Understanding the effects of elevated temperatures on soil organic matter (SOM) decomposition pathways in northern peatlands is central to predicting their fate under future warming. Peatlands role as carbon (C) sink is dependent on both anoxic conditions and low temperatures that limit SOM decomposition. Previous studies have shown that elevated temperatures due to climate change can disrupt peatland's C balance by enhancing SOM decomposition and increasing CO2 emissions. However, little is known about how SOM decomposition pathways change at higher temperatures. Here, we used an integrated research approach to investigate the mechanisms behind enhanced CO2 emissions and SOM decomposition under elevated temperatures of surface peat soil co...
[1] The response of large stores of carbon in boreal forest soils to global warming is a major uncer...
Boreal peatlands currently contain 550 Pg C and are located at high latitudes where mean annual temp...
Climate warming is expected to accelerate peatland degradation and release rates of carbon dioxide (...
Rising temperatures have the potential to directly affect carbon cycling in peatlands by enhancing o...
More than one third of global soil organic matter (SOM) is stored in peatlands, despite them occupyi...
Northern peatlands constitute an important component of the global carbon (C) cycle due to their lon...
Extreme climate events are predicted to become more frequent and intense. Their ecological impacts, ...
Northern peatlands constitute an important component of the global carbon (C) cycle due to their lon...
Peatlands contain one-third of soil carbon (C), mostly buried in deep, saturated anoxic zones (catot...
Large tracts of arctic and subarctic peatlands are underlain by permafrost. These peatlands store la...
Peatlands, which store one third of the terrestrial carbon (C), are subject to large disturbances un...
Feedbacks to global warming may cause terrestrial ecosystems to add to anthropogenic CO2 emissions, ...
Abstract Peatlands are an important carbon (C) reservoir storing one-third of global soil organic ca...
Peatlands act as global sinks of atmospheric carbon (C) through the accumulation of organic matter, ...
The peatland carbon store is threatened by climate change and is expected to provide positive feedba...
[1] The response of large stores of carbon in boreal forest soils to global warming is a major uncer...
Boreal peatlands currently contain 550 Pg C and are located at high latitudes where mean annual temp...
Climate warming is expected to accelerate peatland degradation and release rates of carbon dioxide (...
Rising temperatures have the potential to directly affect carbon cycling in peatlands by enhancing o...
More than one third of global soil organic matter (SOM) is stored in peatlands, despite them occupyi...
Northern peatlands constitute an important component of the global carbon (C) cycle due to their lon...
Extreme climate events are predicted to become more frequent and intense. Their ecological impacts, ...
Northern peatlands constitute an important component of the global carbon (C) cycle due to their lon...
Peatlands contain one-third of soil carbon (C), mostly buried in deep, saturated anoxic zones (catot...
Large tracts of arctic and subarctic peatlands are underlain by permafrost. These peatlands store la...
Peatlands, which store one third of the terrestrial carbon (C), are subject to large disturbances un...
Feedbacks to global warming may cause terrestrial ecosystems to add to anthropogenic CO2 emissions, ...
Abstract Peatlands are an important carbon (C) reservoir storing one-third of global soil organic ca...
Peatlands act as global sinks of atmospheric carbon (C) through the accumulation of organic matter, ...
The peatland carbon store is threatened by climate change and is expected to provide positive feedba...
[1] The response of large stores of carbon in boreal forest soils to global warming is a major uncer...
Boreal peatlands currently contain 550 Pg C and are located at high latitudes where mean annual temp...
Climate warming is expected to accelerate peatland degradation and release rates of carbon dioxide (...