Late-middle Eocene glacioeustacy : evidence from stable isotopes and foraminifera of the the [sic] Planktonic foraminiferan zone P14 (Truncorotaloides rohri zone), Mossy Grove Core, Hinds County, Mississippi
Glacioeustatic control of a late-middle Eocene oxygen isotope record is evident from the comparison of such a record with an independent proxy for sea-level. The data, δ18O and planktonic:benthic foraminifera ratios, were determined from samples of the Mossy Grove Core, Hinds County, Mississippi....
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| Format: | Others |
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2011
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| Online Access: | http://cardinalscholar.bsu.edu/handle/handle/186426 http://liblink.bsu.edu/uhtbin/catkey/1117851 |