The 8200 year B.P. event in the slope water system, western subpolar North Atlantic
[1] Stable isotope, trace metal, alkenone paleothermometry, and radiocarbon methods have been applied to sediment cores in the western subpolar North Atlantic between Hudson Strait and Cape Hatteras to reveal the history of climate in that region over the past 11 kyr. We focus on cores from the Laur...
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Format: | Text |
Language: | English |
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Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.174.1570 http://boyle.mit.edu/%7Eed/PDFs/Keigwin%282005%29Paleoc20.pdf |