Articles | Volume 16, issue 6
https://doi.org/10.5194/cp-16-2255-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/cp-16-2255-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
20 Nov 2020
Research article |
| 20 Nov 2020
| 20 Nov 2020
Aridification signatures from fossil pollen indicate a drying climate in east-central Tibet during the late Eocene
Qin Yuan
Key Laboratory of Comprehensive and Highly Efficient Utilization of Salt Lake Resources, Qinghai Institute of Salt Lakes, Chinese Academy of Sciences, Xining, China
Qinghai Provincial Key Laboratory of Geology and Environment of Salt Lakes, Qinghai Institute of Salt Lakes, Chinese Academy of Sciences, Xining, China
University of Chinese Academy of Sciences, Beijing, China
Department of Palaeobiology, Swedish Museum of Natural History, Stockholm, Sweden
Natasha Barbolini
CORRESPONDING AUTHOR
Department of Ecology, Environment and Plant Sciences and Bolin Centre for Climate Research, Stockholm University, Stockholm, Sweden
Department of Ecosystem and Landscape Dynamics, Institute for Biodiversity and Ecosystem Dynamics, University of Amsterdam, Amsterdam, the Netherlands
Catarina Rydin
Department of Ecology, Environment and Plant Sciences and Bolin Centre for Climate Research, Stockholm University, Stockholm, Sweden
The Bergius Foundation, The Royal Swedish Academy of Sciences, Stockholm, Sweden
Dong-Lin Gao
Key Laboratory of Comprehensive and Highly Efficient Utilization of Salt Lake Resources, Qinghai Institute of Salt Lakes, Chinese Academy of Sciences, Xining, China
Qinghai Provincial Key Laboratory of Geology and Environment of Salt Lakes, Qinghai Institute of Salt Lakes, Chinese Academy of Sciences, Xining, China
Hai-Cheng Wei
Key Laboratory of Comprehensive and Highly Efficient Utilization of Salt Lake Resources, Qinghai Institute of Salt Lakes, Chinese Academy of Sciences, Xining, China
Qinghai Provincial Key Laboratory of Geology and Environment of Salt Lakes, Qinghai Institute of Salt Lakes, Chinese Academy of Sciences, Xining, China
Qi-Shun Fan
Key Laboratory of Comprehensive and Highly Efficient Utilization of Salt Lake Resources, Qinghai Institute of Salt Lakes, Chinese Academy of Sciences, Xining, China
Qinghai Provincial Key Laboratory of Geology and Environment of Salt Lakes, Qinghai Institute of Salt Lakes, Chinese Academy of Sciences, Xining, China
Zhan-Jie Qin
Key Laboratory of Comprehensive and Highly Efficient Utilization of Salt Lake Resources, Qinghai Institute of Salt Lakes, Chinese Academy of Sciences, Xining, China
Qinghai Provincial Key Laboratory of Geology and Environment of Salt Lakes, Qinghai Institute of Salt Lakes, Chinese Academy of Sciences, Xining, China
Yong-Sheng Du
Key Laboratory of Comprehensive and Highly Efficient Utilization of Salt Lake Resources, Qinghai Institute of Salt Lakes, Chinese Academy of Sciences, Xining, China
Qinghai Provincial Key Laboratory of Geology and Environment of Salt Lakes, Qinghai Institute of Salt Lakes, Chinese Academy of Sciences, Xining, China
Jun-Jie Shan
Key Laboratory of Comprehensive and Highly Efficient Utilization of Salt Lake Resources, Qinghai Institute of Salt Lakes, Chinese Academy of Sciences, Xining, China
Qinghai Provincial Key Laboratory of Geology and Environment of Salt Lakes, Qinghai Institute of Salt Lakes, Chinese Academy of Sciences, Xining, China
University of Chinese Academy of Sciences, Beijing, China
Fa-Shou Shan
Key Laboratory of Comprehensive and Highly Efficient Utilization of Salt Lake Resources, Qinghai Institute of Salt Lakes, Chinese Academy of Sciences, Xining, China
Qinghai Provincial Key Laboratory of Geology and Environment of Salt Lakes, Qinghai Institute of Salt Lakes, Chinese Academy of Sciences, Xining, China
Vivi Vajda
Department of Palaeobiology, Swedish Museum of Natural History, Stockholm, Sweden
Viewed
Total article views: 3,865 (including HTML, PDF, and XML)
Cumulative views and downloads
(calculated since 20 Jan 2020)
| HTML | XML | Total | Supplement | BibTeX | EndNote | |
|---|---|---|---|---|---|---|
| 2,861 | 896 | 108 | 3,865 | 307 | 89 | 101 |
- HTML: 2,861
- PDF: 896
- XML: 108
- Total: 3,865
- Supplement: 307
- BibTeX: 89
- EndNote: 101
Total article views: 3,041 (including HTML, PDF, and XML)
Cumulative views and downloads
(calculated since 20 Nov 2020)
| HTML | XML | Total | Supplement | BibTeX | EndNote | |
|---|---|---|---|---|---|---|
| 2,398 | 587 | 56 | 3,041 | 126 | 51 | 65 |
- HTML: 2,398
- PDF: 587
- XML: 56
- Total: 3,041
- Supplement: 126
- BibTeX: 51
- EndNote: 65
Total article views: 824 (including HTML, PDF, and XML)
Cumulative views and downloads
(calculated since 20 Jan 2020)
| HTML | XML | Total | Supplement | BibTeX | EndNote | |
|---|---|---|---|---|---|---|
| 463 | 309 | 52 | 824 | 181 | 38 | 36 |
- HTML: 463
- PDF: 309
- XML: 52
- Total: 824
- Supplement: 181
- BibTeX: 38
- EndNote: 36
Viewed (geographical distribution)
Total article views: 3,865 (including HTML, PDF, and XML)
Thereof 3,408 with geography defined
and 457 with unknown origin.
Total article views: 3,041 (including HTML, PDF, and XML)
Thereof 2,731 with geography defined
and 310 with unknown origin.
Total article views: 824 (including HTML, PDF, and XML)
Thereof 677 with geography defined
and 147 with unknown origin.
| Country | # | Views | % |
|---|
| Country | # | Views | % |
|---|
| Country | # | Views | % |
|---|
| Total: | 0 |
| HTML: | 0 |
| PDF: | 0 |
| XML: | 0 |
- 1
1
| Total: | 0 |
| HTML: | 0 |
| PDF: | 0 |
| XML: | 0 |
- 1
1
| Total: | 0 |
| HTML: | 0 |
| PDF: | 0 |
| XML: | 0 |
- 1
1
Cited
14 citations as recorded by crossref.
- At a crossroads: The late Eocene flora of central Myanmar owes its composition to plate collision and tropical climate H. Huang et al. 10.1016/j.revpalbo.2021.104441
- Long-term drying trend during 51.8–37.5 Ma in the Nangqian Basin, central-eastern Qinghai–Tibet Plateau S. Li et al. 10.3389/feart.2022.866304
- A Classopollis “spike” in the Rugubivesiculites Zone of the Kayan Sandstone, western Sarawak, Borneo, suggests a Danian age for these deposits K. Berry 10.1016/j.revpalbo.2022.104728
- Cold climatic snaps during the Eocene-Oligocene transition in the central Tibetan Plateau: Implications for ice-induced sedimentary structures and isotope geochemistry G. Xia et al. 10.1016/j.palaeo.2023.112010
- Middle Eocene Paleoenvironmental Reconstruction in the Gonjo Basin, Eastern Tibetan Plateau: Evidence From Palynological and Evaporite Records L. Wang et al. 10.3389/feart.2022.818418
- Was the K/Pg boundary Classopollis ‘spike’ a singular event? A review of global palynological records suggests otherwise, with potentially broad implications K. Berry 10.24872/rmgjournal.57.1.35
- Variability of Ephedra dahurica Turcz. Pollen as an Indicator of Humidity for the Modern Climate of Southeastern Transbaikalia S. Reshetova et al. 10.1134/S1028334X24603158
- Biomarker Records From Eocene Lacustrine Sequence in the Eastern Tibet Plateau and Its Implication for Organic Matter Sources J. Wei et al. 10.3389/feart.2022.849041
- Cutting the long branches: Consilience as a path to unearth the evolutionary history of Gnetales M. Coiro et al. 10.3389/fevo.2022.1082639
- Paleogene integrative stratigraphy, biotas, and paleogeographical evolution of the Qinghai-Tibetan Plateau and its surrounding areas J. Liu et al. 10.1007/s11430-023-1182-0
- Northward expansion of Cenozoic Asian humid climate recorded by sporopollen F. Wu et al. 10.1016/j.palaeo.2023.112009
- Palaeoenvironmental changes in Eocene Tibetan lake systems traced by geochemistry, sedimentology and palynofacies Q. Yuan et al. 10.1016/j.jseaes.2021.104778
- The role of paleogeography in Asian monsoon evolution: a review and new insights from climate modelling D. Tardif et al. 10.1016/j.earscirev.2023.104464
- 青藏高原及其周边古近纪综合地层<bold>、</bold>生物群与古地理演化 佳. 刘 et al. 10.1360/SSTe-2023-0023
14 citations as recorded by crossref.
- At a crossroads: The late Eocene flora of central Myanmar owes its composition to plate collision and tropical climate H. Huang et al. 10.1016/j.revpalbo.2021.104441
- Long-term drying trend during 51.8–37.5 Ma in the Nangqian Basin, central-eastern Qinghai–Tibet Plateau S. Li et al. 10.3389/feart.2022.866304
- A Classopollis “spike” in the Rugubivesiculites Zone of the Kayan Sandstone, western Sarawak, Borneo, suggests a Danian age for these deposits K. Berry 10.1016/j.revpalbo.2022.104728
- Cold climatic snaps during the Eocene-Oligocene transition in the central Tibetan Plateau: Implications for ice-induced sedimentary structures and isotope geochemistry G. Xia et al. 10.1016/j.palaeo.2023.112010
- Middle Eocene Paleoenvironmental Reconstruction in the Gonjo Basin, Eastern Tibetan Plateau: Evidence From Palynological and Evaporite Records L. Wang et al. 10.3389/feart.2022.818418
- Was the K/Pg boundary Classopollis ‘spike’ a singular event? A review of global palynological records suggests otherwise, with potentially broad implications K. Berry 10.24872/rmgjournal.57.1.35
- Variability of Ephedra dahurica Turcz. Pollen as an Indicator of Humidity for the Modern Climate of Southeastern Transbaikalia S. Reshetova et al. 10.1134/S1028334X24603158
- Biomarker Records From Eocene Lacustrine Sequence in the Eastern Tibet Plateau and Its Implication for Organic Matter Sources J. Wei et al. 10.3389/feart.2022.849041
- Cutting the long branches: Consilience as a path to unearth the evolutionary history of Gnetales M. Coiro et al. 10.3389/fevo.2022.1082639
- Paleogene integrative stratigraphy, biotas, and paleogeographical evolution of the Qinghai-Tibetan Plateau and its surrounding areas J. Liu et al. 10.1007/s11430-023-1182-0
- Northward expansion of Cenozoic Asian humid climate recorded by sporopollen F. Wu et al. 10.1016/j.palaeo.2023.112009
- Palaeoenvironmental changes in Eocene Tibetan lake systems traced by geochemistry, sedimentology and palynofacies Q. Yuan et al. 10.1016/j.jseaes.2021.104778
- The role of paleogeography in Asian monsoon evolution: a review and new insights from climate modelling D. Tardif et al. 10.1016/j.earscirev.2023.104464
- 青藏高原及其周边古近纪综合地层<bold>、</bold>生物群与古地理演化 佳. 刘 et al. 10.1360/SSTe-2023-0023
Latest update: 23 Nov 2024
Short summary
Fossil pollen and spores reveal that a strongly seasonal steppe–desert ecosystem existed in the Nangqian Basin, east-central Tibet during the late Eocene (41.2–37.8 Ma). Vegetation was characterized by drought-tolerant shrubs, diverse ferns, and broad-leaved forests. The climate warmed temporarily, then rapidly aridified thereafter due to westward regression of the proto-Paratethys Sea from Eurasia. Sea retreat was a main driver of widespread long-term Asian aridification during the late Eocene.
Fossil pollen and spores reveal that a strongly seasonal steppe–desert ecosystem existed in the...
