Deglacial abrupt climate change in the Atlantic Warm Pool: A Gulf of Mexico perspective
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 se...
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fttriple:oai:gotriple.eu:10670/1.0plm3i 2023-05-15T13:58:36+02:00 Deglacial abrupt climate change in the Atlantic Warm Pool: A Gulf of Mexico perspective Williams, Carlie Flower, Benjamin P. Hastings, David W. Guilderson, Thomas P. Quinn, Kelly A. Goddard, Ethan A. 2010-01-01 https://doi.org/10.1029/2010PA001928 https://archimer.ifremer.fr/doc/00230/34137/33059.pdf https://archimer.ifremer.fr/doc/00230/34137/ en eng Amer Geophysical Union doi:10.1029/2010PA001928 10670/1.0plm3i https://archimer.ifremer.fr/doc/00230/34137/33059.pdf https://archimer.ifremer.fr/doc/00230/34137/ other Archimer, archive institutionnelle de l'Ifremer Paleoceanography (0883-8305) (Amer Geophysical Union), 2010-12 , Vol. 25 , N. 4 / PA4221 , P. 1-12 geo envir Text https://vocabularies.coar-repositories.org/resource_types/c_18cf/ 2010 fttriple https://doi.org/10.1029/2010PA001928 2023-01-22T16:47:06Z 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. Text Antarc* Antarctic Greenland Greenland ice core ice core North Atlantic Orca Unknown Antarctic Greenland Paleoceanography 25 4 n/a n/a |
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geo envir Williams, Carlie Flower, Benjamin P. Hastings, David W. Guilderson, Thomas P. Quinn, Kelly A. Goddard, Ethan A. Deglacial abrupt climate change in the Atlantic Warm Pool: A Gulf of Mexico perspective |
topic_facet |
geo envir |
description |
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. |
format |
Text |
author |
Williams, Carlie Flower, Benjamin P. Hastings, David W. Guilderson, Thomas P. Quinn, Kelly A. Goddard, Ethan A. |
author_facet |
Williams, Carlie Flower, Benjamin P. Hastings, David W. Guilderson, Thomas P. Quinn, Kelly A. Goddard, Ethan A. |
author_sort |
Williams, Carlie |
title |
Deglacial abrupt climate change in the Atlantic Warm Pool: A Gulf of Mexico perspective |
title_short |
Deglacial abrupt climate change in the Atlantic Warm Pool: A Gulf of Mexico perspective |
title_full |
Deglacial abrupt climate change in the Atlantic Warm Pool: A Gulf of Mexico perspective |
title_fullStr |
Deglacial abrupt climate change in the Atlantic Warm Pool: A Gulf of Mexico perspective |
title_full_unstemmed |
Deglacial abrupt climate change in the Atlantic Warm Pool: A Gulf of Mexico perspective |
title_sort |
deglacial abrupt climate change in the atlantic warm pool: a gulf of mexico perspective |
publisher |
Amer Geophysical Union |
publishDate |
2010 |
url |
https://doi.org/10.1029/2010PA001928 https://archimer.ifremer.fr/doc/00230/34137/33059.pdf https://archimer.ifremer.fr/doc/00230/34137/ |
geographic |
Antarctic Greenland |
geographic_facet |
Antarctic Greenland |
genre |
Antarc* Antarctic Greenland Greenland ice core ice core North Atlantic Orca |
genre_facet |
Antarc* Antarctic Greenland Greenland ice core ice core North Atlantic Orca |
op_source |
Archimer, archive institutionnelle de l'Ifremer Paleoceanography (0883-8305) (Amer Geophysical Union), 2010-12 , Vol. 25 , N. 4 / PA4221 , P. 1-12 |
op_relation |
doi:10.1029/2010PA001928 10670/1.0plm3i https://archimer.ifremer.fr/doc/00230/34137/33059.pdf https://archimer.ifremer.fr/doc/00230/34137/ |
op_rights |
other |
op_doi |
https://doi.org/10.1029/2010PA001928 |
container_title |
Paleoceanography |
container_volume |
25 |
container_issue |
4 |
container_start_page |
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op_container_end_page |
n/a |
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1766266958749106176 |