is currently cons...
The activities of extracellular enzymes, the proximate agents of decomposition in soils, are known t...
Rising global temperatures may increase the rates of soil organic matter decomposition by heterotrop...
Peatlands store vast amounts of carbon (C) within the global terrestrial biosphere. Drainage and cul...
Temperature acclimation of soil organic matter (SOM) decomposition is one of the major uncertainties...
Rising global temperatures may increase the rates of soil organic matter decomposition by heterotrop...
Microbial enzyme activities are the direct agents of organic matter decomposition, and thus play a c...
As earth\u27s climate continues to warm, it is important to understand how the capacity of terrestri...
Thermal adaptations of soil microorganisms could mitigate or facilitate global warming effects on so...
Rising global temperatures may increase the rates of soil organic matter decomposition by heterotrop...