(Table 2) Detrital Sr isotope ratios of sediment core RC11-83

Sr isotope ratios of the terrigenous sediments from the Cape Basin (southeast Atlantic Ocean) exhibit a systematic pattern of climate-related variability from the Holocene through the last glacial period. Values are high during warm climate intervals (marine isotope stages (MISs) 1 and 3) and lower...

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Bibliographic Details
Main Authors: Ruthberg, Randye L, Goldstein, Steven L, Hemming, Sidney R, Anderson, Robert F
Format: Dataset
Language:English
Published: PANGAEA 2005
Subjects:
AGE
PC
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.837313
https://doi.org/10.1594/PANGAEA.837313