Abstract

A record of atmospheric carbon dioxide (CO 2 ) concentrations measured on the EPICA (European Project for Ice Coring in Antarctica) Dome Concordia ice core extends the Vostok CO 2 record back to 650,000 years before the present (yr B.P.). Before 430,000 yr B.P., partial pressure of atmospheric CO 2 lies within the range of 260 and 180 parts per million by volume. This range is almost 30% smaller than that of the last four glacial cycles; however, the apparent sensitivity between deuterium and CO 2 remains stable throughout the six glacial cycles, suggesting that the relationship between CO 2 and Antarctic climate remained rather constant over this interval.

Keywords

Ice coreGlacial periodCarbon dioxide in Earth's atmospherePleistoceneCarbon cycleGeologyClimate changeCoringQuaternaryCarbon dioxidePaleoclimatologyRange (aeronautics)Physical geographyClimatologyIce sheetAtmospheric sciencesEnvironmental scienceOceanographyPaleontologyGeographyEcosystemChemistryDrillingEcology

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Publication Info

Year
2005
Type
article
Volume
310
Issue
5752
Pages
1313-1317
Citations
1057
Access
Closed

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Urs Siegenthaler, Thomas F. Stocker, Eric Monnin et al. (2005). Stable Carbon CycleClimate Relationship During the Late Pleistocene. Science , 310 (5752) , 1313-1317. https://doi.org/10.1126/science.1120130

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DOI
10.1126/science.1120130