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Penultimate deglacial sea-level timing from uranium/thorium dating of Tahitian corals
Thomas, A.L.; Henderson, G.M.; Deschamps, P.; Yokoyama, Y. (2009). Penultimate deglacial sea-level timing from uranium/thorium dating of Tahitian corals. Science (Wash.) 324(5931): 1186-1189. https://hdl.handle.net/10.1126/science.1168754
In: Science (Washington). American Association for the Advancement of Science: New York, N.Y. ISSN 0036-8075, more
Peer reviewed article  

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Keyword
    Marine

Authors  Top 
  • Thomas, A.L.
  • Henderson, G.M.
  • Deschamps, P.
  • Yokoyama, Y.

Abstract
    The timing of sea-level change provides important constraints on the mechanisms driving Earth's climate between glacial and interglacial states. Fossil corals constrain the timing of past sea level by their suitability for dating and their growth position close to sea level. The coral-derived age for the last deglaciation is consistent with climate change forced by Northern Hemisphere summer insolation (NHI), but the timing of the penultimate deglaciation is more controversial. We found, by means of uranium/thorium dating of fossil corals, that sea level during the penultimate deglaciation had risen to similar to 85 meters below the present sea level by 137,000 years ago, and that it fluctuated on a millennial time scale during deglaciation. This indicates that the penultimate deglaciation occurred earlier with respect to NHI than the last deglacial, beginning when NHI was at a minimum.

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