Evidence for obliquity forcing of glacial termination II
Variations in the intensity of high-latitude Northern Hemisphere summer insolation, driven largely by precession of the equinoxes, are widely thought to control the timing of Late Pleistocene glacial terminations. However, recently it has been suggested that changes in Earth's obliquity may be...
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American Association for the Advancement of Science
2009
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Online Access: | https://eprints.gla.ac.uk/7674/ https://doi.org/10.1126/science.1170371 |
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ftuglasgow:oai:eprints.gla.ac.uk:7674 2024-06-02T08:11:17+00:00 Evidence for obliquity forcing of glacial termination II Drysdale, R.N. Hellstrom, J.C. Zanchetta, G. Fallick, A.E. Sanchez Goni, M.F. Couchoud, I. McDonald, J. Maas, R. Lohmann, G. Isola, I. 2009-09-18 https://eprints.gla.ac.uk/7674/ https://doi.org/10.1126/science.1170371 unknown American Association for the Advancement of Science Drysdale, R.N., Hellstrom, J.C., Zanchetta, G., Fallick, A.E. <http://eprints.gla.ac.uk/view/author/1774.html>, Sanchez Goni, M.F., Couchoud, I., McDonald, J., Maas, R., Lohmann, G. and Isola, I. (2009) Evidence for obliquity forcing of glacial termination II. Science <https://eprints.gla.ac.uk/view/journal_volume/Science.html>, 325(5947), pp. 1527-1531. (doi:10.1126/science.1170371 <https://doi.org/10.1126/science.1170371>) QE Geology Articles PeerReviewed 2009 ftuglasgow https://doi.org/10.1126/science.1170371 2024-05-06T15:05:45Z Variations in the intensity of high-latitude Northern Hemisphere summer insolation, driven largely by precession of the equinoxes, are widely thought to control the timing of Late Pleistocene glacial terminations. However, recently it has been suggested that changes in Earth's obliquity may be a more important mechanism. We present a new speleothem-based North Atlantic marine chronology which shows that the penultimate glacial termination (Termination II) commenced 141,000 ± 2,500 years before present, too early to be explained by Northern Hemisphere summer insolation but consistent with changes in Earth's obliquity. Our record reveals that Terminations I and II are separated by three obliquity cycles and that they started at near-identical obliquity phases. Article in Journal/Newspaper North Atlantic University of Glasgow: Enlighten - Publications Science 325 5947 1527 1531 |
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University of Glasgow: Enlighten - Publications |
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ftuglasgow |
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unknown |
topic |
QE Geology |
spellingShingle |
QE Geology Drysdale, R.N. Hellstrom, J.C. Zanchetta, G. Fallick, A.E. Sanchez Goni, M.F. Couchoud, I. McDonald, J. Maas, R. Lohmann, G. Isola, I. Evidence for obliquity forcing of glacial termination II |
topic_facet |
QE Geology |
description |
Variations in the intensity of high-latitude Northern Hemisphere summer insolation, driven largely by precession of the equinoxes, are widely thought to control the timing of Late Pleistocene glacial terminations. However, recently it has been suggested that changes in Earth's obliquity may be a more important mechanism. We present a new speleothem-based North Atlantic marine chronology which shows that the penultimate glacial termination (Termination II) commenced 141,000 ± 2,500 years before present, too early to be explained by Northern Hemisphere summer insolation but consistent with changes in Earth's obliquity. Our record reveals that Terminations I and II are separated by three obliquity cycles and that they started at near-identical obliquity phases. |
format |
Article in Journal/Newspaper |
author |
Drysdale, R.N. Hellstrom, J.C. Zanchetta, G. Fallick, A.E. Sanchez Goni, M.F. Couchoud, I. McDonald, J. Maas, R. Lohmann, G. Isola, I. |
author_facet |
Drysdale, R.N. Hellstrom, J.C. Zanchetta, G. Fallick, A.E. Sanchez Goni, M.F. Couchoud, I. McDonald, J. Maas, R. Lohmann, G. Isola, I. |
author_sort |
Drysdale, R.N. |
title |
Evidence for obliquity forcing of glacial termination II |
title_short |
Evidence for obliquity forcing of glacial termination II |
title_full |
Evidence for obliquity forcing of glacial termination II |
title_fullStr |
Evidence for obliquity forcing of glacial termination II |
title_full_unstemmed |
Evidence for obliquity forcing of glacial termination II |
title_sort |
evidence for obliquity forcing of glacial termination ii |
publisher |
American Association for the Advancement of Science |
publishDate |
2009 |
url |
https://eprints.gla.ac.uk/7674/ https://doi.org/10.1126/science.1170371 |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_relation |
Drysdale, R.N., Hellstrom, J.C., Zanchetta, G., Fallick, A.E. <http://eprints.gla.ac.uk/view/author/1774.html>, Sanchez Goni, M.F., Couchoud, I., McDonald, J., Maas, R., Lohmann, G. and Isola, I. (2009) Evidence for obliquity forcing of glacial termination II. Science <https://eprints.gla.ac.uk/view/journal_volume/Science.html>, 325(5947), pp. 1527-1531. (doi:10.1126/science.1170371 <https://doi.org/10.1126/science.1170371>) |
op_doi |
https://doi.org/10.1126/science.1170371 |
container_title |
Science |
container_volume |
325 |
container_issue |
5947 |
container_start_page |
1527 |
op_container_end_page |
1531 |
_version_ |
1800757381433393152 |