Shells from Montehano and Carasa, which had enough material to be cut into several subsamples (see detailed explanation in the “Methods” section), showed a trend of lower values at the umbo toward slightly higher values at the ventral margin of the shells for δ 2 H values of both the SOM and IOM (Table 1 , Supplementary Note 1 , Supplementary Figs.
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Stable isotopes in the shell organic matrix for (paleo)environmental reconstructions.
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