Sedimentary geochemical records of late Miocene-early Pliocene palaeovegetation and palaeoclimate evolution in the Ying-Qiong Basin, South China Sea

The sedimentary geochemical records of palaeovegetation and palaeoclimate variations in late Miocene-early Pliocene sediments in the Ying-Qiong Basin, South China Sea have been studied using higher plant-derived biomarkers, palynological records, trace elements, and macerals. Aliphatic biomarkers in...

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Published inMarine geology Vol. 445; p. 106750
Main Authors Ding, Wenjing, Hou, Dujie, Gan, Jun, Jiang, Lian, Zhang, Ziming, George, Simon C.
Format Journal Article
LanguageEnglish
Published Elsevier B.V 01.03.2022
Subjects
Aromatic hydrocarbon
East Asian monsoon
Gymnosperm
Higher plant-derived biomarker
Kerogen
Maceral
Gymnosperm
East Asian monsoon
Higher plant-derived biomarker
Aromatic hydrocarbon
Kerogen
Maceral
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Abstract The sedimentary geochemical records of palaeovegetation and palaeoclimate variations in late Miocene-early Pliocene sediments in the Ying-Qiong Basin, South China Sea have been studied using higher plant-derived biomarkers, palynological records, trace elements, and macerals. Aliphatic biomarkers including oleanane, des-A-oleanane, bicadinanes, and C19 tricyclic terpane, and the vitrinite content of the kerogen, show a remarkable decline in the input of the main angiosperms from about 8.2 to 2.7 Ma, corresponding to the deposition of the upper Huangliu Formation (late Miocene) to the lower Yinggehai Formation (early Pliocene). Aromatic parameters including retene/(retene + cadalene), 1,2,5-TMN/1,3,6-TMN, 1-MP/9-MP and 1,7-DMP/(1,3- + 3,9- + 2,10- + 3,10-DMP) suggest that the upper Huangliu Formation received a greater gymnosperm contribution than older Miocene formations. Trace element ratios (Rb/Sr and Zr/Rb) and the proportion of alginite-amorphous macerals in the shales indicate that a cooler, more arid climate with less seasonal precipitation occurred progressively from about 8.2–2.7 Ma, as also supported by higher abundances of Pinus and Alnus and decreasing proportions of ferns in the flora. Lesser input of terrigenous higher plants and the variation in vegetation types occurred during a cooling climate that was likely associated with a weaker East Asian summer monsoon and uplift of the northern Tibet-Plateau from about 8.5 Ma. •Palaeoclimate and palaeovegetation in Ying-Qiong Basin (S. China) reconstructed.•Higher gymnosperm/angiosperm and more Pinus in flora from 8.2–2.7 Ma.•From late Miocene to early Pliocene there was a cooling and drying climate.•Weakening East Asian summer monsoon occurred from 8.2–2.7 Ma.
AbstractList The sedimentary geochemical records of palaeovegetation and palaeoclimate variations in late Miocene-early Pliocene sediments in the Ying-Qiong Basin, South China Sea have been studied using higher plant-derived biomarkers, palynological records, trace elements, and macerals. Aliphatic biomarkers including oleanane, des-A-oleanane, bicadinanes, and C19 tricyclic terpane, and the vitrinite content of the kerogen, show a remarkable decline in the input of the main angiosperms from about 8.2 to 2.7 Ma, corresponding to the deposition of the upper Huangliu Formation (late Miocene) to the lower Yinggehai Formation (early Pliocene). Aromatic parameters including retene/(retene + cadalene), 1,2,5-TMN/1,3,6-TMN, 1-MP/9-MP and 1,7-DMP/(1,3- + 3,9- + 2,10- + 3,10-DMP) suggest that the upper Huangliu Formation received a greater gymnosperm contribution than older Miocene formations. Trace element ratios (Rb/Sr and Zr/Rb) and the proportion of alginite-amorphous macerals in the shales indicate that a cooler, more arid climate with less seasonal precipitation occurred progressively from about 8.2–2.7 Ma, as also supported by higher abundances of Pinus and Alnus and decreasing proportions of ferns in the flora. Lesser input of terrigenous higher plants and the variation in vegetation types occurred during a cooling climate that was likely associated with a weaker East Asian summer monsoon and uplift of the northern Tibet-Plateau from about 8.5 Ma. •Palaeoclimate and palaeovegetation in Ying-Qiong Basin (S. China) reconstructed.•Higher gymnosperm/angiosperm and more Pinus in flora from 8.2–2.7 Ma.•From late Miocene to early Pliocene there was a cooling and drying climate.•Weakening East Asian summer monsoon occurred from 8.2–2.7 Ma.
ArticleNumber 106750
Author Zhang, Ziming
George, Simon C.
Jiang, Lian
Ding, Wenjing
Gan, Jun
Hou, Dujie
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  fullname: Ding, Wenjing
  organization: School of Energy Resources, China University of Geosciences, Beijing, 100083, China
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  givenname: Dujie
  surname: Hou
  fullname: Hou, Dujie
  email: hdj@cugb.edu.cn
  organization: School of Energy Resources, China University of Geosciences, Beijing, 100083, China
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  givenname: Jun
  surname: Gan
  fullname: Gan, Jun
  organization: Exploration and Development Resource Institute, Zhanjiang Branch of China National Offshore Oil Corporation, Guangdong 524057, China
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  givenname: Lian
  surname: Jiang
  fullname: Jiang, Lian
  organization: School of Natural Sciences, Macquarie University, Sydney, NSW 2109, Australia
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  givenname: Ziming
  surname: Zhang
  fullname: Zhang, Ziming
  organization: School of Energy Resources, China University of Geosciences, Beijing, 100083, China
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  givenname: Simon C.
  surname: George
  fullname: George, Simon C.
  email: simon.george@mq.edu.au
  organization: School of Natural Sciences, Macquarie University, Sydney, NSW 2109, Australia
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Keywords Gymnosperm
East Asian monsoon
Higher plant-derived biomarker
Aromatic hydrocarbon
Kerogen
Maceral
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Snippet The sedimentary geochemical records of palaeovegetation and palaeoclimate variations in late Miocene-early Pliocene sediments in the Ying-Qiong Basin, South...
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SubjectTerms Aromatic hydrocarbon
East Asian monsoon
Gymnosperm
Higher plant-derived biomarker
Kerogen
Maceral
Title Sedimentary geochemical records of late Miocene-early Pliocene palaeovegetation and palaeoclimate evolution in the Ying-Qiong Basin, South China Sea
URI https://dx.doi.org/10.1016/j.margeo.2022.106750
Volume 445
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