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Article
Deglacial Abrupt Climate Change in the Atlantic Warm Pool: A Gulf of Mexico Perspective
Paleoceanography
  • Carlie Williams, University of South Florida St. Petersburg
  • Benjamin P. Flower, University of South Florida St. Petersburg
  • David W. Hastings, Eckerd College
  • Thomas P. Guilderson, Lawrence Livermore National Laboratory
  • Kelly A. Quinn, University of South Florida St. Petersburg
  • Ethan A. Goddard, University of South Florida St. Petersburg
Document Type
Article
Publication Date
12-7-2010
Digital Object Identifier (DOI)
dx.doi.org/10.1029/2010PA001928
Disciplines
Abstract
During the last deglaciation, Greenland ice core and North Atlantic sediment records exhibit multiple abrupt climate events including the Younger Dryas cold episode (12.9-11.7 ka). However, evidence for the presence of the Younger Dryas in the Gulf of Mexico (GOM) and the relationship between GOM sea surface temperature (SST) and high-latitude climate change is less clear. We present new Mg/Ca-SST records from two varieties of the planktonic foraminifer Globigerinoides ruber (white and pink) to assess northern GOM SST history from approximately 18.4-10.8 ka. Thirty-five accelerator mass spectrometry (AMS) C-14 dates from Orca Basin core MD02-2550 provide excellent age control and document high sedimentation rates (similar to 40 cm/kyr). G. ruber (white and pink) Mg/Ca-SST data exhibit increases (similar to 4.6 +/- 0.6 degrees C and similar to 2.2 +/- 0.5 degrees C, respectively) from at least 17.8-16.6 ka, with nearly decadal resolution that are early relative to the onset of the Bolling-Allerod interstadial. Moreover, G. ruber (white) SST decreases at 16.0-14.7 ka (similar to 1.0 +/- 0.5 degrees C) and 12.8-11.6 ka (similar to 2.4 +/- 0.6 degrees C) correlate to the Oldest and Younger Dryas in Greenland and Cariaco Basin. The G. ruber (pink) SST record, which reflects differences in seasonality and/or depth habitat, is often not in phase with G. ruber (white) and closely resembles Antarctic air temperature records. Overall, it appears that Orca Basin SST records follow Antarctic air temperature early in the deglacial sequence and exhibit enhanced seasonality during Greenland stadials.
Citation / Publisher Attribution

Paleoceanography, v. 25, article PA4221.

Citation Information
Carlie Williams, Benjamin P. Flower, David W. Hastings, Thomas P. Guilderson, et al.. "Deglacial Abrupt Climate Change in the Atlantic Warm Pool: A Gulf of Mexico Perspective" Paleoceanography Vol. 25 (2010)
Available at: http://works.bepress.com/benjamin_flower/3/