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A new high-resolution paleotemperature record during the Middle–Late Ordovician transition derived from conodont δ18O paleo-thermometry

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posted on 31.03.2022, 09:14 authored by Kang Liu, Maosheng Jiang, Liyu Zhang, Daizhao Chen
Three supplementary tables (S1, S2, and S3) indicating the in-situ oxygen isotopic results of conodont apatite from the Kalpin Shuinichang-Dawangou composite section, Qinghu standard, and Durango standard, respectively.

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