(Table A1) Stable isotope ratios and paleotemperature calculation of selected planktonic foraminifera from late Campanian and Maastrichtian sediments of DSDP Hole 62-463 from the Mid-Pacific mountains@en
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Paleotemperature estimates were calculated using the equation of Erez and Luz (1983), with seawater delta18O = -1.2 per mil PDB corresponding to a continental ice-free world (Shackleton and Kennett, 1975).
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2026-04-14
