Ocean climate variability in the eastern North Atlantic during interglacial marine isotope stage 11: A partial analogue to the Holocene? ...
Similar orbital geometry and greenhouse gas concentrations during marine isotope stage 11 (MIS 11) and the Holocene make stage 11 perhaps the best geological analogue period for the natural development of the present interglacial climate. Results of a detailed study of core MD01-2443 from the Iberia...
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Online Access: | https://dx.doi.org/10.7916/d8833rtj https://academiccommons.columbia.edu/doi/10.7916/D8833RTJ |
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ftdatacite:10.7916/d8833rtj 2024-10-13T14:09:26+00:00 Ocean climate variability in the eastern North Atlantic during interglacial marine isotope stage 11: A partial analogue to the Holocene? ... De Abreu, Lúcia Abrantes, Fátima F. Shackleton, Nicholas J. Tzedakis, Polychronis C. McManus, Jerry F. Oppo, Delia W. Hall, Michael A. 2005 https://dx.doi.org/10.7916/d8833rtj https://academiccommons.columbia.edu/doi/10.7916/D8833RTJ unknown Columbia University https://dx.doi.org/10.1029/2004pa001091 Ocean temperature Holocene Geologic Period Submarine geology Hydrology Paleoclimatology Text article-journal Articles ScholarlyArticle 2005 ftdatacite https://doi.org/10.7916/d8833rtj10.1029/2004pa001091 2024-10-01T11:38:12Z Similar orbital geometry and greenhouse gas concentrations during marine isotope stage 11 (MIS 11) and the Holocene make stage 11 perhaps the best geological analogue period for the natural development of the present interglacial climate. Results of a detailed study of core MD01-2443 from the Iberian margin suggest that sea surface conditions during stage 11 were not significantly different from those observed during the elapsed portion of the Holocene. Peak interglacial conditions during stage 11 lasted nearly 18 kyr, indicating a Holocene unperturbed by human activity might last an additional 6–7 kyr. A comparison of sea surface temperatures (SST) derived from planktonic foraminifera for all interglacial intervals of the last million years reveals that warm temperatures during peak interglacials MIS 1, 5e, and 11 were higher on the Iberian margin than during substage 7e and most of 9e. The SST results are supported by heavier δ18O values, particularly during 7e, indicating colder SSTs and a larger residual ... Article in Journal/Newspaper North Atlantic Planktonic foraminifera DataCite |
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unknown |
topic |
Ocean temperature Holocene Geologic Period Submarine geology Hydrology Paleoclimatology |
spellingShingle |
Ocean temperature Holocene Geologic Period Submarine geology Hydrology Paleoclimatology De Abreu, Lúcia Abrantes, Fátima F. Shackleton, Nicholas J. Tzedakis, Polychronis C. McManus, Jerry F. Oppo, Delia W. Hall, Michael A. Ocean climate variability in the eastern North Atlantic during interglacial marine isotope stage 11: A partial analogue to the Holocene? ... |
topic_facet |
Ocean temperature Holocene Geologic Period Submarine geology Hydrology Paleoclimatology |
description |
Similar orbital geometry and greenhouse gas concentrations during marine isotope stage 11 (MIS 11) and the Holocene make stage 11 perhaps the best geological analogue period for the natural development of the present interglacial climate. Results of a detailed study of core MD01-2443 from the Iberian margin suggest that sea surface conditions during stage 11 were not significantly different from those observed during the elapsed portion of the Holocene. Peak interglacial conditions during stage 11 lasted nearly 18 kyr, indicating a Holocene unperturbed by human activity might last an additional 6–7 kyr. A comparison of sea surface temperatures (SST) derived from planktonic foraminifera for all interglacial intervals of the last million years reveals that warm temperatures during peak interglacials MIS 1, 5e, and 11 were higher on the Iberian margin than during substage 7e and most of 9e. The SST results are supported by heavier δ18O values, particularly during 7e, indicating colder SSTs and a larger residual ... |
format |
Article in Journal/Newspaper |
author |
De Abreu, Lúcia Abrantes, Fátima F. Shackleton, Nicholas J. Tzedakis, Polychronis C. McManus, Jerry F. Oppo, Delia W. Hall, Michael A. |
author_facet |
De Abreu, Lúcia Abrantes, Fátima F. Shackleton, Nicholas J. Tzedakis, Polychronis C. McManus, Jerry F. Oppo, Delia W. Hall, Michael A. |
author_sort |
De Abreu, Lúcia |
title |
Ocean climate variability in the eastern North Atlantic during interglacial marine isotope stage 11: A partial analogue to the Holocene? ... |
title_short |
Ocean climate variability in the eastern North Atlantic during interglacial marine isotope stage 11: A partial analogue to the Holocene? ... |
title_full |
Ocean climate variability in the eastern North Atlantic during interglacial marine isotope stage 11: A partial analogue to the Holocene? ... |
title_fullStr |
Ocean climate variability in the eastern North Atlantic during interglacial marine isotope stage 11: A partial analogue to the Holocene? ... |
title_full_unstemmed |
Ocean climate variability in the eastern North Atlantic during interglacial marine isotope stage 11: A partial analogue to the Holocene? ... |
title_sort |
ocean climate variability in the eastern north atlantic during interglacial marine isotope stage 11: a partial analogue to the holocene? ... |
publisher |
Columbia University |
publishDate |
2005 |
url |
https://dx.doi.org/10.7916/d8833rtj https://academiccommons.columbia.edu/doi/10.7916/D8833RTJ |
genre |
North Atlantic Planktonic foraminifera |
genre_facet |
North Atlantic Planktonic foraminifera |
op_relation |
https://dx.doi.org/10.1029/2004pa001091 |
op_doi |
https://doi.org/10.7916/d8833rtj10.1029/2004pa001091 |
_version_ |
1812816398788853760 |