Freshwater influx, hydrographic reorganisation and the dispersal of Ice Rafted Detritus in the sub-polar North Atlantic Ocean during the last deglaciation
A sediment core from the north-east North Atlantic contains high-resolution co-registered foraminiferal δ 18 O and ice-rafted detritus (IRD) records for the last deglaciation. These reveal a distinct ice-rafting event that occurred at the time of Greenland Interstade 1d (GI-1d), a feature also seen...
Published in: | Journal of Quaternary Science |
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Main Authors: | , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
2013
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Subjects: | |
Online Access: | https://research-portal.st-andrews.ac.uk/en/publications/a68ce335-ba61-46d0-876f-2e0f7424ce7e https://doi.org/10.1002/jqs.2644 |