(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

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).

Bibliographic Details
Main Authors: Abramovich, Sigal, Keller, Gerta, Stüben, Doris, Berner, Zsolt
Format: Dataset
Language:English
Published: PANGAEA - Data Publisher for Earth & Environmental Science 2003
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.695316
https://doi.pangaea.de/10.1594/PANGAEA.695316
Description
Summary: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).