Plio-Pleistocene climate record on the Tibetan plateau

• Main Authors: Cheng, Feng, Garzione, Carmala, Li, Xiangzhong, Salzmann, Ulrich, Schwarz, Florian, Haywood, Alan, Tindall, Julia, Nie, Junsheng, Li, Lin, Wang, Lin, Abbott, Benjamin, Elliott, Ben, Liu, Weiguo, Upadhyay, Deepshikha, Arnold, Alexandrea, Tripati, Aradhna
• Format: Dataset
• Language: unknown
• Published: figshare 2022
• Subjects: 40104 Climate Change Processes; FOS Earth and related environmental sciences; Geology; Paleoclimatology; 40310 Sedimentology; 40313 Tectonics; permafrost
• Online Access: https://dx.doi.org/10.6084/m9.figshare.19033130.v2; https://figshare.com/articles/dataset/Plio-Pleistocene_climate_record_on_the_Tibetan_plateau/19033130/2

Plio-Pleistocene climate record on the Tibetan plateau (4.3 Ma to 0.8 Ma). Supplementary Data 1 . Results of carbonate (CaCO 3 ) content and carbonate stable isotopes including oxygen (δ 18 O c ), carbon (δ 13 C c ), and clumped isotopes (Δ 47 ), as well as grain size and a suite of organic proxies including total nitrogen (TN), total organic carbon (TOC), carbon to nitrogen ratios (C/N), and carbon isotope ratios in organic matter (δ 13 C org ). Clumped isotopes raw data, cross plots of δ 18 O c and ∆ 47- based temperature, calculations related to mean annual air temperature calculation (MAAT), and surface uplift estimate are also included. Supplementary Data 2 . Estimate of mean annual air temperature (MAAT) using a different temperature-∆ 47 calibration for comparison. Supplementary Data 3 . Calculation of permafrost thawing area and carbon release. Supplement to Cheng F. et al. , Alpine permafrost could account for a quarter of thawed carbon based on Plio-Pleistocene paleoclimate analogue, Nature Communications.