(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...
Main Authors: | , , , |
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Format: | Dataset |
Language: | English |
Published: |
PANGAEA
2005
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.837313 https://doi.org/10.1594/PANGAEA.837313 |