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...

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Bibliographic Details
Main Authors: Sarnthein, Michael, Winn, Kyaw
Format: Other/Unknown Material
Language:English
Published: PANGAEA 1991
Subjects:
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.803254
https://doi.org/10.1594/PANGAEA.803254