(Table 2) Radiocarbon ages of eastern equatorial Pacific sediment cores

We use planktonic oxygen isotope (d18O) records spanning the last 30,000 years (kyr) to constrain the magnitude and spatial pattern of glacial cooling in the upwelling environment of the eastern equatorial Pacific (EEP). Fourteen new downcore d18O records were obtained from surface-dwelling plankton...

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Bibliographic Details
Main Authors: Koutavas, Athanasios, Lynch-Stieglitz, Jean
Format: Dataset
Language:English
Published: PANGAEA 2003
Subjects:
Age
PC
V19
V21
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.841354
https://doi.org/10.1594/PANGAEA.841354