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Shell+oxygen isotopes.tif

By Emma Versteegh (97197)


Thesis Figure 1.6: A transverse section through a Unio tumidus shell and the shell aragonite δ18O (δ18Oar) record of the same specimen. Growth cessations, usually occurring in winter, are visible as dark internal growth lines in the shell and as narrow positive peaks in the shell δ18Oar record

Topics: Paleoclimatology, isotopes, shell
Year: 2012
DOI identifier: 10.6084/m9.figshare.90090.v1
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Provided by: FigShare
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