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.
Original language | English |
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Article number | eaax8474 |
Number of pages | 4 |
Journal | Science |
Volume | 365 |
Issue number | 6459 |
DOIs |
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Publication status | Published - 20 Sept 2019 |