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- W2254383695 abstract "The Younger Dryas climate event occurred during the middle of the last deglacial cycle and is marked by an abrupt shift in the North Atlantic polar front almost to its former glacial position, trending east to west. Using high-precision and high-accuracy U-Th-dated Barbados reef crest coral, Acropora palmata, we generate a detailed sea level record from 13.9 to 9000 years before present (kyr B.P.) and reconstruct the ice volume response to the Younger Dryas cooling. From the mid-Allerod (13.9 kyr B.P.) to the end of the Younger Dryas (11.65 kyr B.P.), rates of sea level rise decreased smoothly from 20 mm yr−1 to 4 mm yr−1, culminating in a 400 year “slow stand” before accelerating into meltwater pulse 1B (MWP-1B). The MWP-1B event at Barbados is better constrained as beginning by 11.45 kyr B.P. and ending at 11.1 kyr B.P. during which time sea level rose 14 ± 2 m and rates of sea level rise reached 40 mm yr−1. We propose that MWP-1B is the direct albeit lagged response of the Northern Hemisphere ice sheets to the rapid warming marking the end of the Younger Dryas coinciding with rapid warming in the circum-North Atlantic region and the polar front shift from its zonal to meridional position 11.65 kyr B.P. As predicted by glaciological models, the ice sheet response to rapid North Atlantic warming was lagged by 400 years due to the thermal inertia of large ice sheets. The regional circum-North Atlantic Younger Dryas climate event is elevated to a global response through sea level changes, starting with the global slowdown in sea level rise during the Younger Dryas and culminating with MWP-1B. No meltwater pulses are evident at the initiation of the Younger Dryas climate event as is often speculated." @default.
- W2254383695 created "2016-06-24" @default.
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- W2254383695 creator A5048215674 @default.
- W2254383695 date "2016-02-01" @default.
- W2254383695 modified "2023-10-12" @default.
- W2254383695 title "Younger Dryas sea level and meltwater pulse 1B recorded in Barbados reef crest coral<i>Acropora palmata</i>" @default.
- W2254383695 cites W1497667361 @default.
- W2254383695 cites W1516822430 @default.
- W2254383695 cites W1545493978 @default.
- W2254383695 cites W1636485319 @default.
- W2254383695 cites W1654234791 @default.
- W2254383695 cites W1663212967 @default.
- W2254383695 cites W1667204707 @default.
- W2254383695 cites W1677857930 @default.
- W2254383695 cites W1882489491 @default.
- W2254383695 cites W1964618265 @default.
- W2254383695 cites W1966216066 @default.
- W2254383695 cites W1966949260 @default.
- W2254383695 cites W1971816180 @default.
- W2254383695 cites W1972104269 @default.
- W2254383695 cites W1973227610 @default.
- W2254383695 cites W1974828561 @default.
- W2254383695 cites W1975697763 @default.
- W2254383695 cites W1975725752 @default.
- W2254383695 cites W1980046754 @default.
- W2254383695 cites W1981267808 @default.
- W2254383695 cites W1981964335 @default.
- W2254383695 cites W1985182243 @default.
- W2254383695 cites W1986192312 @default.
- W2254383695 cites W1987244610 @default.
- W2254383695 cites W1987425355 @default.
- W2254383695 cites W1989673732 @default.
- W2254383695 cites W1990194322 @default.
- W2254383695 cites W1990989473 @default.
- W2254383695 cites W1993479310 @default.
- W2254383695 cites W1996207238 @default.
- W2254383695 cites W1996862213 @default.
- W2254383695 cites W1997290536 @default.
- W2254383695 cites W1999216384 @default.
- W2254383695 cites W2000443539 @default.
- W2254383695 cites W2001072306 @default.
- W2254383695 cites W2002717773 @default.
- W2254383695 cites W2005536752 @default.
- W2254383695 cites W2006099900 @default.
- W2254383695 cites W2006518213 @default.
- W2254383695 cites W2006725392 @default.
- W2254383695 cites W2007137128 @default.
- W2254383695 cites W2007217700 @default.
- W2254383695 cites W2008875043 @default.
- W2254383695 cites W2011654501 @default.
- W2254383695 cites W2012782576 @default.
- W2254383695 cites W2012787657 @default.
- W2254383695 cites W2013430677 @default.
- W2254383695 cites W2013878295 @default.
- W2254383695 cites W2017494658 @default.
- W2254383695 cites W2018560310 @default.
- W2254383695 cites W2018811644 @default.
- W2254383695 cites W2019112800 @default.
- W2254383695 cites W2022545034 @default.
- W2254383695 cites W2022716702 @default.
- W2254383695 cites W2024369723 @default.
- W2254383695 cites W2027949041 @default.
- W2254383695 cites W2032191739 @default.
- W2254383695 cites W2033994827 @default.
- W2254383695 cites W2035587516 @default.
- W2254383695 cites W2036265699 @default.
- W2254383695 cites W2037409667 @default.
- W2254383695 cites W2038049971 @default.
- W2254383695 cites W2040611564 @default.
- W2254383695 cites W2040967573 @default.
- W2254383695 cites W2041414130 @default.
- W2254383695 cites W2041963168 @default.
- W2254383695 cites W2046806827 @default.
- W2254383695 cites W2047203508 @default.
- W2254383695 cites W2047576107 @default.
- W2254383695 cites W2047577495 @default.
- W2254383695 cites W2051087039 @default.
- W2254383695 cites W2052726929 @default.
- W2254383695 cites W2054179059 @default.
- W2254383695 cites W2054307300 @default.
- W2254383695 cites W2054521717 @default.
- W2254383695 cites W2054892272 @default.
- W2254383695 cites W2056428803 @default.
- W2254383695 cites W2056588603 @default.
- W2254383695 cites W2056724834 @default.
- W2254383695 cites W2057015339 @default.
- W2254383695 cites W2059369040 @default.
- W2254383695 cites W2059740639 @default.
- W2254383695 cites W2060140623 @default.
- W2254383695 cites W2063926313 @default.
- W2254383695 cites W2064072661 @default.
- W2254383695 cites W2066904459 @default.
- W2254383695 cites W2067150205 @default.
- W2254383695 cites W2068151576 @default.
- W2254383695 cites W2068589879 @default.