The paleo-oceanic environment and organic matter enrichment mechanism of the early Cambrian in the southern Lower Yangtze platform, China

This study focuses on the Lower Yangtze Platform located in southern Anhui Province, focusing on the black shale of the early Cambrian Hetang Formation as the primary research subject. Three field sections representing distinct sedimentary structural units were selected for investigation. Analytical...

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Published inMarine and petroleum geology Vol. 170; p. 107119
Main Authors Zhou, Dongsheng, Dong, Hezheng, Huang, Xiaowei, Liang, Yufei, Deng, Ziyan, Huang, Lei, Jiang, Shu
Format Journal Article
LanguageEnglish
Published Elsevier Ltd 01.12.2024
Subjects
Black shale
Early cambrian
Hetang formation
Hydrothermal fluid
Lower yangtze
Organic matter accumulation
Hetang formation
Organic matter accumulation
Black shale
Lower yangtze
Early cambrian
Hydrothermal fluid
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Abstract This study focuses on the Lower Yangtze Platform located in southern Anhui Province, focusing on the black shale of the early Cambrian Hetang Formation as the primary research subject. Three field sections representing distinct sedimentary structural units were selected for investigation. Analytical methodologies encompassing organic geochemistry, elemental geochemistry, and scanning electron microscopy were employed to reconstruct paleo-oceanic environmental conditions. These analyses aimed to elucidate the characteristics of marine surface productivity and identify the factors controlling organic matter formation, thereby establishing a model for organic matter accumulation processes. These findings suggest that the Jiangnan paleo-uplift exerted differentiated control over organic matter formation and accumulation. Specifically, the barrier function of the paleo-uplift fostered a relatively enclosed and restricted water environment in certain regions, which proved conducive to the formation, accumulation, and preservation of organic matter. Furthermore, the paleo-upwelling system and hydrothermal groundwater circulation triggered by the activation of the Jiangnan deep fault played crucial roles in controlling the formation and accumulation of organic matter in the early Cambrian. Notably, the research also revealed that intermittent hydrothermal activity had a dual impact on organic matter accumulation within various paleo-oceanic settings. This process potentially facilitated organic matter enrichment and led to the dilution of organic matter concentrations. [Display omitted] •Reveals the significant impact of early Cambrian marine conditions on organic matter deposition.•Identifies hydrothermal sources and evaluates their differential impact on organic matter accumulation.•Analyzes key sedimentary and geochemical factors controlling organic matter enrichment.•Proposes a new model for early Cambrian organic matter accumulation, offering a framework for related studies.
AbstractList This study focuses on the Lower Yangtze Platform located in southern Anhui Province, focusing on the black shale of the early Cambrian Hetang Formation as the primary research subject. Three field sections representing distinct sedimentary structural units were selected for investigation. Analytical methodologies encompassing organic geochemistry, elemental geochemistry, and scanning electron microscopy were employed to reconstruct paleo-oceanic environmental conditions. These analyses aimed to elucidate the characteristics of marine surface productivity and identify the factors controlling organic matter formation, thereby establishing a model for organic matter accumulation processes. These findings suggest that the Jiangnan paleo-uplift exerted differentiated control over organic matter formation and accumulation. Specifically, the barrier function of the paleo-uplift fostered a relatively enclosed and restricted water environment in certain regions, which proved conducive to the formation, accumulation, and preservation of organic matter. Furthermore, the paleo-upwelling system and hydrothermal groundwater circulation triggered by the activation of the Jiangnan deep fault played crucial roles in controlling the formation and accumulation of organic matter in the early Cambrian. Notably, the research also revealed that intermittent hydrothermal activity had a dual impact on organic matter accumulation within various paleo-oceanic settings. This process potentially facilitated organic matter enrichment and led to the dilution of organic matter concentrations. [Display omitted] •Reveals the significant impact of early Cambrian marine conditions on organic matter deposition.•Identifies hydrothermal sources and evaluates their differential impact on organic matter accumulation.•Analyzes key sedimentary and geochemical factors controlling organic matter enrichment.•Proposes a new model for early Cambrian organic matter accumulation, offering a framework for related studies.
ArticleNumber 107119
Author Huang, Xiaowei
Huang, Lei
Liang, Yufei
Deng, Ziyan
Dong, Hezheng
Jiang, Shu
Zhou, Dongsheng
Author_xml – sequence: 1
  givenname: Dongsheng
  orcidid: 0000-0002-5686-4428
  surname: Zhou
  fullname: Zhou, Dongsheng
  organization: School of Ocean Sciences, China University of Geosciences (Beijing), Beijing, 100083, China
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  givenname: Hezheng
  surname: Dong
  fullname: Dong, Hezheng
  email: 3111240006@email.cugb.edu.cn
  organization: School of Ocean Sciences, China University of Geosciences (Beijing), Beijing, 100083, China
– sequence: 3
  givenname: Xiaowei
  surname: Huang
  fullname: Huang, Xiaowei
  organization: School of Ocean Sciences, China University of Geosciences (Beijing), Beijing, 100083, China
– sequence: 4
  givenname: Yufei
  surname: Liang
  fullname: Liang, Yufei
  organization: School of Ocean Sciences, China University of Geosciences (Beijing), Beijing, 100083, China
– sequence: 5
  givenname: Ziyan
  surname: Deng
  fullname: Deng, Ziyan
  organization: School of Ocean Sciences, China University of Geosciences (Beijing), Beijing, 100083, China
– sequence: 6
  givenname: Lei
  surname: Huang
  fullname: Huang, Lei
  organization: School of Ocean Sciences, China University of Geosciences (Beijing), Beijing, 100083, China
– sequence: 7
  givenname: Shu
  surname: Jiang
  fullname: Jiang, Shu
  email: jiangsu@cug.edu.cn
  organization: School of Sustainable Energy, China University of Geosciences, Wuhan, 430074, China
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Keywords Hetang formation
Organic matter accumulation
Black shale
Lower yangtze
Early cambrian
Hydrothermal fluid
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Snippet This study focuses on the Lower Yangtze Platform located in southern Anhui Province, focusing on the black shale of the early Cambrian Hetang Formation as the...
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StartPage 107119
SubjectTerms Black shale
Early cambrian
Hetang formation
Hydrothermal fluid
Lower yangtze
Organic matter accumulation
Title The paleo-oceanic environment and organic matter enrichment mechanism of the early Cambrian in the southern Lower Yangtze platform, China
URI https://dx.doi.org/10.1016/j.marpetgeo.2024.107119
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