Stable carbon and oxygen isotope ratios of foraminifera from sediments of the Iberian margin, supplement to: Shackleton, Nicholas J; Hall, Michael A; Vincent, Edith (2000): Phase relationships between millennial-scale events 64,000-24,000 years ago. Paleoceanography, 15(6), 565-569

A core recovered on the Iberian margin off southern Portugal can be correlated with Greenland ice cores using oxygen isotope variability in planktonic foraminifera which closely matches the ice core records of temperature over Greenland. Our age model identifies the base of every interstadial betwee...

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Bibliographic Details
Main Authors: Shackleton, Nicholas J, Hall, Michael A, Vincent, Edith
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA - Data Publisher for Earth & Environmental Science 2000
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.700954
https://doi.pangaea.de/10.1594/PANGAEA.700954