Centennial-scale changes in the global carbon cycle during the last deglaciation

Shaun A. Marcott (), Thomas K. Bauska, Christo Buizert, Eric J. Steig, Julia L. Rosen, Kurt M. Cuffey, T. J. Fudge, Jeffery P. Severinghaus, Jinho Ahn, Michael L. Kalk, Joseph R. McConnell, Todd Sowers, Kendrick C. Taylor, James W. C. White and Edward J. Brook
Additional contact information
Shaun A. Marcott: College of Earth, Ocean, and Atmospheric Sciences, Oregon State University
Thomas K. Bauska: College of Earth, Ocean, and Atmospheric Sciences, Oregon State University
Christo Buizert: College of Earth, Ocean, and Atmospheric Sciences, Oregon State University
Eric J. Steig: University of Washington
Julia L. Rosen: College of Earth, Ocean, and Atmospheric Sciences, Oregon State University
Kurt M. Cuffey: University of California
T. J. Fudge: University of Washington
Jeffery P. Severinghaus: Scripps Institution of Oceanography, University of California
Jinho Ahn: School of Earth and Environmental Sciences, Seoul National University
Michael L. Kalk: College of Earth, Ocean, and Atmospheric Sciences, Oregon State University
Joseph R. McConnell: Desert Research Institute, Nevada System of Higher Education
Todd Sowers: Earth and Environmental Systems Institute, Pennsylvania State University, University Park
Kendrick C. Taylor: Desert Research Institute, Nevada System of Higher Education
James W. C. White: INSTAAR, University of Colorado
Edward J. Brook: College of Earth, Ocean, and Atmospheric Sciences, Oregon State University

Nature, 2014, vol. 514, issue 7524, 616-619

Abstract: Carbon dioxide and methane records from a West Antarctic ice core show that although gradual variations in the concentration of atmospheric carbon dioxide during the last glacial termination are linked to changes in Antarctic temperature, the concentration underwent three abrupt, centennial-scale changes related to sudden climate changes in the Northern Hemisphere.

Date: 2014
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DOI: 10.1038/nature13799

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