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 |
|---|---|
| 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 |
UN SDGs
This output contributes to the following UN Sustainable Development Goals (SDGs)
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SDG 13 Climate Action
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