Partially decomposed plant and animal remains have been accumulating in organic soils (i.e.>40% C content) for mil- lennia, making them the largest terrestrial carbon store. There is growing concern that, in a warming world, soil biotic processing will accelerate and release greenhouse gases that further exacerbate climate change. However, the magnitude of this response remains uncertain as the constraints are abiotic, biotic and interactive. Here, we examined the influence of resource quality and biological activity on the temperature sensitivity of soil respiration under different soil moisture regimes. Organic soils were sampled from 13 boreal and peatland ecosystems located in the United Kingdom, Ireland, Spain, Finland and Sweden, rep...
[1] One predicted positive feedback of increasing temperatures in the boreal region is carbon (C) lo...
Northern peatlands constitute an important component of the global carbon (C) cycle due to their lon...
The climate is changing and with it the capacity of soils to store carbon in all likelihood, since t...
Feedbacks to global warming may cause terrestrial ecosystems to add to anthropogenic CO<sub>2&...
Soil stores more carbon (C) than plants and atmosphere combined and it is vulnerable to increased mi...
Feedbacks to global warming may cause terrestrial ecosystems to add to anthropogenic CO2 emissions, ...
Feedbacks to global warming may cause terrestrial ecosystems to add to anthropogenic CO2 emissions, ...
Biogeochemical cycles, such as the carbon (C) cycle, are being continuously affected by anthropogeni...
Determining the temperature sensitivity of terrestrial carbon (C) stores is an urgent priority for p...
A positive soil carbon (C)−climate feedback is embedded into the climatic models of the IPCC. Howeve...
A positive soil carbon (C)-climate feedback is embedded into the climatic models of the IPCC. Howeve...
Soil carbon losses to the atmosphere through soil respiration are expected to rise with ongoing temp...
Northern peatlands constitute an important component of the global carbon (C) cycle due to their lon...
types: Journal Article; Research Support, Non-U.S. Gov'tThis a post-print, author-produced version o...
Soils store about four times as much carbon as plant biomass1, and soil microbial respiration releas...
[1] One predicted positive feedback of increasing temperatures in the boreal region is carbon (C) lo...
Northern peatlands constitute an important component of the global carbon (C) cycle due to their lon...
The climate is changing and with it the capacity of soils to store carbon in all likelihood, since t...
Feedbacks to global warming may cause terrestrial ecosystems to add to anthropogenic CO<sub>2&...
Soil stores more carbon (C) than plants and atmosphere combined and it is vulnerable to increased mi...
Feedbacks to global warming may cause terrestrial ecosystems to add to anthropogenic CO2 emissions, ...
Feedbacks to global warming may cause terrestrial ecosystems to add to anthropogenic CO2 emissions, ...
Biogeochemical cycles, such as the carbon (C) cycle, are being continuously affected by anthropogeni...
Determining the temperature sensitivity of terrestrial carbon (C) stores is an urgent priority for p...
A positive soil carbon (C)−climate feedback is embedded into the climatic models of the IPCC. Howeve...
A positive soil carbon (C)-climate feedback is embedded into the climatic models of the IPCC. Howeve...
Soil carbon losses to the atmosphere through soil respiration are expected to rise with ongoing temp...
Northern peatlands constitute an important component of the global carbon (C) cycle due to their lon...
types: Journal Article; Research Support, Non-U.S. Gov'tThis a post-print, author-produced version o...
Soils store about four times as much carbon as plant biomass1, and soil microbial respiration releas...
[1] One predicted positive feedback of increasing temperatures in the boreal region is carbon (C) lo...
Northern peatlands constitute an important component of the global carbon (C) cycle due to their lon...
The climate is changing and with it the capacity of soils to store carbon in all likelihood, since t...