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. 2019 Mar 19;9:4877. doi: 10.1038/s41598-019-41257-3

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© The Author(s) 2019

Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/.

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Surface uplift estimates for each physiographic region based on lapse rates in Fig. 5. Estimates are calculated based on the most negative and mean pre-shift (>−90‰) and post-shift (<−90‰) water-glass fractionation corrected dD_pw values³³. Estimates take into account Oligocene – Pleistocene global cooling climate correction (see text and Supplementary Information for details). Shaded horizontal colored bars are ±1σ standard deviation of modern elevation.