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|a A 17,000-year glacio-eustatic sea level record |h [electronic resource] |b influence of glacial melting rates on the Younger Dryas event and deep-ocean circulation |y English. |
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|a [S.l.] : |b Nature Publishing Group, |c 1989. |
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|a Nature Magazine Volume 342. |
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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 Coral reefs drilled offshore of Barbados provide the first continuous and detailed record of sea level change during the last deglaciation. The sea level was 121 ± 5 metres below present level during the last glacial maximum. The deglacial sea level rise was not monotonic; rather, it was marked by two intervals of rapid rise. Varying rates of melt-water discharge to the North Atlantic surface ocean dramatically affected North Atlantic deep-water production and oceanic oxygen isotope chemistry. A global oxygen isotope record for ocean water has been calculated from the Barbados sea level curve, allowing separation of the ice volume component common to all oxygen isotope records measured in deep-sea cores. |
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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 Coral reefs and islands. |
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|a Fairbanks, Richard G.. |
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|t A 17,000-year glacio-eustatic sea level record |
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|a dpSobek |c Sea Level Rise |
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|u http://dpanther.fiu.edu/dpService/dpPurlService/purl/FI15061979/00001 |y Click here for full text |
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|3 FULL TEXT |u http://www.nature.com/nature/journal/v342/n6250/pdf/342637a0.pdf |y A 17,000-year glacio-eustatic sea level record |
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|a http://dpanther.fiu.edu/sobek/content/FI/15/06/19/79/00001/FI15061979_thm.jpg |
