| Literature DB >> 31604210 |
Paul J Valdes1, Ding Lin2,3, Alex Farnsworth4, Robert A Spicer5,6, Shi-Hu Li7, Su Tao3,6.
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.Entities:
Year: 2019 PMID: 31604210 DOI: 10.1126/science.aax8474
Source DB: PubMed Journal: Science ISSN: 0036-8075 Impact factor: 47.728