Biomarkers reveal the terrigenous organic matter enrichment in the late Oligocene—early Miocene marine shales in the Ying-Qiong Basin, South China Sea

The increase of total organic carbon content of the late Oligocene—early Miocene terrigenously-dominated marine shales in the shallower depth intervals was reported in the Ying-Qiong Basin, South China Sea. The organic enriched lower Sanya Formation shales (early Miocene) have biomarker characterist...

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Published inActa oceanologica Sinica Vol. 42; no. 3; pp. 31 - 53
Main Authors Ding, Wenjing, Li, Youchuan, Lei, Lan, Li, Li, Yang, Shuchun, Yang, Yongcai, Hou, Dujie
Format Journal Article
LanguageEnglish
Published Berlin/Heidelberg Springer Berlin Heidelberg 01.03.2023
Springer Nature B.V
School of Natural Sciences,Macquarie University,Sydney 2109,Australia
China National Offshors Oil Corporation(CNOOC)Research Institute Co.,Ltd.,Beijing 100028,China
School of Energy Resources,China University of Geosciences,Beijing 100083,China%China National Offshors Oil Corporation(CNOOC)Research Institute Co.,Ltd.,Beijing 100028,China%CNOOC International Limited,Beijing 100028,China%School of Energy Resources,China University of Geosciences,Beijing 100083,China
Subjects
Alkanes
Angiosperms
Biomarkers
Carbon content
Climatology
Earth and Environmental Science
Earth Sciences
East Asian monsoon
Ecology
Engineering Fluid Dynamics
Enrichment
Environmental Chemistry
Flora
Humid climates
Marine & Freshwater Sciences
Miocene
Molecular weight
Monsoon intensity
Ocean floor
Oceanography
Oligocene
Organic carbon
Organic matter
Sea floor spreading
Sea level changes
Seafloor spreading
Shales
Summer monsoon
Total organic carbon
South China Sea
tropical/subtropical plants
higher plant-derived biomarkers
East Asian monsoonal climate
total organic carbon
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Abstract The increase of total organic carbon content of the late Oligocene—early Miocene terrigenously-dominated marine shales in the shallower depth intervals was reported in the Ying-Qiong Basin, South China Sea. The organic enriched lower Sanya Formation shales (early Miocene) have biomarker characteristics of tropical/subtropical plants, with abundant high molecular weight n-alkanes, angiosperm-derived oleanane, rearranged oleananes I, II, II, tricyclic/tetracyclic terpanes including des-A-oleanane, X, *, Y, Z, Z1 and bicadinanes W, T, T1, R. The biomarker characteristics are suggestive of larger influx of the dominant tropical/subtropical angiosperms in flora under a warming and more humid climate during depositions of the lower Sanya Formation (early Miocene) than the older Lingshui Formation (late Oligocene). The tropical/subtropical angiosperm input was thought as the prime control of terrigenous organic matter enrichment relative to the redox condition, and the coeval sea level changes and seafloor spreading in the South China Sea. Enrichment of the terrigenous organic matter in the early Miocene shales is likely in association with the coeval peak East Asian summer monsoon intensity in the South China Sea.
AbstractList The increase of total organic carbon content of the late Oligocene—early Miocene terrigenously-dominated marine shales in the shallower depth intervals was reported in the Ying-Qiong Basin, South China Sea. The organic enriched lower Sanya Formation shales (early Miocene) have biomarker characteristics of tropical/subtropical plants, with abundant high molecular weight n-alkanes, angiosperm-derived oleanane, rearranged oleananes I, II, II, tricyclic/tetracyclic terpanes including des-A-oleanane, X, *, Y, Z, Z1 and bicadinanes W, T, T1, R. The biomarker characteristics are suggestive of larger influx of the dominant tropical/subtropical angiosperms in flora under a warming and more humid climate during depositions of the lower Sanya Formation (early Miocene) than the older Lingshui Formation (late Oligocene). The tropical/subtropical angiosperm input was thought as the prime control of terrigenous organic matter enrichment relative to the redox condition, and the coeval sea level changes and seafloor spreading in the South China Sea. Enrichment of the terrigenous organic matter in the early Miocene shales is likely in association with the coeval peak East Asian summer monsoon intensity in the South China Sea.
The increase of total organic carbon content of the late Oligocene?early Miocene terrigenously-dominated marine shales in the shallower depth intervals was reported in the Ying-Qiong Basin, South China Sea. The organic enriched lower Sanya Formation shales (early Miocene) have biomarker characteristics of tropical/subtropical plants, with abundant high molecular weight n-alkanes, angiosperm-derived oleanane, rearranged oleananes I,Ⅱ,Ⅱ, tricyclic/tetracyclic terpanes including des-A-oleanane, X, *, Y, Z, Z1 and bicadinanes W, T, T1, R. The biomarker characteristics are suggestive of larger influx of the dominant tropical/subtropical angiosperms in flora under a warming and more humid climate during depositions of the lower Sanya Formation (early Miocene) than the older Lingshui Formation (late Oligocene). The tropical/ subtropical angiosperm input was thought as the prime control of terrigenous organic matter enrichment relative to the redox condition, and the coeval sea level changes and seafloor spreading in the South China Sea. Enrichment of the terrigenous organic matter in the early Miocene shales is likely in association with the coeval peak East Asian summer monsoon intensity in the South China Sea.
Author Li, Youchuan
Lei, Lan
Li, Li
Ding, Wenjing
Yang, Shuchun
Hou, Dujie
Yang, Yongcai
AuthorAffiliation China National Offshors Oil Corporation(CNOOC)Research Institute Co.,Ltd.,Beijing 100028,China;School of Natural Sciences,Macquarie University,Sydney 2109,Australia;School of Energy Resources,China University of Geosciences,Beijing 100083,China%China National Offshors Oil Corporation(CNOOC)Research Institute Co.,Ltd.,Beijing 100028,China%CNOOC International Limited,Beijing 100028,China%School of Energy Resources,China University of Geosciences,Beijing 100083,China
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PublicationTitle Acta oceanologica Sinica
PublicationTitleAbbrev Acta Oceanol. Sin
PublicationTitle_FL Acta Oceanologica Sinica
PublicationYear 2023
Publisher Springer Berlin Heidelberg
Springer Nature B.V
School of Natural Sciences,Macquarie University,Sydney 2109,Australia
China National Offshors Oil Corporation(CNOOC)Research Institute Co.,Ltd.,Beijing 100028,China
School of Energy Resources,China University of Geosciences,Beijing 100083,China%China National Offshors Oil Corporation(CNOOC)Research Institute Co.,Ltd.,Beijing 100028,China%CNOOC International Limited,Beijing 100028,China%School of Energy Resources,China University of Geosciences,Beijing 100083,China
Publisher_xml – name: Springer Berlin Heidelberg
– name: Springer Nature B.V
– name: School of Energy Resources,China University of Geosciences,Beijing 100083,China%China National Offshors Oil Corporation(CNOOC)Research Institute Co.,Ltd.,Beijing 100028,China%CNOOC International Limited,Beijing 100028,China%School of Energy Resources,China University of Geosciences,Beijing 100083,China
– name: School of Natural Sciences,Macquarie University,Sydney 2109,Australia
– name: China National Offshors Oil Corporation(CNOOC)Research Institute Co.,Ltd.,Beijing 100028,China
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Snippet The increase of total organic carbon content of the late Oligocene—early Miocene terrigenously-dominated marine shales in the shallower depth intervals was...
The increase of total organic carbon content of the late Oligocene?early Miocene terrigenously-dominated marine shales in the shallower depth intervals was...
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SubjectTerms Alkanes
Angiosperms
Biomarkers
Carbon content
Climatology
Earth and Environmental Science
Earth Sciences
East Asian monsoon
Ecology
Engineering Fluid Dynamics
Enrichment
Environmental Chemistry
Flora
Humid climates
Marine & Freshwater Sciences
Miocene
Molecular weight
Monsoon intensity
Ocean floor
Oceanography
Oligocene
Organic carbon
Organic matter
Sea floor spreading
Sea level changes
Seafloor spreading
Shales
Summer monsoon
Total organic carbon
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Title Biomarkers reveal the terrigenous organic matter enrichment in the late Oligocene—early Miocene marine shales in the Ying-Qiong Basin, South China Sea
URI https://link.springer.com/article/10.1007/s13131-022-2081-6
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https://d.wanfangdata.com.cn/periodical/hyxb-e202303003
Volume 42
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