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|a Deglacial Meltwater Pulse 1B and Younger Dyas Sea Levels Revisited with Boreholes at Tahiti |h [electronic resource]. |
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|a [S.l.] : |b American Association for the Advancement of Science, |c 2010. |
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|a Science Magazine Volume 327 Issue 1235. |
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|a Please contact the owning institution for licensing and permissions. It is the user's responsibility to ensure use does not violate any third party rights. |
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|a Reconstructing sea-level changes during the last deglaciation provides a way of understanding the ice dynamics that can perturb large continental ice sheets. The resolution of the few sea-level records covering the critical time interval between 14,000 and 9,000 calendar years before the present is still insufficient to draw conclusions about sea-level changes associated with the Younger Dryas cold event and the meltwater pulse 1B (MWP-1B). We used the uranium-thorium method to date shallow-living corals from three new cores drilled onshore in the Tahiti barrier reef. No significant discontinuity can be detected in the sea-level rise during the MWP-1B period. The new Tahiti sea-level record shows that the sea-level rise slowed down during the Younger Dryas before accelerating again during the Holocene. |
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|a Electronic reproduction. |c Florida International University, |d 2015. |f (dpSobek) |n Mode of access: World Wide Web. |n System requirements: Internet connectivity; Web browser software. |
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|a Delanghe-Sabatier, Doriane. |
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|t Deglacial Meltwater Pulse 1B and Younger Dyas Sea Levels Revisited with Boreholes at Tahiti |
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|a dpSobek |c Sea Level Rise |
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|u http://dpanther.fiu.edu/dpService/dpPurlService/purl/FI15062042/00001 |y Click here for full text |
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|3 Host material |u http://www.sciencemag.org/content/327/5970/1235 |y Deglacial Meltwater Pulse 1B and Younger Dyas Sea Levels Revisited with Boreholes at Tahiti |
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|a http://dpanther.fiu.edu/sobek/content/FI/15/06/20/42/00001/FI15062042thm.jpg |
