Freshwater input and abrupt deglacial climate change in the North Atlantic
Greenland ice core records indicate that the last deglaciation (∼7–21 ka) was punctuated by numerous abrupt climate reversals involving temperature changes of up to 5°C–10°C within decades. However, the cause behind many of these events is uncertain. A likely candidate may have been the input of deg...
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ftucl:oai:eprints.ucl.ac.uk.OAI2:1396379 2023-12-24T10:17:14+01:00 Freshwater input and abrupt deglacial climate change in the North Atlantic Thornalley, DJR McCave, IN Elderfield, H 2010-03 text https://discovery.ucl.ac.uk/id/eprint/1396379/1/Thornalley_et_al-2010-Paleoceanography.pdf https://discovery.ucl.ac.uk/id/eprint/1396379/ eng eng https://discovery.ucl.ac.uk/id/eprint/1396379/1/Thornalley_et_al-2010-Paleoceanography.pdf https://discovery.ucl.ac.uk/id/eprint/1396379/ open Paleoceanography , 25 (1) , Article PA1201. (2010) Article 2010 ftucl 2023-11-27T13:07:38Z Greenland ice core records indicate that the last deglaciation (∼7–21 ka) was punctuated by numerous abrupt climate reversals involving temperature changes of up to 5°C–10°C within decades. However, the cause behind many of these events is uncertain. A likely candidate may have been the input of deglacial meltwater, from the Laurentide ice sheet (LIS), to the high-latitude North Atlantic, which disrupted ocean circulation and triggered cooling. Yet the direct evidence of meltwater input for many of these events has so far remained undetected. In this study, we use the geochemistry (paired Mg/Ca-δ18O) of planktonic foraminifera from a sediment core south of Iceland to reconstruct the input of freshwater to the northern North Atlantic during abrupt deglacial climate change. Our record can be placed on the same timescale as ice cores and therefore provides a direct comparison between the timing of freshwater input and climate variability. Meltwater events coincide with the onset of numerous cold intervals, including the Older Dryas (14.0 ka), two events during the Allerød (at ∼13.1 and 13.6 ka), the Younger Dryas (12.9 ka), and the 8.2 ka event, supporting a causal link between these abrupt climate changes and meltwater input. During the Bølling-Allerød warm interval, we find that periods of warming are associated with an increased meltwater flux to the northern North Atlantic, which in turn induces abrupt cooling, a cessation in meltwater input, and eventual climate recovery. This implies that feedback between climate and meltwater input produced a highly variable climate. A comparison to published data sets suggests that this feedback likely included fluctuations in the southern margin of the LIS causing rerouting of LIS meltwater between southern and eastern drainage outlets, as proposed by Clark et al. (2001). Article in Journal/Newspaper Greenland Greenland ice core ice core Ice Sheet Iceland North Atlantic Planktonic foraminifera University College London: UCL Discovery Greenland |
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University College London: UCL Discovery |
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language |
English |
description |
Greenland ice core records indicate that the last deglaciation (∼7–21 ka) was punctuated by numerous abrupt climate reversals involving temperature changes of up to 5°C–10°C within decades. However, the cause behind many of these events is uncertain. A likely candidate may have been the input of deglacial meltwater, from the Laurentide ice sheet (LIS), to the high-latitude North Atlantic, which disrupted ocean circulation and triggered cooling. Yet the direct evidence of meltwater input for many of these events has so far remained undetected. In this study, we use the geochemistry (paired Mg/Ca-δ18O) of planktonic foraminifera from a sediment core south of Iceland to reconstruct the input of freshwater to the northern North Atlantic during abrupt deglacial climate change. Our record can be placed on the same timescale as ice cores and therefore provides a direct comparison between the timing of freshwater input and climate variability. Meltwater events coincide with the onset of numerous cold intervals, including the Older Dryas (14.0 ka), two events during the Allerød (at ∼13.1 and 13.6 ka), the Younger Dryas (12.9 ka), and the 8.2 ka event, supporting a causal link between these abrupt climate changes and meltwater input. During the Bølling-Allerød warm interval, we find that periods of warming are associated with an increased meltwater flux to the northern North Atlantic, which in turn induces abrupt cooling, a cessation in meltwater input, and eventual climate recovery. This implies that feedback between climate and meltwater input produced a highly variable climate. A comparison to published data sets suggests that this feedback likely included fluctuations in the southern margin of the LIS causing rerouting of LIS meltwater between southern and eastern drainage outlets, as proposed by Clark et al. (2001). |
format |
Article in Journal/Newspaper |
author |
Thornalley, DJR McCave, IN Elderfield, H |
spellingShingle |
Thornalley, DJR McCave, IN Elderfield, H Freshwater input and abrupt deglacial climate change in the North Atlantic |
author_facet |
Thornalley, DJR McCave, IN Elderfield, H |
author_sort |
Thornalley, DJR |
title |
Freshwater input and abrupt deglacial climate change in the North Atlantic |
title_short |
Freshwater input and abrupt deglacial climate change in the North Atlantic |
title_full |
Freshwater input and abrupt deglacial climate change in the North Atlantic |
title_fullStr |
Freshwater input and abrupt deglacial climate change in the North Atlantic |
title_full_unstemmed |
Freshwater input and abrupt deglacial climate change in the North Atlantic |
title_sort |
freshwater input and abrupt deglacial climate change in the north atlantic |
publishDate |
2010 |
url |
https://discovery.ucl.ac.uk/id/eprint/1396379/1/Thornalley_et_al-2010-Paleoceanography.pdf https://discovery.ucl.ac.uk/id/eprint/1396379/ |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Greenland Greenland ice core ice core Ice Sheet Iceland North Atlantic Planktonic foraminifera |
genre_facet |
Greenland Greenland ice core ice core Ice Sheet Iceland North Atlantic Planktonic foraminifera |
op_source |
Paleoceanography , 25 (1) , Article PA1201. (2010) |
op_relation |
https://discovery.ucl.ac.uk/id/eprint/1396379/1/Thornalley_et_al-2010-Paleoceanography.pdf https://discovery.ucl.ac.uk/id/eprint/1396379/ |
op_rights |
open |
_version_ |
1786205224283668480 |