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Valdes, Paul J.; Lin, Ding; Farnsworth, Alex; Spicer, Robert A.; Li, Shi-Hu and Tao, Su
(2019).
DOI: https://doi.org/10.1126/science.aax8474
Abstract
Botsyun et al. (Research Articles, 1 March 2019, eaaq1436) have suggested that the Tibetan Plateau was low (substantially less than 3000 meters) during the Eocene, based on a comparison of oxygen isotope proxy data with isotope-enabled climate model simulations. However, we contend that their conclusions are flawed as the result of a number of failings of both the modeling and the data comparison.
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- Item ORO ID
- 67047
- Item Type
- Journal Item
- ISSN
- 1095-9203
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Faculty of Science, Technology, Engineering and Mathematics (STEM) > Environment, Earth and Ecosystem Sciences
Faculty of Science, Technology, Engineering and Mathematics (STEM) - Copyright Holders
- © 2019 American Association for the Advancement of Science
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