Enhanced organic carbon burial intensified the end-Ordovician glaciation

doi:10.7185/geochemlet.2210

NIGPAS OpenIR

	Enhanced organic carbon burial intensified the end-Ordovician glaciation
通讯作者	Liu, S-A([email protected])
	Lv, Y.1,2; Liu, S-A 1,2; Wu, H.3; Sun, Z.4; Li, C.5,6; Fan, J. X.7
	2022-03-25
发表期刊	GEOCHEMICAL PERSPECTIVES LETTERS
ISSN	2410-339X
卷号	21 页码:13-+
摘要	The end-Ordovician (Hirnantian) glaciation, causally linked with the first of five Phanerozoic mass extinction events, is the first major Phanerozoic-glaciation with short duration and paradoxically happened under a relative greenhouse-condition. Here, we present the first zinc isotope study on both carbonate and shale successions that span the Ordovician-Silurian boundary interval in South China. Two positive shifts in Zn isotope composition are observed during two main periods of glacial maxima, indicative of two pulses of extensive carbon burial. The enhanced organic carbon burial during glacial maxima intervals might be causatively linked to cooling- induced elevation in organic carbon burial efficiency. This implies that a large oceanic organic carbon reservoir played a vital role in regulating the atmospheric pCO(2), causing the Hirnantian glaciation and producing the pattern of glacial-to-deglacial change, sensitive to the temperature effect.
DOI	10.7185/geochemlet.2210
收录类别	SCI
语种	英语
关键词[WOS]	ZINC ISOTOPE FRACTIONATION ; OCEANIC MASS-BALANCE ; SEDIMENTS ; ZN ; GEOCHEMISTRY ; EVOLUTION ; INSIGHTS ; CALCITE ; SULFUR ; BARITE
资助项目	National Key R&D Program of China[2019YFA0708400] ; National Natural Science Foundation of China[41730214] ; National Natural Science Foundation of China[42003013] ; National Natural Science Foundation of China[41725007] ; Fundamental Research Funds for the Central Universities[2-9-2020-042]
WOS研究方向	Geochemistry & Geophysics
WOS类目	Geochemistry & Geophysics
WOS记录号	WOS:000778064300001
项目资助者	National Key R&D Program of China ; National Natural Science Foundation of China ; Fundamental Research Funds for the Central Universities
出版者	EUROPEAN ASSOC GEOCHEMISTRY
文献类型	期刊论文
条目标识符	http://ir.nigpas.ac.cn/handle/332004/40563
专题	中国科学院南京地质古生物研究所
通讯作者	Liu, S-A
作者单位	1.China Univ Geosci, State Key Lab Geol Proc & Mineral Resources, Beijing 100083, Peoples R China 2.China Univ Geosci, Sch Earth Sci & Resources, Beijing 100083, Peoples R China 3.China Univ Geosci, Sch Marine Sci, Beijing 100083, Peoples R China 4.Chengdu Univ Technol, Inst Sedimentary Geol, State Key Lab Oil & Gas Reservoir Geol & Exploita, Chengdu 610059, Peoples R China 5.Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, Nanjing 210008, Peoples R China 6.Chinese Acad Sci, Ctr Excellence Life & Paleoenvironm, Nanjing 210008, Peoples R China 7.Nanjing Univ, Sch Earth Sci & Engn, State Key Lab Mineral Deposits Res, Nanjing 210023, Peoples R China
推荐引用方式 GB/T 7714	Lv, Y.,Liu, S-A,Wu, H.,et al. Enhanced organic carbon burial intensified the end-Ordovician glaciation[J]. GEOCHEMICAL PERSPECTIVES LETTERS,2022,21:13-+.
APA	Lv, Y.,Liu, S-A,Wu, H.,Sun, Z.,Li, C.,&Fan, J. X..(2022).Enhanced organic carbon burial intensified the end-Ordovician glaciation.GEOCHEMICAL PERSPECTIVES LETTERS,21,13-+.
MLA	Lv, Y.,et al."Enhanced organic carbon burial intensified the end-Ordovician glaciation".GEOCHEMICAL PERSPECTIVES LETTERS 21(2022):13-+.