Enhanced climate instability in the North Atlantic and southern Europe during the Last Interglacial
Considerable ambiguity remains over the extent and nature of millennial/centennial-scale climate instability during the Last Interglacial (LIG). Here we analyse marine and terrestrial proxies from a deep-sea sediment sequence on the Portuguese Margin and combine results with an intensively dated Ita...
Published in: | Nature Communications |
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Springer Nature
2018
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Online Access: | http://eprints.esc.cam.ac.uk/4349/ http://eprints.esc.cam.ac.uk/4349/1/s41467-018-06683-3.pdf http://eprints.esc.cam.ac.uk/4349/2/41467_2018_6683_MOESM1_ESM.pdf http://eprints.esc.cam.ac.uk/4349/3/41467_2018_6683_MOESM2_ESM.pdf http://eprints.esc.cam.ac.uk/4349/4/41467_2018_6683_MOESM3_ESM.xlsx http://eprints.esc.cam.ac.uk/4349/5/41467_2018_6683_MOESM4_ESM.xlsx http://eprints.esc.cam.ac.uk/4349/6/41467_2018_6683_MOESM5_ESM.xlsx http://eprints.esc.cam.ac.uk/4349/7/41467_2018_6683_MOESM6_ESM.xlsx https://doi.org/10.1038/s41467-018-06683-3 |
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ftucambridgeesc:oai:eprints.esc.cam.ac.uk:4349 2023-05-15T16:29:05+02:00 Enhanced climate instability in the North Atlantic and southern Europe during the Last Interglacial Tzedakis, P. C. Drysdale, R. N. Margari, V. Skinner, L. C. Menviel, L. Rhodes, R. H. Taschetto, A. S. Hodell, D. A. Crowhurst, S. J. Hellstrom, J. C. Fallick, A. E. Grimalt, J. O. McManus, J. F. Martrat, B. Mokeddem, Z. Parrenin, F. Regattieri, E. Roe, K. Zanchetta, G. 2018 text http://eprints.esc.cam.ac.uk/4349/ http://eprints.esc.cam.ac.uk/4349/1/s41467-018-06683-3.pdf http://eprints.esc.cam.ac.uk/4349/2/41467_2018_6683_MOESM1_ESM.pdf http://eprints.esc.cam.ac.uk/4349/3/41467_2018_6683_MOESM2_ESM.pdf http://eprints.esc.cam.ac.uk/4349/4/41467_2018_6683_MOESM3_ESM.xlsx http://eprints.esc.cam.ac.uk/4349/5/41467_2018_6683_MOESM4_ESM.xlsx http://eprints.esc.cam.ac.uk/4349/6/41467_2018_6683_MOESM5_ESM.xlsx http://eprints.esc.cam.ac.uk/4349/7/41467_2018_6683_MOESM6_ESM.xlsx https://doi.org/10.1038/s41467-018-06683-3 en eng Springer Nature http://eprints.esc.cam.ac.uk/4349/1/s41467-018-06683-3.pdf http://eprints.esc.cam.ac.uk/4349/2/41467_2018_6683_MOESM1_ESM.pdf http://eprints.esc.cam.ac.uk/4349/3/41467_2018_6683_MOESM2_ESM.pdf http://eprints.esc.cam.ac.uk/4349/4/41467_2018_6683_MOESM3_ESM.xlsx http://eprints.esc.cam.ac.uk/4349/5/41467_2018_6683_MOESM4_ESM.xlsx http://eprints.esc.cam.ac.uk/4349/6/41467_2018_6683_MOESM5_ESM.xlsx http://eprints.esc.cam.ac.uk/4349/7/41467_2018_6683_MOESM6_ESM.xlsx Tzedakis, P. C. and Drysdale, R. N. and Margari, V. and Skinner, L. C. and Menviel, L. and Rhodes, R. H. and Taschetto, A. S. and Hodell, D. A. and Crowhurst, S. J. and Hellstrom, J. C. and Fallick, A. E. and Grimalt, J. O. and McManus, J. F. and Martrat, B. and Mokeddem, Z. and Parrenin, F. and Regattieri, E. and Roe, K. and Zanchetta, G. (2018) Enhanced climate instability in the North Atlantic and southern Europe during the Last Interglacial. Nature Communications, 9 (4235). ISSN 2041-1723 DOI https://doi.org/10.1038/s41467-018-06683-3 <https://doi.org/10.1038/s41467-018-06683-3> 01 - Climate Change and Earth-Ocean Atmosphere Systems Article PeerReviewed 2018 ftucambridgeesc https://doi.org/10.1038/s41467-018-06683-3 2020-08-27T18:09:58Z Considerable ambiguity remains over the extent and nature of millennial/centennial-scale climate instability during the Last Interglacial (LIG). Here we analyse marine and terrestrial proxies from a deep-sea sediment sequence on the Portuguese Margin and combine results with an intensively dated Italian speleothem record and climate-model experiments. The strongest expression of climate variability occurred during the transitions into and out of the LIG. Our records also document a series of multi-centennial intra-interglacial arid events in southern Europe, coherent with cold water-mass expansions in the North Atlantic. The spatial and temporal fingerprints of these changes indicate a reorganization of ocean surface circulation, consistent with low-intensity disruptions of the Atlantic meridional overturning circulation (AMOC). The amplitude of this LIG variability is greater than that observed in Holocene records. Episodic Greenland ice melt and runoff as a result of excess warmth may have contributed to AMOC weakening and increased climate instability throughout the LIG. Article in Journal/Newspaper Greenland North Atlantic University of Cambridge, Department of Earth Sciences: ESC Publications Greenland Nature Communications 9 1 |
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 Tzedakis, P. C. Drysdale, R. N. Margari, V. Skinner, L. C. Menviel, L. Rhodes, R. H. Taschetto, A. S. Hodell, D. A. Crowhurst, S. J. Hellstrom, J. C. Fallick, A. E. Grimalt, J. O. McManus, J. F. Martrat, B. Mokeddem, Z. Parrenin, F. Regattieri, E. Roe, K. Zanchetta, G. Enhanced climate instability in the North Atlantic and southern Europe during the Last Interglacial |
topic_facet |
01 - Climate Change and Earth-Ocean Atmosphere Systems |
description |
Considerable ambiguity remains over the extent and nature of millennial/centennial-scale climate instability during the Last Interglacial (LIG). Here we analyse marine and terrestrial proxies from a deep-sea sediment sequence on the Portuguese Margin and combine results with an intensively dated Italian speleothem record and climate-model experiments. The strongest expression of climate variability occurred during the transitions into and out of the LIG. Our records also document a series of multi-centennial intra-interglacial arid events in southern Europe, coherent with cold water-mass expansions in the North Atlantic. The spatial and temporal fingerprints of these changes indicate a reorganization of ocean surface circulation, consistent with low-intensity disruptions of the Atlantic meridional overturning circulation (AMOC). The amplitude of this LIG variability is greater than that observed in Holocene records. Episodic Greenland ice melt and runoff as a result of excess warmth may have contributed to AMOC weakening and increased climate instability throughout the LIG. |
format |
Article in Journal/Newspaper |
author |
Tzedakis, P. C. Drysdale, R. N. Margari, V. Skinner, L. C. Menviel, L. Rhodes, R. H. Taschetto, A. S. Hodell, D. A. Crowhurst, S. J. Hellstrom, J. C. Fallick, A. E. Grimalt, J. O. McManus, J. F. Martrat, B. Mokeddem, Z. Parrenin, F. Regattieri, E. Roe, K. Zanchetta, G. |
author_facet |
Tzedakis, P. C. Drysdale, R. N. Margari, V. Skinner, L. C. Menviel, L. Rhodes, R. H. Taschetto, A. S. Hodell, D. A. Crowhurst, S. J. Hellstrom, J. C. Fallick, A. E. Grimalt, J. O. McManus, J. F. Martrat, B. Mokeddem, Z. Parrenin, F. Regattieri, E. Roe, K. Zanchetta, G. |
author_sort |
Tzedakis, P. C. |
title |
Enhanced climate instability in the North Atlantic and southern Europe during the Last Interglacial |
title_short |
Enhanced climate instability in the North Atlantic and southern Europe during the Last Interglacial |
title_full |
Enhanced climate instability in the North Atlantic and southern Europe during the Last Interglacial |
title_fullStr |
Enhanced climate instability in the North Atlantic and southern Europe during the Last Interglacial |
title_full_unstemmed |
Enhanced climate instability in the North Atlantic and southern Europe during the Last Interglacial |
title_sort |
enhanced climate instability in the north atlantic and southern europe during the last interglacial |
publisher |
Springer Nature |
publishDate |
2018 |
url |
http://eprints.esc.cam.ac.uk/4349/ http://eprints.esc.cam.ac.uk/4349/1/s41467-018-06683-3.pdf http://eprints.esc.cam.ac.uk/4349/2/41467_2018_6683_MOESM1_ESM.pdf http://eprints.esc.cam.ac.uk/4349/3/41467_2018_6683_MOESM2_ESM.pdf http://eprints.esc.cam.ac.uk/4349/4/41467_2018_6683_MOESM3_ESM.xlsx http://eprints.esc.cam.ac.uk/4349/5/41467_2018_6683_MOESM4_ESM.xlsx http://eprints.esc.cam.ac.uk/4349/6/41467_2018_6683_MOESM5_ESM.xlsx http://eprints.esc.cam.ac.uk/4349/7/41467_2018_6683_MOESM6_ESM.xlsx https://doi.org/10.1038/s41467-018-06683-3 |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Greenland North Atlantic |
genre_facet |
Greenland North Atlantic |
op_relation |
http://eprints.esc.cam.ac.uk/4349/1/s41467-018-06683-3.pdf http://eprints.esc.cam.ac.uk/4349/2/41467_2018_6683_MOESM1_ESM.pdf http://eprints.esc.cam.ac.uk/4349/3/41467_2018_6683_MOESM2_ESM.pdf http://eprints.esc.cam.ac.uk/4349/4/41467_2018_6683_MOESM3_ESM.xlsx http://eprints.esc.cam.ac.uk/4349/5/41467_2018_6683_MOESM4_ESM.xlsx http://eprints.esc.cam.ac.uk/4349/6/41467_2018_6683_MOESM5_ESM.xlsx http://eprints.esc.cam.ac.uk/4349/7/41467_2018_6683_MOESM6_ESM.xlsx Tzedakis, P. C. and Drysdale, R. N. and Margari, V. and Skinner, L. C. and Menviel, L. and Rhodes, R. H. and Taschetto, A. S. and Hodell, D. A. and Crowhurst, S. J. and Hellstrom, J. C. and Fallick, A. E. and Grimalt, J. O. and McManus, J. F. and Martrat, B. and Mokeddem, Z. and Parrenin, F. and Regattieri, E. and Roe, K. and Zanchetta, G. (2018) Enhanced climate instability in the North Atlantic and southern Europe during the Last Interglacial. Nature Communications, 9 (4235). ISSN 2041-1723 DOI https://doi.org/10.1038/s41467-018-06683-3 <https://doi.org/10.1038/s41467-018-06683-3> |
op_doi |
https://doi.org/10.1038/s41467-018-06683-3 |
container_title |
Nature Communications |
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9 |
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