Organic carbon paleo-pCO2 and marine-ice core correlations and chronology

Physics

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Oceanography: General: Paleoceanography, Global Change: Atmosphere, Atmospheric Composition And Structure: Evolution Of The Atmosphere

Scientific paper

Here we present evidence that marine organic matter δ13C measurements can closely reproduce the Vostok ice core CO2 record and, in addition, can be used to evaluate the absolute Vostok chronology and the transfer of that chronology between the marine and terrestrial realm. Our data supports recent speculations that the base of the Vostok ice core (2755 m) is still within oxygen isotope stage 7, in agreement with recent orbitally-tuned ice core chronologies.

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