Sedimentology, age models and stable isotope ratios of sediment cores from the equatorial Pacific
Based on detailed reconstructions of global distribution patterns, both paleoproductivity and the benthic d13C record of CO2, which is dissolved in the deep ocean, strongly differed between the Last Glacial Maximum and the Holocene. With the onset of Termination I about 15,000 years ago, the new (ex...
Main Authors: | , |
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Format: | Other/Unknown Material |
Language: | English |
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PANGAEA
1991
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.803254 https://doi.org/10.1594/PANGAEA.803254 |