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. 2020 Sep 7;11:4436. doi: 10.1038/s41467-020-17887-x

Fig. 3. Early Eocene weathering, organic carbon burial and circulation changes.

Fig. 3

a The CO2 record as in Fig. 2. b The marine 187Os/188Os compilation from ref. 27 c the marine 87Sr/86Sr record from refs. 30,32,94. d The marine δ7Li are from ref. 33, with red symbols/line updated to the same age model as for the CO2 and δ18O data39. e The marine δ34S are from ref. 51 (red circles), with the updated age model to GTS2012 (green circles) from ref. 53 f, g Marine carbonate δ13C and δ18O, color coding refers to the same references as in Fig. 2c. Purple bar envelopes the δ34S increase, and “N” indicates the preceding CIE within C23n.2nH139. Light blue bar indicates the timing of temperature and CO2 decline after the EECO. Green light bar indicates the timing of potential circulation changes in the early Eocene, as demonstrated in the δ13C record of f. Overlying solid black and yellow bars represent the timing of volcanism2126.