Climate warming is predicted to considerably affect variations in soil organic carbon (SOC), especially in alpine ecosystems. Microbial necromass carbon (MNC) is an important contributor to stable soil organic carbon pools. However, accumulation and persistence of soil MNC across a gradient of warming are still poorly understood. An eight-year field experiment with four levels of warming was conducted in a Tibetan meadow. We found that low-level (+0-1.5 ℃) warming mostly enhanced bacterial necromass carbon (BNC), fungal necromass carbon (FNC), and total MNC compared with control treatment across soil layers, while no significant effect was caused between high-level (+1.5-2.5 ℃) treatments and control treatments. The contributions of both MN...
Soil microbial communities regulate soil carbon feedbacks to climate warming through microbial respi...
Information on how soil microbial communities respond to warming is still scarce for alpine scrub ec...
The alpine grasslands of the Tibetan Plateau store 23.2 Pg soil organic carbon (SOC), which becomes ...
Current consensus on global climate change predicts warming trends with more pronounced temperature ...
As climate cooling is increasingly regarded as important natural variability of long-term global war...
Warming is known to reduce soil carbon (C) stocks by promoting microbial respiration, which is assoc...
Warming has been shown to cause soil carbon (C) loss in northern grasslands owing to accelerated mic...
Subsoils of alpine grasslands on the Qinghai-Tibetan Plateau represent a tremendous yet poorly inves...
Warming has been shown to cause soil carbon (C) loss in northern grasslands owing to accelerated mic...
Previous studies have explored the effects of global change on above-ground vegetation in grassland ...
Soil microbes are directly involved in soil organic carbon (SOC) decomposition, yet the importance o...
Subsoils of alpine grasslands on the Qinghai-Tibetan Plateau represent a tremendous yet poorly inves...
Changes in labile carbon (LC) pools and microbial communities are the primary factors controlling so...
In order to understand the response of soil microbial biomass to warming, field warming experiments ...
Soil microbial communities regulate soil carbon feedbacks to climate warming through microbial respi...
Information on how soil microbial communities respond to warming is still scarce for alpine scrub ec...
The alpine grasslands of the Tibetan Plateau store 23.2 Pg soil organic carbon (SOC), which becomes ...
Current consensus on global climate change predicts warming trends with more pronounced temperature ...
As climate cooling is increasingly regarded as important natural variability of long-term global war...
Warming is known to reduce soil carbon (C) stocks by promoting microbial respiration, which is assoc...
Warming has been shown to cause soil carbon (C) loss in northern grasslands owing to accelerated mic...
Subsoils of alpine grasslands on the Qinghai-Tibetan Plateau represent a tremendous yet poorly inves...
Warming has been shown to cause soil carbon (C) loss in northern grasslands owing to accelerated mic...
Previous studies have explored the effects of global change on above-ground vegetation in grassland ...
Soil microbes are directly involved in soil organic carbon (SOC) decomposition, yet the importance o...
Subsoils of alpine grasslands on the Qinghai-Tibetan Plateau represent a tremendous yet poorly inves...
Changes in labile carbon (LC) pools and microbial communities are the primary factors controlling so...
In order to understand the response of soil microbial biomass to warming, field warming experiments ...
Soil microbial communities regulate soil carbon feedbacks to climate warming through microbial respi...
Information on how soil microbial communities respond to warming is still scarce for alpine scrub ec...
The alpine grasslands of the Tibetan Plateau store 23.2 Pg soil organic carbon (SOC), which becomes ...