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Archive · collection · 1996

Stable oxygen isotope record of foraminifera from the Ontong Java Plateau

Listed in PANGAEA and DataCite — shown once because both records carry DOI 10.1594/pangaea.711824

We provide a reconstruction of atmospheric CO2 from deep-sea sediments, for the past 625000 years (Milankovitch chron).

Description

Our database consists of a Milankovitch template of sea-level variation in combination with a unique data set for the deep-sea record for Ontong Java plateau in the western equatorial Pacific. We redate the Vostok ice-core data of Barnola et al. (1987, doi:10.1038/329408a0).

To make the reconstructions we employ multiple regression between deep-sea data, on one hand, and ice-core CO2 data in Antarctica, on the other. The patterns of correlation suggest that the main factors controlling atmospheric CO2 can be described as a combination of sea-level state and sea-level change. For best results squared values of state and change are used.

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The square-of-sea-level rule agrees with the concept that shelf processes are important modulators of atmospheric CO2 (e.g., budgets of shelf organic carbon and shelf carbonate, nitrate reduction). The square-of-change rule implies that, on short timescales, any major disturbance of the system results in a temporary rise in atmospheric CO2.

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Inferred from text
Geochemistry 74%
Provenance · 2 source records, 8 field assertions
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PANGAEAoai:pangaea.de:doi:10.1594/PANGAEA.71182414 d agoJSON v1
DataCite10.1594/pangaea.71182414 d agoJSON v1
FieldAssertionExtractorEvidence
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