DOI: 10.1126/science.269.5221.210. Climate Records Covering the Last Deglaciation

Climate Records Covering the Last Deglaciation

10.1126/science.269.5221.210

Crossref journal-article

American Association for the Advancement of Science (AAAS)

Science (221)

Abstract

The oxygen-18/oxygen-16 ratio of molecular oxygen trapped in ice cores provides a time-stratigraphic marker for transferring the absolute chronology for the Greenland Ice Sheet Project (GISP) II ice core to the Vostok and Byrd ice cores in Antarctica. Comparison of the climate records from these cores suggests that, near the beginning of the last deglaciation, warming in Antarctica began approximately 3000 years before the onset of the warm Bølling period in Greenland. Atmospheric carbon dioxide and methane concentrations began to rise 2000 to 3000 years before the warming began in Greenland and must have contributed to deglaciation and warming of temperate and boreal regions in the Northern Hemisphere.

Bibliography

Sowers, T., & Bender, M. (1995). Climate Records Covering the Last Deglaciation. Science, 269(5221), 210â214.

Authors 2

Todd Sowers (first)
Michael Bender (additional)

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Dates

Type	When
Created	18 years, 10 months ago (Oct. 27, 2006, 2:19 p.m.)
Deposited	1 year, 7 months ago (Jan. 12, 2024, 6:50 p.m.)
Indexed	2 months, 3 weeks ago (June 5, 2025, 7:27 a.m.)
Issued	30 years, 1 month ago (July 14, 1995)
Published	30 years, 1 month ago (July 14, 1995)
Published Print	30 years, 1 month ago (July 14, 1995)

Funders 0

None

BibTeX

@article{Sowers_1995, title={Climate Records Covering the Last Deglaciation}, volume={269}, ISSN={1095-9203}, url={http://dx.doi.org/10.1126/science.269.5221.210}, DOI={10.1126/science.269.5221.210}, number={5221}, journal={Science}, publisher={American Association for the Advancement of Science (AAAS)}, author={Sowers, Todd and Bender, Michael}, year={1995}, month=jul, pages={210–214} }

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