Futing Liu
Chinese Academy of Sciences
19 Papers
Futing Liu is an academic researcher from Chinese Academy of Sciences. The author has contributed to research in topics: Permafrost & Chemistry. The author has an hindex of 7, co-authored 13 publications.
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Papers
Nitrogen availability regulates topsoil carbon dynamics after permafrost thaw by altering microbial metabolic efficiency.
Leiyi Chen,Li Liu,Chao Mao,Shuqi Qin,Jun Wang,Futing Liu,Sergey Blagodatsky,Guibiao Yang,Qiwen Zhang,Dianye Zhang,Jianchun Yu,Yuanhe Yang +11 more
TL;DR: Soil nitrogen availability may alter carbon dynamics after permafrost thaw, but experimental evidence for this carbon-nitrogen interaction is still lacking, soil carbon release is inhibited through its enhancement in microbial metabolic efficiency.
Temperature sensitivity of SOM decomposition governed by aggregate protection and microbial communities
TL;DR: It is found that lower microbial abundance and stronger aggregate protection were coexisting mechanisms underlying the lower Q10 in the subsoil, which highlights the crucial role of soil C stabilization mechanisms in regulating temperature response of SOM decomposition, potentially attenuating the terrestrial C-climate feedback.
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Large-scale evidence for microbial response and associated carbon release after permafrost thaw
Yongliang Chen,Yongliang Chen,Futing Liu,Luyao Kang,Dianye Zhang,Dan Kou,Chao Mao,Shuqi Qin,Qiwen Zhang,Yuanhe Yang +9 more
TL;DR: It is demonstrated that permafrost thaw could accelerate C emissions by altering the function potentials of microbial communities rather than taxonomic diversity, highlighting the crucial role of microbial functional genes in mediating the responses ofpermafrost C cycle to climate warming.
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Divergent changes in particulate and mineral-associated organic carbon upon permafrost thaw
TL;DR: In this paper , the authors explore how the functionally distinct fractions, including particulate and mineral-associated organic C (POC and MAOC), as well as iron-bound organic C(OC-Fe), respond to permafrost thaw using systematic measurements derived from one permafure thaw sequence and five additional thermokarst-impacted sites on the Tibetan Plateau.
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Phosphorus rather than nitrogen regulates ecosystem carbon dynamics after permafrost thaw.
Guibiao Yang,Yunfeng Peng,Benjamin W. Abbott,Christina Biasi,Bin Wei,Dianye Zhang,Jun Wang,Jianchun Yu,Fei Li,Guanqin Wang,Dan Kou,Dan Kou,Futing Liu,Yuanhe Yang +13 more
TL;DR: In this article, the potential role of soil phosphorus (P) availability in permafrost thaw has been investigated and it was found that changes in soil P availability rather than nitrogen availability played an important role in regulating gross primary productivity and net ecosystem productivity along the thaw sequence.
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