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Divergent changes in particulate and mineral-associated organic carbon upon permafrost thaw

Author

Listed:
  • Futing Liu

    (Chinese Academy of Forestry
    Chinese Academy of Sciences)

  • Shuqi Qin

    (Chinese Academy of Sciences
    University of Chinese Academy of Sciences)

  • Kai Fang

    (Chinese Academy of Sciences
    University of Chinese Academy of Sciences)

  • Leiyi Chen

    (Chinese Academy of Sciences)

  • Yunfeng Peng

    (Chinese Academy of Sciences)

  • Pete Smith

    (University of Aberdeen)

  • Yuanhe Yang

    (Chinese Academy of Sciences
    University of Chinese Academy of Sciences)

Abstract

Permafrost thaw can stimulate microbial decomposition and induce soil carbon (C) loss, potentially triggering a positive C-climate feedback. However, earlier observations have concentrated on bulk soil C dynamics upon permafrost thaw, with limited evidence involving soil C fractions. Here, we 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 permafrost thaw sequence and five additional thermokarst-impacted sites on the Tibetan Plateau. We find that topsoil POC content substantially decreases, while MAOC content remains stable and OC-Fe accumulates due to the enriched Fe oxides after permafrost thaw. Moreover, the proportion of MAOC and OC-Fe increases along the thaw sequence and at most of the thermokarst-impacted sites. The relatively enriched stable soil C fractions would alleviate microbial decomposition and weaken its feedback to climate warming over long-term thermokarst development.

Suggested Citation

  • Futing Liu & Shuqi Qin & Kai Fang & Leiyi Chen & Yunfeng Peng & Pete Smith & Yuanhe Yang, 2022. "Divergent changes in particulate and mineral-associated organic carbon upon permafrost thaw," Nature Communications, Nature, vol. 13(1), pages 1-10, December.
  • Handle: RePEc:nat:natcom:v:13:y:2022:i:1:d:10.1038_s41467-022-32681-7
    DOI: 10.1038/s41467-022-32681-7
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    References listed on IDEAS

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    1. Leiyi Chen & Li Liu & Chao Mao & Shuqi Qin & Jun Wang & Futing Liu & Sergey Blagodatsky & Guibiao Yang & Qiwen Zhang & Dianye Zhang & Jianchun Yu & Yuanhe Yang, 2018. "Nitrogen availability regulates topsoil carbon dynamics after permafrost thaw by altering microbial metabolic efficiency," Nature Communications, Nature, vol. 9(1), pages 1-11, December.
    2. Carmody K. McCalley & Ben J. Woodcroft & Suzanne B. Hodgkins & Richard A. Wehr & Eun-Hae Kim & Rhiannon Mondav & Patrick M. Crill & Jeffrey P. Chanton & Virginia I. Rich & Gene W. Tyson & Scott R. Sal, 2014. "Methane dynamics regulated by microbial community response to permafrost thaw," Nature, Nature, vol. 514(7523), pages 478-481, October.
    3. Wenjuan Huang & Steven J. Hall, 2017. "Elevated moisture stimulates carbon loss from mineral soils by releasing protected organic matter," Nature Communications, Nature, vol. 8(1), pages 1-10, December.
    4. Leiyi Chen & Junyi Liang & Shuqi Qin & Li Liu & Kai Fang & Yunping Xu & Jinzhi Ding & Fei Li & Yiqi Luo & Yuanhe Yang, 2016. "Determinants of carbon release from the active layer and permafrost deposits on the Tibetan Plateau," Nature Communications, Nature, vol. 7(1), pages 1-12, December.
    5. Monique S. Patzner & Carsten W. Mueller & Miroslava Malusova & Moritz Baur & Verena Nikeleit & Thomas Scholten & Carmen Hoeschen & James M. Byrne & Thomas Borch & Andreas Kappler & Casey Bryce, 2020. "Iron mineral dissolution releases iron and associated organic carbon during permafrost thaw," Nature Communications, Nature, vol. 11(1), pages 1-11, December.
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    7. Chunmei Chen & Steven J. Hall & Elizabeth Coward & Aaron Thompson, 2020. "Iron-mediated organic matter decomposition in humid soils can counteract protection," Nature Communications, Nature, vol. 11(1), pages 1-13, December.
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