(Table 1) Age determination of western North Atlantic sediment cores

Foraminiferal abundance, 14C ventilation ages, and stable isotope ratios in cores from high deposition rate locations in the western subtropical North Atlantic are used to infer changes in ocean and climate during the Younger Dryas (YD) and Last Glacial Maximum (LGM). The d18O of the surface dwellin...

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Bibliographic Details
Main Author: Keigwin, Lloyd D
Format: Dataset
Language:English
Published: PANGAEA 2004
Subjects:
Age
GC
GGC
JPC
ODP
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.837767
https://doi.org/10.1594/PANGAEA.837767