The status and stability of permafrost carbon on the Tibetan Plateau
Permafrost regions at high latitudes and altitudes store about half of the Earth's soil organic
carbon (SOC). These areas are also some of the most intensely affected by anthropogenic …
carbon (SOC). These areas are also some of the most intensely affected by anthropogenic …
[HTML][HTML] Arctic soil microbial diversity in a changing world
The Arctic region is a unique environment, subject to extreme environmental conditions,
shaping life therein and contributing to its sensitivity to environmental change. The Arctic is …
shaping life therein and contributing to its sensitivity to environmental change. The Arctic is …
Determinants of carbon release from the active layer and permafrost deposits on the Tibetan Plateau
The sign and magnitude of permafrost carbon (C)-climate feedback are highly uncertain due
to the limited understanding of the decomposability of thawing permafrost and relevant …
to the limited understanding of the decomposability of thawing permafrost and relevant …
Temperature sensitivity of permafrost carbon release mediated by mineral and microbial properties
Temperature sensitivity (Q 10) of permafrost carbon (C) release upon thaw is a vital
parameter for projecting permafrost C dynamics under climate warming. However, it remains …
parameter for projecting permafrost C dynamics under climate warming. However, it remains …
Rising temperature may trigger deep soil carbon loss across forest ecosystems
Significantly more carbon (C) is stored in deep soil than in shallow horizons, yet how the
decomposition of deep soil organic C (SOC) will respond to rising temperature remains …
decomposition of deep soil organic C (SOC) will respond to rising temperature remains …
Biochar persistence, priming and microbial responses to pyrolysis temperature series
Biochar and its properties can be significantly altered according to how it is produced, and
this has ramifications towards how biochar behaves once added to soil. We produced …
this has ramifications towards how biochar behaves once added to soil. We produced …
Temperature sensitivity (Q10) of stable, primed and easily available organic matter pools during decomposition in paddy soil
The response of stable and labile C pools to global warming is uncertain, especially in
paddy soils with very low oxygen availability and the dominance of electron acceptors with …
paddy soils with very low oxygen availability and the dominance of electron acceptors with …
The temperature sensitivity of soil organic carbon decomposition is greater in subsoil than in topsoil during laboratory incubation
The turnover of soil organic carbon (SOC) in cropland plays an important role in terrestrial
carbon cycling, but little is known about the temperature sensitivity (Q 10) of SOC …
carbon cycling, but little is known about the temperature sensitivity (Q 10) of SOC …
Carbon dioxide and methane release following abrupt thaw of Pleistocene permafrost deposits in Arctic Siberia
C Knoblauch, C Beer, A Schuett… - Journal of …, 2021 - Wiley Online Library
The decomposition of thawing permafrost organic matter (OM) to the greenhouse gases
(GHG) carbon dioxide (CO2) and methane forms a positive feedback to global climate …
(GHG) carbon dioxide (CO2) and methane forms a positive feedback to global climate …
[HTML][HTML] Temperature sensitivity of soil organic matter decomposition after forest fire in Canadian permafrost region
H Aaltonen, M Palviainen, X Zhou, E Köster… - Journal of environmental …, 2019 - Elsevier
Climate warming in arctic/subarctic ecosystems will result in increased frequency of forest
fires, elevated soil temperatures and thawing of permafrost, which have implications for soil …
fires, elevated soil temperatures and thawing of permafrost, which have implications for soil …