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The residence time of Southern Ocean surface waters and the 100,000-year ice age cycle

Type of publication Peer-reviewed
Publikationsform Original article (peer-reviewed)
Author Hasenfratz Adam P., Jaccard Samuel L., Martínez-García Alfredo, Sigman Daniel M., Hodell David A., Vance Derek, Bernasconi Stefano M., Kleiven Helga (Kikki) F., Haumann F. Alexander, Haug Gerald H.,
Project The role of Southern Ocean stratification in future ocean CO2 and heat uptake
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Original article (peer-reviewed)

Journal Science
Volume (Issue) 363(6431)
Page(s) 1080 - 1084
Title of proceedings Science
DOI 10.1126/science.aat7067

Abstract

From 1.25 million to 700,000 years ago, the ice age cycle deepened and lengthened from 41,000- to 100,000-year periodicity, a transition that remains unexplained. Using surface- and bottom-dwelling foraminifera from the Antarctic Zone of the Southern Ocean to reconstruct the deep-to-surface supply of water during the ice ages of the past 1.5 million years, we found that a reduction in deep water supply and a concomitant freshening of the surface ocean coincided with the emergence of the high-amplitude 100,000-year glacial cycle. We propose that this slowing of deep-to-surface circulation (i.e., a longer residence time for Antarctic surface waters) prolonged ice ages by allowing the Antarctic halocline to strengthen, which increased the resistance of the Antarctic upper water column to orbitally paced drivers of carbon dioxide release.
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