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• W129569514 abstract "The last deglaciation was characterized by a rapid sea-level rise and coeval abrupt environmental changes.The Integrated Ocean Drilling Program Expeditions 310 “Tahiti Sea Level” and 325 “Great Barrier Reef Environmental Changes” aimed to provide the most comprehensive last deglacial sea-level and climatic records by conducting offshore drilling of fossil coral reefs now preserved at 40–130 m below present sea level. These expeditions have provided unparalleled reef records of the last and penultimate deglaciations and brought a wealth of new information in various scientific fields.They have demonstrated the pivotal importance of coral reef records to reconstruct the amplitude and timing of sea-level rise caused by the melting of land ice after the Last Glacial Maximum ∼23,000 years ago. In particular, short periods of dramatic sea-level rise indicating varying rates of melting imply the presence of thresholds within the dynamic behavior of ice sheets and provide a challenging test for ice sheet models used to predict future sea-level rise. The sea-level jump during meltwater pulse 1A, newly constrained by Expedition 310 with a magnitude of 16 ± 2 m in ∼350 years (14.6–14.3 ka), induced the retrogradation of shallow-water coral assemblages, gradual deepening, and incipient reef drowning. Reefs accreted continuously between 16 and 10 ka, mostly through aggradational processes, at growth rates averaging 10 mm/year. No cessation of reef growth, even temporary, was observed during this period at Tahiti. Post-cruise analyses are still in progress but initial results confirm that Expedition 325 will extend this record of sea level, environmental changes, and reef response in the South Pacific back to ∼30,000 years ago. Drilling of multiple sites around the globe, spanning several glacial–interglacial transitions, is needed to better constrain the timing and amplitude of sea-level change that resulted in the disintegration of large ice sheets, and to evaluate the response of ocean meridional overturning circulation to freshwater inputs." @default.
• W129569514 created "2016-06-24" @default.
• W129569514 creator A5013326071 @default.
• W129569514 creator A5059292421 @default.
• W129569514 date "2014-01-01" @default.
• W129569514 modified "2023-09-25" @default.
• W129569514 title "Coral Reefs and Sea-Level Change" @default.
• W129569514 cites W1227740874 @default.
• W129569514 cites W1489903658 @default.
• W129569514 cites W1500438875 @default.
• W129569514 cites W1511524149 @default.
• W129569514 cites W1528217364 @default.
• W129569514 cites W1569546865 @default.
• W129569514 cites W1603555063 @default.
• W129569514 cites W1663212967 @default.
• W129569514 cites W1677857930 @default.
• W129569514 cites W1870218624 @default.
• W129569514 cites W1893802248 @default.
• W129569514 cites W1915797674 @default.
• W129569514 cites W1943336573 @default.
• W129569514 cites W1963653848 @default.
• W129569514 cites W1964164599 @default.
• W129569514 cites W1966976771 @default.
• W129569514 cites W1968905104 @default.
• W129569514 cites W1972440568 @default.
• W129569514 cites W1973201527 @default.
• W129569514 cites W1975286425 @default.
• W129569514 cites W1978338754 @default.
• W129569514 cites W1978933468 @default.
• W129569514 cites W1980046754 @default.
• W129569514 cites W1981075441 @default.
• W129569514 cites W1981267808 @default.
• W129569514 cites W1983619939 @default.
• W129569514 cites W1985182243 @default.
• W129569514 cites W1985454049 @default.
• W129569514 cites W1985503063 @default.
• W129569514 cites W1986059175 @default.
• W129569514 cites W1987137619 @default.
• W129569514 cites W1987153756 @default.
• W129569514 cites W1987244610 @default.
• W129569514 cites W1989199095 @default.
• W129569514 cites W1989368656 @default.
• W129569514 cites W1990136463 @default.
• W129569514 cites W1992010123 @default.
• W129569514 cites W1996673305 @default.
• W129569514 cites W1999183744 @default.
• W129569514 cites W2000051334 @default.
• W129569514 cites W2002773274 @default.
• W129569514 cites W2002790717 @default.
• W129569514 cites W2005536752 @default.
• W129569514 cites W2006311299 @default.
• W129569514 cites W2007714064 @default.
• W129569514 cites W2007729714 @default.
• W129569514 cites W2009198894 @default.
• W129569514 cites W2012166732 @default.
• W129569514 cites W2012787657 @default.
• W129569514 cites W2013160730 @default.
• W129569514 cites W2013499862 @default.
• W129569514 cites W2014128187 @default.
• W129569514 cites W2015728521 @default.
• W129569514 cites W2015970155 @default.
• W129569514 cites W2015985850 @default.
• W129569514 cites W2016117158 @default.
• W129569514 cites W2017921774 @default.
• W129569514 cites W2018560310 @default.
• W129569514 cites W2018811644 @default.
• W129569514 cites W2022716702 @default.
• W129569514 cites W2023464499 @default.
• W129569514 cites W2024369723 @default.
• W129569514 cites W2027605790 @default.
• W129569514 cites W2034143948 @default.
• W129569514 cites W2040798879 @default.
• W129569514 cites W2042671618 @default.
• W129569514 cites W2042795871 @default.
• W129569514 cites W2046593598 @default.
• W129569514 cites W2055615694 @default.
• W129569514 cites W2056415813 @default.
• W129569514 cites W2059369040 @default.
• W129569514 cites W2063458827 @default.
• W129569514 cites W2064820367 @default.
• W129569514 cites W2067288914 @default.
• W129569514 cites W2068151576 @default.
• W129569514 cites W2069385803 @default.
• W129569514 cites W2070485016 @default.
• W129569514 cites W2071105325 @default.
• W129569514 cites W2073194484 @default.
• W129569514 cites W2076923852 @default.
• W129569514 cites W2078702313 @default.
• W129569514 cites W2079180189 @default.
• W129569514 cites W2080208946 @default.
• W129569514 cites W2087233175 @default.
• W129569514 cites W2089661799 @default.
• W129569514 cites W2090197982 @default.
• W129569514 cites W2092250359 @default.
• W129569514 cites W2093623870 @default.
• W129569514 cites W2093807014 @default.
• W129569514 cites W2094033454 @default.
• W129569514 cites W2094394939 @default.
• W129569514 cites W2094866962 @default.
• W129569514 cites W2094988303 @default.

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