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Sea levels from ancient seashells

  • Schneider R
Nature (2014) 508(7497) 465-466
DOI: 10.1038/nature13328
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Abstract

The isotopic composition of oxygen in sea water correlates with changes in global mean sea level. Microfossils carrying oxygen-isotope signals have been used to extend sea-level records as far back as 5 million years ago. See Article p.477 RALPH

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Schneider, R. (2014). Sea levels from ancient seashells. Nature, 508(7497), 465–466. https://doi.org/10.1038/nature13328

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