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Divergent changes in particulate and mineral-associated organic carbon upon permafrost thaw | |
Liu, Futing1; Qin, Shuqi1,2; Fang, Kai1,2; Chen, Leiyi1; Peng, Yunfeng1; Smith, Pete3; Yang, Yuanhe1,2 | |
2022 | |
发表期刊 | NATURE COMMUNICATIONS |
卷号 | 13期号:1 |
摘要 | 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. Based on observations from thermokarst-impacted sites on the Tibetan Plateau, the authors find substantial particulate organic carbon loss but stable mineral-associated organic carbon and enriched iron-bound organic carbon upon permafrost thaw. |
学科领域 | Multidisciplinary Sciences |
DOI | 10.1038/s41467-022-32681-7 |
收录类别 | SCI |
语种 | 英语 |
WOS关键词 | SOIL CARBON ; MATTER FORMATION ; CLIMATE-CHANGE ; STABILIZATION ; PERSISTENCE ; NITROGEN ; BIODEGRADABILITY ; DECOMPOSITION ; MECHANISMS ; RELEVANCE |
WOS研究方向 | Science Citation Index Expanded (SCI-EXPANDED) |
WOS记录号 | WOS:000847533800011 |
出版者 | NATURE PORTFOLIO |
文献子类 | Article |
出版地 | BERLIN |
EISSN | 2041-1723 |
资助机构 | National Natural Science Foundation of China [31988102, 31825006, 91837312, 32101332] ; Second Tibetan Plateau Scientific Expedition and Research (STEP) program [2019QZKK0106, 2019QZKK0302] ; Fundamental Research Foundation of Chinese Academy of Forestry [CAFYBB2020MA008] |
作者邮箱 | yhyang@ibcas.ac.cn |
作品OA属性 | Green Published, gold |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://ir.ibcas.ac.cn/handle/2S10CLM1/28833 |
专题 | 植被与环境变化国家重点实验室 |
作者单位 | 1.Chinese Acad Forestry, Key Lab Forest Ecol & Environm, Natl Forestry & Grassland Adm, Ecol & Nat Conservat Inst, Beijing 100091, Peoples R China 2.Chinese Acad Sci, Inst Bot, State Key Lab Vegetat & Environm Change, Beijing 100093, Peoples R China 3.Univ Chinese Acad Sci, Beijing 100049, Peoples R China 4.Univ Aberdeen, Inst Biol & Environm Sci, Aberdeen AB24 3UU, Scotland |
推荐引用方式 GB/T 7714 | Liu, Futing,Qin, Shuqi,Fang, Kai,et al. Divergent changes in particulate and mineral-associated organic carbon upon permafrost thaw[J]. NATURE COMMUNICATIONS,2022,13(1). |
APA | Liu, Futing.,Qin, Shuqi.,Fang, Kai.,Chen, Leiyi.,Peng, Yunfeng.,...&Yang, Yuanhe.(2022).Divergent changes in particulate and mineral-associated organic carbon upon permafrost thaw.NATURE COMMUNICATIONS,13(1). |
MLA | Liu, Futing,et al."Divergent changes in particulate and mineral-associated organic carbon upon permafrost thaw".NATURE COMMUNICATIONS 13.1(2022). |
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Liu-2022-Divergent c(2102KB) | 期刊论文 | 出版稿 | 开放获取 | CC BY-NC-SA | 浏览 请求全文 |
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