Delta 18O values of mudrocks: More evidence for an 18O-buffered ocean

Details Delta 18O values of mudrocks: More evidence for an 18O-buffered ocean Delta 18O values of mudrocks: More evidence for an 18O-buffered ocean

Sep 1996

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1996gecoa..60.3347l&link_type=abstract

Geochimica et Cosmochimica Acta, vol. 60, Issue 17, pp.3347-3352

Physics

5

Scientific paper

The whole-rock 18 O of mudrocks, as well as the 18 O of the
clay-sized silicate fraction, does not change in any systematic manner
over Paleozoic and late Proterozoic time. Therefore, the 18 O of the
ocean has not changed (except a per mil or so as the result of
glaciation/deglaciation) over the last billion years of Earth history.

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