silica rich waters from the
[1] Models indicate that a complete shutdown of deep and intermediate water production is a possible consequence of extreme climate conditions in the northern North Atlantic, and the high ratio of 231Pa to 230Th on Bermuda Rise is evidence that this might have happened 17 ka during Heinrich event 1...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.537.2388 2023-05-15T17:29:08+02:00 silica rich waters from the Lloyd D. Keigwin Edward A. Boyle The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.537.2388 http://boyle.mit.edu/~ed/PDFs/Keigwin(2008)Paleoc23.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.537.2388 http://boyle.mit.edu/~ed/PDFs/Keigwin(2008)Paleoc23.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://boyle.mit.edu/~ed/PDFs/Keigwin(2008)Paleoc23.pdf PA1101 doi 10.1029/2007PA001500 text ftciteseerx 2016-01-08T10:52:11Z [1] Models indicate that a complete shutdown of deep and intermediate water production is a possible consequence of extreme climate conditions in the northern North Atlantic, and the high ratio of 231Pa to 230Th on Bermuda Rise is evidence that this might have happened 17 ka during Heinrich event 1 (H1). However, new radiocarbon data from bivalves that lived at 4.6 km on the Bermuda Rise during H1 lead to a different conclusion. The bivalve data do indeed indicate ventilation of the deep western North Atlantic was suppressed during H1 but not as much as it was during the last glacial maximum. We propose that high diatom flux to the Bermuda Rise during H1 is at least in part responsible for increased 231Pa/230Th at that time. Although we cannot say for sure why opal production was so high in a gyre center location at that time, increased leakage of Text North Atlantic Unknown |
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Open Polar |
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English |
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PA1101 doi 10.1029/2007PA001500 |
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PA1101 doi 10.1029/2007PA001500 Lloyd D. Keigwin Edward A. Boyle silica rich waters from the |
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PA1101 doi 10.1029/2007PA001500 |
description |
[1] Models indicate that a complete shutdown of deep and intermediate water production is a possible consequence of extreme climate conditions in the northern North Atlantic, and the high ratio of 231Pa to 230Th on Bermuda Rise is evidence that this might have happened 17 ka during Heinrich event 1 (H1). However, new radiocarbon data from bivalves that lived at 4.6 km on the Bermuda Rise during H1 lead to a different conclusion. The bivalve data do indeed indicate ventilation of the deep western North Atlantic was suppressed during H1 but not as much as it was during the last glacial maximum. We propose that high diatom flux to the Bermuda Rise during H1 is at least in part responsible for increased 231Pa/230Th at that time. Although we cannot say for sure why opal production was so high in a gyre center location at that time, increased leakage of |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Lloyd D. Keigwin Edward A. Boyle |
author_facet |
Lloyd D. Keigwin Edward A. Boyle |
author_sort |
Lloyd D. Keigwin |
title |
silica rich waters from the |
title_short |
silica rich waters from the |
title_full |
silica rich waters from the |
title_fullStr |
silica rich waters from the |
title_full_unstemmed |
silica rich waters from the |
title_sort |
silica rich waters from the |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.537.2388 http://boyle.mit.edu/~ed/PDFs/Keigwin(2008)Paleoc23.pdf |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
http://boyle.mit.edu/~ed/PDFs/Keigwin(2008)Paleoc23.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.537.2388 http://boyle.mit.edu/~ed/PDFs/Keigwin(2008)Paleoc23.pdf |
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Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766122750684954624 |