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. 2017 Aug 23;7:8310. doi: 10.1038/s41598-017-08234-0

Figure 1.

Figure 1

Comparison of the carbon isotope compositions of leaves of the fossil conifer Frenelopsis13Cleaf) obtained for each studied episode with the evolution of the carbon isotope composition of atmospheric CO213CCO2) throughout the Cretaceous estimated by Barral et al.16. Envelopes and bar errors correspond to ±1σ.