Age model, sedimentation rates and stable carbon isotopic rates of sediment core GeoB6212-1

Abrupt millennial-scale climate change events of the last deglaciation (i.e. Heinrich Stadial 1 and the Younger Dryas) were accompanied by marked increases in atmospheric CO2 (CO2atm) and decreases in its stable carbon isotopic ratios (d13C), i.e. d13CO2atm, presumably due to outgassing from the oce...

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Bibliographic Details
Main Authors: de Carvalho Campos, Marília, Chiessi, Cristiano Mazur, Voigt, Ines, Piola, Alberto R, Kuhnert, Henning, Mulitza, Stefan
Format: Dataset
Language:English
Published: PANGAEA 2017
Subjects:
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.874350
https://doi.org/10.1594/PANGAEA.874350