The synchronization of palaeoclimatic events in the North Atlantic region during Greenland Stadial 3 (ca 27.5 to 23.3 kyr b2k)

Two high resolution marine sediment cores located 83 km apart in the NE Atlantic have been studied: MD95-2006 (Barra Fan; 57 degrees 01.82 N. 10 degrees 03.48 W; 2120 m water depth) and MD04-2822 (Rockall Trough; 56 degrees 50.54 N, 11 degrees 22.96 W; 2344 m water depth). The records are anchored t...

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Bibliographic Details
Published in:Quaternary Science Reviews
Main Authors: Austin, W. E. N., Hibbert, F. D., Rasmussen, S. O., Peters, C., Abbott, P. M., Bryant, C. L.
Format: Article in Journal/Newspaper
Language:English
Published: 2012
Subjects:
Online Access:https://research-portal.st-andrews.ac.uk/en/researchoutput/the-synchronization-of-palaeoclimatic-events-in-the-north-atlantic-region-during-greenland-stadial-3-ca-275-to-233-kyr-b2k(1071c871-a0e6-43e4-80ed-578875b695a6).html
https://doi.org/10.1016/j.quascirev.2010.12.014