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DOI10.1038/s41586-020-2233-9
Millennial-scale hydroclimate control of tropical soil carbon storage
Lam, Tommy Tsan-Yuk1,2; Jia, Na3; Zhang, Ya-Wei3; Shum, Marcus Ho-Hin2; Jiang, Jia-Fu3; Zhu, Hua-Chen1,2; Tong, Yi-Gang4; Shi, Yong-Xia5; Ni, Xue-Bing2; Liao, Yun-Shi2; Li, Wen-Juan4; Jiang, Bao-Gui3; Wei, Wei6; Yuan, Ting-Ting3; Zheng, Kui5; Cui, Xiao-Ming3; Li, Jie3; Pei, Guang-Qian3
2020-05-06
发表期刊NATURE
ISSN0028-0836
EISSN1476-4687
出版年2020
卷号581期号:7806页码:63-+
文章类型Article
语种英语
国家USA; Switzerland; Canada
英文关键词

Over the past 18,000 years, the residence time and amount of soil carbon stored in the Ganges-Brahmaputra basin have been controlled by the intensity of Indian Summer Monsoon rainfall, with greater carbon destabilization during wetter, warmer conditions.


The storage of organic carbon in the terrestrial biosphere directly affects atmospheric concentrations of carbon dioxide over a wide range of timescales. Within the terrestrial biosphere, the magnitude of carbon storage can vary in response to environmental perturbations such as changing temperature or hydroclimate(1), potentially generating feedback on the atmospheric inventory of carbon dioxide. Although temperature controls the storage of soil organic carbon at mid and high latitudes(2,3), hydroclimate may be the dominant driver of soil carbon persistence in the tropics(4,5) however, the sensitivity of tropical soil carbon turnover to large-scale hydroclimate variability remains poorly understood. Here we show that changes in Indian Summer Monsoon rainfall have controlled the residence time of soil carbon in the Ganges-Brahmaputra basin over the past 18,000 years. Comparison of radiocarbon ages of bulk organic carbon and terrestrial higher-plant biomarkers with co-located palaeohydrological records(6) reveals a negative relationship between monsoon rainfall and soil organic carbon stocks on a millennial timescale. Across the deglaciation period, a depletion of basin-wide soil carbon stocks was triggered by increasing rainfall and associated enhanced soil respiration rates. Our results suggest that future hydroclimate changes in tropical regions are likely to accelerate soil carbon destabilization, further increasing atmospheric carbon dioxide concentrations.


领域地球科学 ; 气候变化 ; 资源环境
收录类别SCI-E
WOS记录号WOS:000530868200011
WOS关键词ORGANIC-CARBON ; BENGAL FAN ; OLD CARBON ; CLIMATE ; OCEAN ; CYCLE ; CALIBRATION ; FEEDBACKS ; DISCHARGE ; RESPONSES
WOS类目Multidisciplinary Sciences
WOS研究方向Science & Technology - Other Topics
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引用统计
文献类型期刊论文
条目标识符http://119.78.100.173/C666/handle/2XK7JSWQ/249201
专题地球科学
资源环境科学
作者单位1.Shantou Univ, Guangdong Hongkong Joint Lab Emerging Infect Dis, Joint Inst Virol Shantou Univ & Univ Hong Kong, Shantou, Peoples R China;
2.Univ Hong Kong, Sch Publ Hlth, State Key Lab Emerging Infect Dis, Hong Kong, Peoples R China;
3.Beijing Inst Microbiol & Epidemiol, State Key Lab Pathogen & Biosecur, Beijing, Peoples R China;
4.Beijing Univ Chem Technol, Coll Life Sci & Technol, Beijing Adv Innovat Ctr Soft Matter Sci & Engn BA, Beijing, Peoples R China;
5.Guangzhou Customs Technol Ctr, Guangzhou, Peoples R China;
6.Guangxi Med Univ, Life Sci Inst, Nanning, Peoples R China;
7.Guangxi Med Univ, Sch Informat & Management, Nanning, Peoples R China;
8.Univ Sydney, Sch Life & Environm Sci, Marie Bashir Inst Infect Dis & Biosecur, Sydney, NSW, Australia;
9.Univ Sydney, Sch Med Sci, Sydney, NSW, Australia;
10.Guangxi Med Univ, Ctr Genom & Personalized Med, Nanning, Peoples R China
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Lam, Tommy Tsan-Yuk,Jia, Na,Zhang, Ya-Wei,et al. Millennial-scale hydroclimate control of tropical soil carbon storage[J]. NATURE,2020,581(7806):63-+.
APA Lam, Tommy Tsan-Yuk.,Jia, Na.,Zhang, Ya-Wei.,Shum, Marcus Ho-Hin.,Jiang, Jia-Fu.,...&Pei, Guang-Qian.(2020).Millennial-scale hydroclimate control of tropical soil carbon storage.NATURE,581(7806),63-+.
MLA Lam, Tommy Tsan-Yuk,et al."Millennial-scale hydroclimate control of tropical soil carbon storage".NATURE 581.7806(2020):63-+.
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