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. 2021 Apr 1;16(4):e0248711. doi: 10.1371/journal.pone.0248711

Fig 3. Effects of the variables predicted by the univariate model of carbon isotope ratios selected based on the AICc.

Fig 3

The estimated Year slopes (c) which were explained by the oceanic Suess effect were used to correct the δ13Coto values prior to the estimation of Cresp.