The DOI matches its Crossref record; 24 of the 24 references it cites were found in a registry or an index.
Tibetan uplift prior to the Eocene-Oligocene climate transition: Evidence from pollen analysis of the Xining Basin
Abstract
Uplift of the Tibetan Plateau and the Himalayas since the onset of the Indo-Asia collision is held responsible for Asian aridification and monsoon intensification, but may also have gradually cooled global climate, leading to the 34 Ma Eocene-Oligocene transition. To unravel the interplay between Tibetan uplift and global climate, proxy records of Asian paleoenvironments constrained by accurate age models are needed for the Paleogene Period. Here we report the 38 Ma appearance of high-altitude vegetation recovered from palynological assemblages in precisely dated lacustrine sediments from the Xining Basin of the northeastern Tibetan Plateau region. This result confirms previous evidence for important regional uplift in the central and northern Tibetan Plateau regions during the early stage of the Indo-Asia collision. This is consistent with the idea that the associated increase in rock weathering and erosion contributed to lowering of atmospheric CO2, leading to the Eocene-Oligocene transition.
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Cites
A long-term numerical solution for the insolation quantities of the Earth
Laskar, J., Robutel, P., Joutel, F., Gastineau, M., Correia, A. C. M., & Levrard, B. (2004) · Astronomy & Astrophysics · doi:10.1051/0004-6361:20041335 · Cited by 3,837
Journal of Geophysical Research
(1949) · Nature · doi:10.1038/163436b0 · Cited by 3,480
(2013) · Chinese Science Bulletin · doi:10.1007/11434.1861-9541 · Cited by 1,955
Rapid Cenozoic glaciation of Antarctica induced by declining atmospheric CO2
DeConto, R. M., & Pollard, D. (2003) · Nature · doi:10.1038/nature01290 · Cited by 1,232
Influence of late Cenozoic mountain building on ocean geochemical cycles
Raymo, M. E., Ruddiman, W. F., & Froelich, P. N. (1988) · Geology · doi:10.1130/0091-7613(1988)016<0649:iolcmb>2.3.co;2 · Cited by 895
How old is the Asian monsoon system?—Palaeobotanical records from China
Sun, X., & Wang, P. (2005) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/j.palaeo.2005.03.005 · Cited by 892
Constraints on the early uplift history of the Tibetan Plateau
Wang, C., Zhao, X., Liu, Z., Lippert, P. C., Graham, S. A., Coe, R. S., Yi, H., Zhu, L., Liu, S., & Li, Y. (2008) · Proceedings of the National Academy of Sciences · doi:10.1073/pnas.0703595105 · Cited by 877
Palaeo-altimetry of the late Eocene to Miocene Lunpola basin, central Tibet
Rowley, D. B., & Currie, B. S. (2006) · Nature · doi:10.1038/nature04506 · Cited by 802
Tibetan plateau aridification linked to global cooling at the Eocene–Oligocene transition
Dupont‐Nivet, G., Krijgsman, W., Langereis, C. G., Abels, H. A., Dai, S., & Fang, X. (2007) · Nature · doi:10.1038/nature05516 · Cited by 644
Self-citationHigh and dry in central Tibet during the Late Oligocene
DeCelles, P. G., Quade, J., Kapp, P., Fan, M., Dettman, D. L., & Ding, L. (2007) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2006.11.001 · Cited by 356
Cited by
Asian monsoons in a late Eocene greenhouse world
Licht, A., van Cappelle, M., Abels, H. A., Ladant, J.-B., Trabucho-Alexandre, J., France-Lanord, C., Donnadieu, Y., Vandenberghe, J., Rigaudier, T., Lécuyer, C., et al. (2014) · Nature · doi:10.1038/nature13704 · Cited by 527
Self-citationTAYLOR, L. L., LEAKE, J. R., QUIRK, J., HARDY, K., BANWART, S. A., & BEERLING, D. J. (2009) · Geobiology · doi:10.1111/j.1472-4669.2009.00194.x · Cited by 331
Metadata
- Authors
- Dupont-Nivet, G., Hoorn, C., & Konert, M.
- Venue
- Geology
- Publisher
- Geological Society of America
- Published
- 2008
- Volume
- 36
- Issue
- 12
- Pages
- 987
- ISSN
- 0091-7613 (ISSN-L)
- OpenAlex
- W2098727981
- Cited by
- 256
- References
- 24
- FWCI
- 8.24
- Type
- journal article
- Language
- en
- Open access
- closed
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- Dupont-Nivet, G., Hoorn, C., & Konert, M. (2008). Tibetan uplift prior to the Eocene-Oligocene climate transition: Evidence from pollen analysis of the Xining Basin. Geology. https://doi.org/10.1130/g25063a.1
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