(Appendix C) Stable isotope ratios and paleotemperature calculation of selected planktonic foraminifera from Maastrichtian sediments of DSDP Hole 74-525A from Walvis Ridge, South Atlantic

Absolute age estimates were determined based on average sedimentation rates within each planktonic foraminiferal biozone and magnetochron. 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-...

Full description

Bibliographic Details
Main Authors: Abramovich, Sigal, Keller, Gerta
Format: Dataset
Language:English
Published: PANGAEA - Data Publisher for Earth & Environmental Science 2003
Subjects:
AGE
Online Access:https://dx.doi.org/10.1594/pangaea.678298
https://doi.pangaea.de/10.1594/PANGAEA.678298
Description
Summary:Absolute age estimates were determined based on average sedimentation rates within each planktonic foraminiferal biozone and magnetochron. 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).