中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Human Activities Induced Stronger Silicate Weathering in the Red River Basin: A Growing Carbon Sink During the Late Holocene

文献类型:期刊论文

作者Wang, Xiaowei5,6; Wan, Shiming4,6; Clift, Peter D.2,3; Zhao, Debo6; Cai, Guanqiang1; Yang, Yifei6; Zhang, Jin6; Yu, Zhaojie6; Jin, Hualong6; Song, Zehua6
刊名JOURNAL OF GEOPHYSICAL RESEARCH-EARTH SURFACE
出版日期2025-10-24
卷号130期号:10页码:19
关键词silicate weathering human activities carbon cycle Red River Basin South China Sea late Holocene
ISSN号2169-9003
DOI10.1029/2025JF008433
通讯作者Wan, Shiming(wanshiming@ms.qdio.ac.cn) ; Zhao, Debo(zhaodebo@qdio.ac.cn)
英文摘要Silicate weathering is essential for the global carbon cycle and is a driver of climate change through the consumption of atmospheric CO2. Recent studies have pointed out that silicate weathering in the late Holocene was widely influenced by human activities, but the carbon sink effect of silicate weathering under anthropogenic influence remains unclear. In this study, we present continuous records of clay minerals, major elements, and terrigenous mass accumulation rates of Core 45A in the Western South China Sea to reconstruct the evolutionary history of weathering and erosion in the Red River Basin since 3800 cal yr BP. We investigate the interactions between weathering, climate, and human activities. Our results reveal that the silicate weathering intensity and erosion rate have increased significantly since similar to 1500 cal yr BP, which is decoupled from the trend to a cooler and drier climate but coincides well with stronger human activities, suggesting the significance of anthropogenic influence on silicate weathering. We also reconstruct the CO2 consumption flux induced by silicate weathering to quantitatively evaluate the impact of human activities on the carbon sink capacity of silicate weathering. The calculated CO2 consumption fluxes contributed by anthropogenic activities on silicate weathering show an approximate 150% increase compared to natural conditions in the Red River. Thus, this study highlights that human-enhanced silicate weathering has reduced atmospheric CO2 and played an important role in the global carbon cycle during the late Holocene, which has never occurred in the Earth's geological past.
WOS关键词NORTHWESTERN YUNNAN PROVINCE ; CLAY MINERAL ASSEMBLAGES ; SOUTH CHINA SEA ; ASIAN MONSOON ; CLIMATE-CHANGE ; HUMAN IMPACT ; LAND-USE ; GLOBAL CARBON ; LAKE ERHAI ; SEDIMENT
资助项目Strategic Priority Research Program of Chinese Academy Sciences
WOS研究方向Geology
语种英语
WOS记录号WOS:001599721900001
出版者AMER GEOPHYSICAL UNION
源URL[http://ir.qdio.ac.cn/handle/337002/203662]  
专题海洋研究所_海洋地质与环境重点实验室
通讯作者Wan, Shiming; Zhao, Debo
作者单位1.Guangzhou Marine Geol Survey, Guangzhou, Peoples R China
2.Univ Szczecin, Inst Marine & Environm Sci, Szczecin, Poland
3.UCL, Dept Earth Sci, London, England
4.Qingdao Marine Sci & Technol Ctr, Lab Marine Geol, Qingdao, Peoples R China
5.Univ Chinese Acad Sci, Beijing, Peoples R China
6.Chinese Acad Sci, Inst Oceanol, Key Lab Marine Geol & Environm, Qingdao, Peoples R China
推荐引用方式
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Wang, Xiaowei,Wan, Shiming,Clift, Peter D.,et al. Human Activities Induced Stronger Silicate Weathering in the Red River Basin: A Growing Carbon Sink During the Late Holocene[J]. JOURNAL OF GEOPHYSICAL RESEARCH-EARTH SURFACE,2025,130(10):19.
APA Wang, Xiaowei.,Wan, Shiming.,Clift, Peter D..,Zhao, Debo.,Cai, Guanqiang.,...&Li, Anchun.(2025).Human Activities Induced Stronger Silicate Weathering in the Red River Basin: A Growing Carbon Sink During the Late Holocene.JOURNAL OF GEOPHYSICAL RESEARCH-EARTH SURFACE,130(10),19.
MLA Wang, Xiaowei,et al."Human Activities Induced Stronger Silicate Weathering in the Red River Basin: A Growing Carbon Sink During the Late Holocene".JOURNAL OF GEOPHYSICAL RESEARCH-EARTH SURFACE 130.10(2025):19.

入库方式: OAI收割

来源:海洋研究所

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