Reduced microbial stability in the active layer is associated with carbon loss under alpine permafrost degradation

Reduced microbial stability in the active layer is associated with carbon loss under alpine permafrost degradation
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活性层微生物稳定性降低与高山永久冻土退化下的碳损失有关

DOI:
10.1073/pnas.2025321118
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发表时间:
2021-06
影响因子:
11.1
通讯作者:
Wang Yanfen
Wang Yanfen
中科院分区:
综合性期刊1区
文献类型:
--
作者:
Minghui Wu;Shengyun Chen;Jianwei Chen;Kai Xue;Shilong Chen;Xiaoming Wang;Tuo Chen;Shichang Kang;Junpeng Rui;Thies E. Janice;Bardgett D. Richard;Wang Yanfen

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冻土退化可能导致土壤碳(C)损失,这对全球碳循环至关重要,并由微生物介导。我们在原地证明,永久冻土退化改变了多样性,并可能降低活性层微生物群落的稳定性。这些变化与土壤碳流失和潜在的正碳反馈有关。这项研究提供了微生物介导的机制,负责退化的永久冻土活动层内的碳损失,有助于模拟未来情景下的碳排放。
Permafrost degradation may induce soil carbon (C) loss, critical for global C cycling, and be mediated by microbes. Despite larger C stored within the active layer of permafrost regions, which are more affected by warming, and the critical roles of Qinghai-Tibet Plateau in C cycling, most previous studies focused on the permafrost layer and in high-latitude areas. We demonstrate in situ that permafrost degradation alters the diversity and potentially decreases the stability of active layer microbial communities. These changes are associated with soil C loss and potentially a positive C feedback. This study provides insights into microbial-mediated mechanisms responsible for C loss within the active layer in degraded permafrost, aiding in the modeling of C emission under future scenarios.
DOI: 10.1073/pnas.1003577107
发表时间: 2010-09
期刊: Proceedings of the National Academy of Sciences
影响因子: --
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