Middle Miocene paleoenvironmental change and paleoelevation of the Lunpola Basin, Central Tibet
The Tibetan region underwent diachronous differential rises during the Cenozoic era. Its elevation history is critical for understanding the processes of mountain building, and for evaluating its climatic effects on atmospheric circulations. However, knowledge of paleoenvironment and paleoelevation...
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| Published in | Global and planetary change Vol. 220; p. 104009 |
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| Main Authors | , , , , , , , |
| Format | Journal Article |
| Language | English |
| Published |
Elsevier B.V
01.01.2023
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| Subjects | |
| Online Access | Get full text |
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| Abstract | The Tibetan region underwent diachronous differential rises during the Cenozoic era. Its elevation history is critical for understanding the processes of mountain building, and for evaluating its climatic effects on atmospheric circulations. However, knowledge of paleoenvironment and paleoelevation in different geological domains of the Tibetan Plateau is still limited. Here we provide chronology of lacustrine deposits of the Upper Dingqing Formation in the Lunpola Basin in Central Tibet, which yields a middle Miocene age (15–12 Ma). Both stable isotope and palynological records indicate a climatic transition at ∼13.8 Ma marked by a change towards a cooler and drier climate after the Middle Miocene Climate Transition driven by global climatic cooling. Pollen and spore assemblages suggest that the vegetation was dominated by mixed coniferous–broadleaved forest with some grasslands. New palynological elevation reconstructions constrained by the co-existence approach yield a maximum paleo-elevation of 3100–3600 m (average 3350 m) of the Lunpola Basin, which was consistent with a maximum elevation of 3400 m based on floating-leaf plants. Our new data do not support previous views that the Lunpola Basin achieved its current elevation as early as the late Eocene or early Oligocene, but instead we suggest there has been a rise of up to 1200 m since 12 million years ago. Our results bring new light on both the paleoenvironmental reconstructions and the paleo-elevation estimates of the Lunpola Basin, Central Tibet.
•Mid-Miocene age (15–12 Ma) of the upper Dingqing Formation in Central Tibet.•Climatic shifted to a cooler/drier climate after ca.13.8 Ma in Central Tibet.•The vegetation was dominated by mixed coniferous–broadleaved forest at 15–12 Ma.•The Lunpola Basin only attained a maximum elevation of 3400 m in the middle Miocene. |
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| AbstractList | The Tibetan region underwent diachronous differential rises during the Cenozoic era. Its elevation history is critical for understanding the processes of mountain building, and for evaluating its climatic effects on atmospheric circulations. However, knowledge of paleoenvironment and paleoelevation in different geological domains of the Tibetan Plateau is still limited. Here we provide chronology of lacustrine deposits of the Upper Dingqing Formation in the Lunpola Basin in Central Tibet, which yields a middle Miocene age (15–12 Ma). Both stable isotope and palynological records indicate a climatic transition at ∼13.8 Ma marked by a change towards a cooler and drier climate after the Middle Miocene Climate Transition driven by global climatic cooling. Pollen and spore assemblages suggest that the vegetation was dominated by mixed coniferous–broadleaved forest with some grasslands. New palynological elevation reconstructions constrained by the co-existence approach yield a maximum paleo-elevation of 3100–3600 m (average 3350 m) of the Lunpola Basin, which was consistent with a maximum elevation of 3400 m based on floating-leaf plants. Our new data do not support previous views that the Lunpola Basin achieved its current elevation as early as the late Eocene or early Oligocene, but instead we suggest there has been a rise of up to 1200 m since 12 million years ago. Our results bring new light on both the paleoenvironmental reconstructions and the paleo-elevation estimates of the Lunpola Basin, Central Tibet.
•Mid-Miocene age (15–12 Ma) of the upper Dingqing Formation in Central Tibet.•Climatic shifted to a cooler/drier climate after ca.13.8 Ma in Central Tibet.•The vegetation was dominated by mixed coniferous–broadleaved forest at 15–12 Ma.•The Lunpola Basin only attained a maximum elevation of 3400 m in the middle Miocene. |
| ArticleNumber | 104009 |
| Author | Li, Jianguo Farnsworth, Alex Zhang, Zhiliang Sun, Jimin Jin, Chunsheng Windley, Brian F. Xiao, Wenjiao Liu, Weiguo |
| Author_xml | – sequence: 1 givenname: Jimin surname: Sun fullname: Sun, Jimin email: jmsun@mail.iggcas.ac.cn organization: Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China – sequence: 2 givenname: Jianguo surname: Li fullname: Li, Jianguo organization: University of Chinese Academy of Sciences, Beijing 100049, China – sequence: 3 givenname: Weiguo surname: Liu fullname: Liu, Weiguo organization: Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710061, China – sequence: 4 givenname: Brian F. surname: Windley fullname: Windley, Brian F. organization: School of Geography, Geology and the Environment, University of Leicester, Leicester LEI 7RH, UK – sequence: 5 givenname: Alex surname: Farnsworth fullname: Farnsworth, Alex organization: State Key Laboratory of Tibetan Plateau Earth System, Resources and Environment (TPESRE), Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China – sequence: 6 givenname: Chunsheng surname: Jin fullname: Jin, Chunsheng organization: Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China – sequence: 7 givenname: Zhiliang surname: Zhang fullname: Zhang, Zhiliang organization: Institute of Geology, China Earthquake Administration, Beijing 100029, China – sequence: 8 givenname: Wenjiao surname: Xiao fullname: Xiao, Wenjiao organization: Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China |
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| CitedBy_id | crossref_primary_10_1029_2023PA004698 crossref_primary_10_1360_SSTe_2022_0412 crossref_primary_10_1360_TB_2023_0653 crossref_primary_10_1016_j_gloplacha_2023_104338 crossref_primary_10_1016_j_palaeo_2023_111858 crossref_primary_10_1016_j_quascirev_2024_108799 crossref_primary_10_1007_s11430_022_1115_5 |
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| Keywords | Paleoclimate Paleoaltitude Tibetan Plateau Pollen and stable isotope Mid-Miocene |
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