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    Holocene (~4.5-1.7 cal. kyr BP) paleoenvironmental conditions in central Argentina inferred from entire-shell and intra-shell stable isotope composition of terrestrial gastropods by IDACOR, Yanes, Yurena, Cattáneo, Roxana, Izeta, Andrés D., Gordillo, Sandra, Costa, Thiago

    Published 2014
    “…Intra-shell isotopic profiles suggest that modern and fossil specimens deposited their shells throughout two-to-three summer/winter cycles. Intra-shell δ18O values varied ~5‰, matching with the seasonal variation of rain δ18O values. …”
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    info:ar-repo/semantics/artículo
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