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Shallow ocean deoxygenation drove trilobite turnover during the late Cambrian SPICE event
Yang, Aihua1; Chen, Bo2; Sun, Zhixin2,3; Tostevin, Rosalie4; He, Tianchen5; Chen, Xi1; Chen, Jitao2; Lu, Miao2; Hu, Chunlin2; Du, Shengxian6; Chen, Jun6; Jiao, Wenjun7; Zhu, Maoyan2,3
2024-06-17
发表期刊GEOLOGY
ISSN0091-7613
页码6
通讯作者Chen, Bo(chenbo@nigpas.ac.cn)
摘要The spread of marine anoxia is believed to have played a key role in the development of the SPICE (Steptoean Positive Carbon Isotope Excursion) event and the end-Marjuman extinction in the late Cambrian (similar to 497.5 m.y. ago), but their cause-and-effect relationship is poorly constrained. Here we present an integrated analysis of carbonate delta 13C, cerium anomalies (Ce/Ce*), and genus-level diversity data of trilobites from the North China Platform. Our results show tightly coupled changes between the SPICE, an increase in Ce/Ce*, and a trilobite turnover event, which we interpret as indicating enhanced productivity and organic remineralization, leading to the development of low-oxygen conditions in shallowwater settings. This study therefore establishes a direct link between local ecological stress and trilobite turnover during the global SPICE event. Furthermore, the presence of low-oxygen rather than fully anoxic conditions during the peak of the SPICE event could explain the nature of the end-Marjuman crisis, which was characterized by the replacement of shallowwater fauna by deeper-water counterparts that were potentially more tolerant of hypoxia.
DOI10.1130/G52200.1
收录类别SCI
语种英语
资助项目National Key R&D Program of China[2022YFF0800100] ; National Natural Science Foundation of China[41921002] ; National Natural Science Foundation of China[41872011] ; National Natural Science Foundation of China[42073006] ; Fundamental Research Funds for the Central Universities of China[0206-14380137] ; NRF-COE (South African National Research Foundation Centre of Excellence) GENUS ; South African Biogeo-chemistry Research Infrastructure Platform (BIOGRIP) ; Jiangsu Specially-Appointed Professor Award
WOS研究方向Geology
WOS类目Geology
WOS记录号WOS:001249890200001
出版者GEOLOGICAL SOC AMER, INC
WOS关键词RARE-EARTH-ELEMENT ; DIAGENESIS ; STRATIGRAPHY ; EXTINCTIONS ; EUXINIA ; OXYGEN
引用统计
文献类型期刊论文
条目标识符http://ir.qdio.ac.cn/handle/337002/186504
专题海洋地质与环境重点实验室
通讯作者Chen, Bo
作者单位1.Nanjing Univ, Sch Earth Sci & Engn, Nanjing 210023, Peoples R China
2.Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, State Key Lab Palaeobiol & Stratig, Nanjing 210008, Peoples R China
3.Univ CAS, Coll Earth & Planetary Sci, Beijing 100049, Peoples R China
4.Univ Cape Town, Dept Geol Sci, ZA-7701 Cape Town, South Africa
5.Hohai Univ, Coll Oceanog, Nanjing 210024, Peoples R China
6.Shandong Inst Geol Sci, Jinan 250013, Peoples R China
7.Chinese Acad Sci, Inst Oceanol, Key Lab Marine Geol & Environm, Qingdao 266071, Peoples R China
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GB/T 7714
Yang, Aihua,Chen, Bo,Sun, Zhixin,et al. Shallow ocean deoxygenation drove trilobite turnover during the late Cambrian SPICE event[J]. GEOLOGY,2024:6.
APA Yang, Aihua.,Chen, Bo.,Sun, Zhixin.,Tostevin, Rosalie.,He, Tianchen.,...&Zhu, Maoyan.(2024).Shallow ocean deoxygenation drove trilobite turnover during the late Cambrian SPICE event.GEOLOGY,6.
MLA Yang, Aihua,et al."Shallow ocean deoxygenation drove trilobite turnover during the late Cambrian SPICE event".GEOLOGY (2024):6.
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