NIGPAS OpenIR
Global microbial carbonate proliferation after the end-Devonian mass extinction: Mainly controlled by demise of skeletal bioconstructors
Yao, Le (要乐)1,2,3; Aretz, Markus3; Chen, Jitao (陈吉涛)1; Webb, Gregory E.4; Wang, Xiangdong (王向东)1
2016-12-23
发表期刊SCIENTIFIC REPORTS
ISSN2045-2322
卷号6页码:9
摘要

Microbial carbonates commonly flourished following mass extinction events. The end-Devonian (Hangenberg) mass extinction event is a first-order mass extinction on the scale of the 'Big Five' extinctions. However, to date, it is still unclear whether global microbial carbonate proliferation occurred after the Hangenberg event. The earliest known Carboniferous stromatolites on tidal flats are described from intertidal environments of the lowermost Tournaisian (Qianheishan Formation) in northwestern China. With other early Tournaisian microbe-dominated bioconstructions extensively distributed on shelves, the Qianheishan stromatolites support microbial carbonate proliferation after the Hangenberg extinction. Additional support comes from quantitative analysis of the abundance of microbe-dominated bioconstructions through the Famennian and early Tournaisian, which shows that they were globally distributed (between 40 degrees latitude on both sides of the palaeoequator) and that their abundance increased distinctly in the early Tournaisian compared to the latest Devonian (Strunian). Comparison of variations in the relative abundance of skeleton-versus microbe-dominated bioconstructions across the Hangenberg and 'Big Five' extinctions suggests that changes in abundance of skeletal bioconstructors may play a first-order control on microbial carbonate proliferation during extinction transitions but that microbial proliferation is not a general necessary feature after mass extinctions.

DOI10.1038/srep39694
语种英语
关键词[WOS]Stromatolite Reef ; Gudman Formation ; Disaster Forms ; South China ; Australia ; Metazoan ; Event ; Precipitation ; Queensland ; Aftermath
资助项目Chinese Academy of Sciences[XDB18030400] ; National Natural Science Foundation of China[41290260] ; National Natural Science Foundation of China[41290262] ; Ministry of Science and Technology Foundation ; CNRS-INSU (SYSTER)
WOS研究方向Science & Technology - Other Topics
WOS类目Multidisciplinary Sciences
WOS记录号WOS:000390753700001
项目资助者Chinese Academy of Sciences ; National Natural Science Foundation of China ; Ministry of Science and Technology Foundation ; CNRS-INSU (SYSTER)
出版者NATURE PUBLISHING GROUP
文献类型期刊论文
条目标识符http://ir.nigpas.ac.cn/handle/332004/20848
专题中国科学院南京地质古生物研究所
其他
通讯作者Aretz, Markus; Wang, Xiangdong (王向东)
作者单位1.Chinese Acad Sci, Key Lab Econ Stratig & Palaeogeog, Nanjing Inst Geol & Palaeontol, Nanjing 210008, Jiangsu, Peoples R China
2.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
3.Univ Toulouse, UPS OMP, GET, 14 Ave Edouard Belin, F-31400 Toulouse, France
4.Univ Queensland, Sch Earth Sci, St Lucia, Qld 4072, Australia
推荐引用方式
GB/T 7714
Yao, Le ,Aretz, Markus,Chen, Jitao ,et al. Global microbial carbonate proliferation after the end-Devonian mass extinction: Mainly controlled by demise of skeletal bioconstructors[J]. SCIENTIFIC REPORTS,2016,6:9.
APA Yao, Le ,Aretz, Markus,Chen, Jitao ,Webb, Gregory E.,&Wang, Xiangdong .(2016).Global microbial carbonate proliferation after the end-Devonian mass extinction: Mainly controlled by demise of skeletal bioconstructors.SCIENTIFIC REPORTS,6,9.
MLA Yao, Le ,et al."Global microbial carbonate proliferation after the end-Devonian mass extinction: Mainly controlled by demise of skeletal bioconstructors".SCIENTIFIC REPORTS 6(2016):9.
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