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Carbon isotope of the Early Cretaceous sediments from the West Pacific and the Sulu orogenic belt: Implying the global atmospheric pCO2 changes during the Early Aptian Oceanic Anoxic Event 1a
Wu, Si-fan1,3; Li, Cong-ying1,2; Huang, Jing1
2023-03-01
发表期刊DEEP-SEA RESEARCH PART I-OCEANOGRAPHIC RESEARCH PAPERS
ISSN0967-0637
卷号193页码:9
通讯作者Li, Cong-ying(licongying@qdio.ac.cn) ; Huang, Jing(hjmail@qdio.ac.cn)
摘要Multiple lines of evidence revealed that enormous CO2 was input into the ocean-atmosphere system during Oceanic Anoxic Event 1a (OAE 1a), which led to a series of environmental perturbations (e.g. temperature rising, enhanced weathering, promoted primary productivity and marine anoxia). Among them, increased carbon isotope fractionation (Delta 13Ccarb-org) between the carbonate (delta 13Ccarb) and organic carbon (delta 13Corg) in the sedi-ments is one of the most important indicators to the enhanced atmospheric pCO2. However, only a few research reported high-resolution paired carbon isotopes during OAE 1a, which were almost limited around the western Tethys. Here, we report new paired carbon isotopes of the Early Cretaceous sediments from the ODP site 866A in the western Pacific and the Lingshan Island section in the Sulu orogenic belt. The delta 13Ccarb curves from both sections correlate well with OAE 1a, in which a positive delta 13Ccarb excursion is identified between the C3-C6 segments. The Delta 13Ccarb-org displays a-7-11 parts per thousand positive shift coinciding with the delta 13Ccarb excursion, indicating a remarkable increase and a gradual decrease in CO2 in water and atmosphere, which further support significant atmospheric pCO2 changes during OAE 1a on a global scale. The sediments also show a few variations in carbon isotope records during OAE 1a between different locations, which may reflect different influences from local environments, and the deviations of stratigraphic correlation and diagenesis cannot be ruled out either.
关键词Carbon isotope AtmosphericpCO2 Ocean Anoxic Event 1a Early Cretaceous Western Pacific East China
DOI10.1016/j.dsr.2022.103954
收录类别SCI
语种英语
资助项目Strategic Priority Research Program of the Chinese Academy of Sciences[XDA22050103] ; Strategic Priority Research Program of the Chinese Academy of Sciences[LSKJ202204100] ; National Natural Science Foundation of China[42176070]
WOS研究方向Oceanography
WOS类目Oceanography
WOS记录号WOS:000993062700001
出版者PERGAMON-ELSEVIER SCIENCE LTD
WOS关键词LINGSHAN ISLAND ; PAIRED DELTA-C-13(CARB) ; VOLCANIC-ROCKS ; ORGANIC-MATTER ; NORTH-AMERICA ; OAE 1A ; PALEOCEANOGRAPHY ; GEOCHEMISTRY ; EVOLUTION ; BASIN
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被引频次:1[WOS]   [WOS记录]     [WOS相关记录]
文献类型期刊论文
条目标识符http://ir.qdio.ac.cn/handle/337002/183151
专题深海极端环境与生命过程研究中心
通讯作者Li, Cong-ying; Huang, Jing
作者单位1.Chinese Acad Sci, Inst Oceanol, Ctr Deep Sea Res, Qingdao 266071, Peoples R China
2.Lab Marine Mineral Resources, Qingdao Natl Lab Marine Sci & Technol, Qingdao 266237, Peoples R China
3.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
第一作者单位深海极端环境与生命过程研究中心
通讯作者单位深海极端环境与生命过程研究中心
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Wu, Si-fan,Li, Cong-ying,Huang, Jing. Carbon isotope of the Early Cretaceous sediments from the West Pacific and the Sulu orogenic belt: Implying the global atmospheric pCO2 changes during the Early Aptian Oceanic Anoxic Event 1a[J]. DEEP-SEA RESEARCH PART I-OCEANOGRAPHIC RESEARCH PAPERS,2023,193:9.
APA Wu, Si-fan,Li, Cong-ying,&Huang, Jing.(2023).Carbon isotope of the Early Cretaceous sediments from the West Pacific and the Sulu orogenic belt: Implying the global atmospheric pCO2 changes during the Early Aptian Oceanic Anoxic Event 1a.DEEP-SEA RESEARCH PART I-OCEANOGRAPHIC RESEARCH PAPERS,193,9.
MLA Wu, Si-fan,et al."Carbon isotope of the Early Cretaceous sediments from the West Pacific and the Sulu orogenic belt: Implying the global atmospheric pCO2 changes during the Early Aptian Oceanic Anoxic Event 1a".DEEP-SEA RESEARCH PART I-OCEANOGRAPHIC RESEARCH PAPERS 193(2023):9.
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