Articles | Volume 12, issue 2
https://doi.org/10.5194/cp-12-255-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/cp-12-255-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Terrestrial responses of low-latitude Asia to the Eocene–Oligocene climate transition revealed by integrated chronostratigraphy
State Key Laboratory for Mineral Deposits Research, Key Laboratory of Surficial
Geochemistry, Ministry of Education, School of Earth Sciences and Engineering, 210046 Nanjing, China
W. J. Jiao
State Key Laboratory for Mineral Deposits Research, Key Laboratory of Surficial
Geochemistry, Ministry of Education, School of Earth Sciences and Engineering, 210046 Nanjing, China
Z. H. Liu
Department of Earth Sciences, The University of Hong Kong, Hong Kong,
China
J. H. Jin
State Key Laboratory of Biocontrol and Guangdong Provincial Key
Laboratory of Plant Resources, School of Life Sciences, Sun Yat-sen
University, 510275 Guangzhou, China
D. H. Wang
College of Earth Sciences, Jilin University, 130061 Changchun, China
Department of Earth Sciences, Zhejiang University, Hangzhou, China
C. Quan
CORRESPONDING AUTHOR
Research Center of Paleontology and Stratigraphy, Jilin University, 130026 Changchun, China
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- Orbital climate variability on the northeastern Tibetan Plateau across the Eocene–Oligocene transition H. Ao et al. 10.1038/s41467-020-18824-8
- Astronomical influence of the development of Paleogene thin coal seam groups in offshore Lacustrine basins: A case study of the Zhu I Depression’s Enping Formation located in the northern South China Sea Y. Liu et al. 10.1007/s13131-024-2332-x
- Phylogenetic analysis of a new morphological dataset elucidates the evolutionary history of Crocodylia and resolves the long-standing gharial problem J. Rio & P. Mannion 10.7717/peerj.12094
- The Paleoclimate Significance of the δ13C Composition of Individual Hydrocarbon Compounds in the Maoming Oil Shales, China X. Cao et al. 10.3389/feart.2021.648176
- East Asian hydroclimate responses to the Eocene-Oligocene transition in the Weihe Basin, central China Y. Wang et al. 10.1016/j.palaeo.2023.111436
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13 citations as recorded by crossref.
- Geochemical and petrographic evidence for the co-occurrence of races B and L of Botryococcus braunii in the Maoming oil shales, China H. Lu et al. 10.1016/j.orggeochem.2018.08.006
- High-resolution Palaeogene sequence stratigraphic framework for the Cuu Long Basin, offshore Vietnam, driven by climate change and tectonics, established from sequence biostratigraphy R. Morley et al. 10.1016/j.palaeo.2019.05.010
- Anthracotheriid artiodactylAnthracokeryxand an upper Eocene age for the Youganwo Formation of southern China A. Averianov et al. 10.1080/08912963.2017.1421639
- Sequence biostratigraphy of the late Oligocene to Miocene succession in the northern Song Hong Basin, offshore Vietnam N. Chung et al. 10.1016/j.palaeo.2021.110322
- Long-term floristic and climatic stability of northern Indochina: Evidence from the Oligocene Ha Long flora, Vietnam J. Huang et al. 10.1016/j.palaeo.2022.110930
- Global Cooling‐Driven Summer Monsoon Weakening in South China Across the Eocene‐Oligocene Transition W. Jiao et al. 10.1029/2023JB027265
- Astronomically forced climate cooling across the Eocene–Oligocene transition in the Pearl River Mouth Basin, northern South China Sea X. Wei et al. 10.1016/j.palaeo.2020.109945
- Orbital climate variability on the northeastern Tibetan Plateau across the Eocene–Oligocene transition H. Ao et al. 10.1038/s41467-020-18824-8
- Astronomical influence of the development of Paleogene thin coal seam groups in offshore Lacustrine basins: A case study of the Zhu I Depression’s Enping Formation located in the northern South China Sea Y. Liu et al. 10.1007/s13131-024-2332-x
- Phylogenetic analysis of a new morphological dataset elucidates the evolutionary history of Crocodylia and resolves the long-standing gharial problem J. Rio & P. Mannion 10.7717/peerj.12094
- The Paleoclimate Significance of the δ13C Composition of Individual Hydrocarbon Compounds in the Maoming Oil Shales, China X. Cao et al. 10.3389/feart.2021.648176
- East Asian hydroclimate responses to the Eocene-Oligocene transition in the Weihe Basin, central China Y. Wang et al. 10.1016/j.palaeo.2023.111436
- Plastome phylogenomics, systematics, and divergence time estimation of the Beilschmiedia group (Lauraceae) H. Li et al. 10.1016/j.ympev.2020.106901
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Discussed (final revised paper)
Latest update: 02 Nov 2024
Short summary
An integrated litho-, bio-, cyclo-, and magnetostratigraphy constrains the onset of a depositional environmental change from a lacustrine to a deltaic environment in the Maoming Basin, China, at 33.88 Ma. This coincides with the global cooling during the Eocene-Oligocene transition (EOT) at ~ 33.7–33.9 Ma. This change represents terrestrial responses of low-latitude Asia to the EOT. The greatly refined chronology permits detailed examination of the late Paleogene climate change in southeast Asia.
An integrated litho-, bio-, cyclo-, and magnetostratigraphy constrains the onset of a...