Paleoclimate history of Galapagos surface waters over the last 135,000 yr
Records of planktonic and benthic foraminiferal δ18O and planktonic Mg/Ca from core TR163-22, just northwest of the Galápagos Islands, reveal a detailed (250–450 year resolution) climate history of the region over the last 135 thousand years (kyr). Sea surface temperatures (SSTs), reconstructed from...
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ftucambridgeesc:oai:eprints.esc.cam.ac.uk:471 2023-05-15T13:32:21+02:00 Paleoclimate history of Galapagos surface waters over the last 135,000 yr Lea, D. W. Pak, D. K. Belanger, C. L. Spero, H. J. Hall, M. A. Shackleton, N. J. 2006-06 application/pdf http://eprints.esc.cam.ac.uk/471/ http://eprints.esc.cam.ac.uk/471/1/Hall_Shackleton_QSR_25_2006.pdf https://doi.org/10.1016/j.quascirev.2005.11.010 en eng http://eprints.esc.cam.ac.uk/471/1/Hall_Shackleton_QSR_25_2006.pdf Lea, D. W. and Pak, D. K. and Belanger, C. L. and Spero, H. J. and Hall, M. A. and Shackleton, N. J. (2006) Paleoclimate history of Galapagos surface waters over the last 135,000 yr. Quaternary Science Reviews, 25 (11-12). pp. 1152-1167. DOI https://doi.org/10.1016/j.quascirev.2005.11.010 <https://doi.org/10.1016/j.quascirev.2005.11.010> 01 - Climate Change and Earth-Ocean Atmosphere Systems Article PeerReviewed 2006 ftucambridgeesc https://doi.org/10.1016/j.quascirev.2005.11.010 2020-08-27T18:08:32Z Records of planktonic and benthic foraminiferal δ18O and planktonic Mg/Ca from core TR163-22, just northwest of the Galápagos Islands, reveal a detailed (250–450 year resolution) climate history of the region over the last 135 thousand years (kyr). Sea surface temperatures (SSTs), reconstructed from G. ruber Mg/Ca, averaged 24.3±0.4 °C during the Holocene, 22.6±0.6 °C during marine isotope stage (MIS) 2, 3 and 4, and 26.0±0.9 °C during MIS 5e. Changes in SST lead changes in both planktonic and benthic δ18O by an average not, vert, similar3 kyr, suggesting that SST changes in this region predated continental ice volume changes. Changes in SST display clear millennial scale variability, especially in marine isotope stage 3, with behavior somewhat similar to Antarctic proxy air temperature and South Pacific SST records. Removal of the temperature component from the planktonic δ18O record demonstrates that glacial-interglacial δ18O-water changes at this site were 1.0±0.2‰, similar to estimates for mean ocean shifts, implying that salinity changes due to regional hydrological variation between the Last Glacial Maximum and Holocene in the Galápagos region were minimal. Comparison between the TR163-22 SST record and an SST record from core TR163-19 North of the Equatorial Front reveals a largely similar broad-scale climate history, suggesting that changes in the Galápagos region were caused by large scale forcing rather than by local or regional dynamical changes. Changes in atmospheric greenhouse forcing are the most plausible explanation for the observed large-scale climate changes in the eastern equatorial Pacific. Article in Journal/Newspaper Antarc* Antarctic University of Cambridge, Department of Earth Sciences: ESC Publications Antarctic Galapagos Pacific Quaternary Science Reviews 25 11-12 1152 1167 |
institution |
Open Polar |
collection |
University of Cambridge, Department of Earth Sciences: ESC Publications |
op_collection_id |
ftucambridgeesc |
language |
English |
topic |
01 - Climate Change and Earth-Ocean Atmosphere Systems |
spellingShingle |
01 - Climate Change and Earth-Ocean Atmosphere Systems Lea, D. W. Pak, D. K. Belanger, C. L. Spero, H. J. Hall, M. A. Shackleton, N. J. Paleoclimate history of Galapagos surface waters over the last 135,000 yr |
topic_facet |
01 - Climate Change and Earth-Ocean Atmosphere Systems |
description |
Records of planktonic and benthic foraminiferal δ18O and planktonic Mg/Ca from core TR163-22, just northwest of the Galápagos Islands, reveal a detailed (250–450 year resolution) climate history of the region over the last 135 thousand years (kyr). Sea surface temperatures (SSTs), reconstructed from G. ruber Mg/Ca, averaged 24.3±0.4 °C during the Holocene, 22.6±0.6 °C during marine isotope stage (MIS) 2, 3 and 4, and 26.0±0.9 °C during MIS 5e. Changes in SST lead changes in both planktonic and benthic δ18O by an average not, vert, similar3 kyr, suggesting that SST changes in this region predated continental ice volume changes. Changes in SST display clear millennial scale variability, especially in marine isotope stage 3, with behavior somewhat similar to Antarctic proxy air temperature and South Pacific SST records. Removal of the temperature component from the planktonic δ18O record demonstrates that glacial-interglacial δ18O-water changes at this site were 1.0±0.2‰, similar to estimates for mean ocean shifts, implying that salinity changes due to regional hydrological variation between the Last Glacial Maximum and Holocene in the Galápagos region were minimal. Comparison between the TR163-22 SST record and an SST record from core TR163-19 North of the Equatorial Front reveals a largely similar broad-scale climate history, suggesting that changes in the Galápagos region were caused by large scale forcing rather than by local or regional dynamical changes. Changes in atmospheric greenhouse forcing are the most plausible explanation for the observed large-scale climate changes in the eastern equatorial Pacific. |
format |
Article in Journal/Newspaper |
author |
Lea, D. W. Pak, D. K. Belanger, C. L. Spero, H. J. Hall, M. A. Shackleton, N. J. |
author_facet |
Lea, D. W. Pak, D. K. Belanger, C. L. Spero, H. J. Hall, M. A. Shackleton, N. J. |
author_sort |
Lea, D. W. |
title |
Paleoclimate history of Galapagos surface waters over the last 135,000 yr |
title_short |
Paleoclimate history of Galapagos surface waters over the last 135,000 yr |
title_full |
Paleoclimate history of Galapagos surface waters over the last 135,000 yr |
title_fullStr |
Paleoclimate history of Galapagos surface waters over the last 135,000 yr |
title_full_unstemmed |
Paleoclimate history of Galapagos surface waters over the last 135,000 yr |
title_sort |
paleoclimate history of galapagos surface waters over the last 135,000 yr |
publishDate |
2006 |
url |
http://eprints.esc.cam.ac.uk/471/ http://eprints.esc.cam.ac.uk/471/1/Hall_Shackleton_QSR_25_2006.pdf https://doi.org/10.1016/j.quascirev.2005.11.010 |
geographic |
Antarctic Galapagos Pacific |
geographic_facet |
Antarctic Galapagos Pacific |
genre |
Antarc* Antarctic |
genre_facet |
Antarc* Antarctic |
op_relation |
http://eprints.esc.cam.ac.uk/471/1/Hall_Shackleton_QSR_25_2006.pdf Lea, D. W. and Pak, D. K. and Belanger, C. L. and Spero, H. J. and Hall, M. A. and Shackleton, N. J. (2006) Paleoclimate history of Galapagos surface waters over the last 135,000 yr. Quaternary Science Reviews, 25 (11-12). pp. 1152-1167. DOI https://doi.org/10.1016/j.quascirev.2005.11.010 <https://doi.org/10.1016/j.quascirev.2005.11.010> |
op_doi |
https://doi.org/10.1016/j.quascirev.2005.11.010 |
container_title |
Quaternary Science Reviews |
container_volume |
25 |
container_issue |
11-12 |
container_start_page |
1152 |
op_container_end_page |
1167 |
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1766026058575904768 |