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Sea-Level Fingerprinting as a Direct Test for the Source of Global Meltwater Pulse IA

Clark, P.U; Mitrovica, J.X; Milne, G.A; Tamisiea, M

Authors

P.U Clark

J.X Mitrovica

G.A Milne

M Tamisiea



Abstract

The ice reservoir that served as the source for the meltwater pulse IA remains enigmatic and controversial. We show that each of the melting scenarios that have been proposed for the event produces a distinct variation, or fingerprint, in the global distribution of meltwater. We compare sea-level fingerprints associated with various melting scenarios to existing sea-level records from Barbados and the Sunda Shelf and conclude that the southern Laurentide Ice Sheet could not have been the sole source of the meltwater pulse, whereas a substantial contribution from the Antarctic Ice Sheet is consistent with these records.

Citation

Clark, P., Mitrovica, J., Milne, G., & Tamisiea, M. (2002). Sea-Level Fingerprinting as a Direct Test for the Source of Global Meltwater Pulse IA. Science, 295(5564), 2438-2441. https://doi.org/10.1126/science.1068797

Journal Article Type Article
Publication Date 2002-03
Deposit Date Mar 15, 2007
Journal Science
Print ISSN 0036-8075
Electronic ISSN 1095-9203
Publisher American Association for the Advancement of Science
Peer Reviewed Peer Reviewed
Volume 295
Issue 5564
Pages 2438-2441
DOI https://doi.org/10.1126/science.1068797
Keywords Laurentide ice-sheet, Younger dryas event, Record, Ocean, Model, Circulation, Corals, Deglaciation, Discharge, Mexico.
Publisher URL http://www.sciencemag.org/cgi/content/abstract/295/5564/2438