The response of soil organic matter (OM) decomposition to increasing temperature is a
critical aspect of ecosystem responses to global change. The impacts of climate warming on …

Temperature regulates the rate of biogeochemical cycles. One way it does so is through
control of microbial metabolism. Warming effects on metabolism change with time as …

土壤呼吸是陆地生态系统碳循环的重要环节之一, 其对温度升高的敏感程度在很大程度上决定着
全球气候变化与碳循环之间的反馈关系. 为了深刻理解地下生态过程对气候变化的响应和适应 …

Temperature sensitivity (Q10) of soil organic matter (SOM) decomposition is a crucial
parameter to predict the fate of soil carbon (C) under global warming. Nonetheless, the …

The temperature sensitivity (Q 10) of soil respiration (Rs) is crucial to assess the carbon (C)
budget of terrestrial ecosystems under global warming. The Q 10 changes along a climatic …

Soil organic matter (SOM) represents one of the largest reservoirs of carbon on the global
scale. Thus, the temperature sensitivity of bulk SOM and of different SOM fractions is a key …

The elevational pattern of soil microbial diversity along mountain slopes has received
considerable interest over the last decade. An increasing amount of taxonomic data on soil …

Microbial breakdown of soil organic matter influences the potential for terrestrial ecosystems
to sequester carbon, and the amount of carbon dioxide released to the atmosphere …

The temperature sensitivity of soil respiration is a main factor determining the response of
global terrestrial soil carbon to global warming and, consequently, its feedback on …

Plant-microbial interactions alter C and N balance in the rhizosphere and affect the microbial
carbon use efficiency (CUE)–the fundamental characteristic of microbial metabolism …