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• W2156865657 abstract "Observations of δ13C and Cd/Ca from benthic foraminifera have been interpreted to reflect a shoaling of northern source waters by about 1000 m during the Last Glacial Maximum, with the degree of shoaling being significant enough for the water mass to be renamed Glacial North Atlantic Intermediate Water. These nutrient tracers, however, may not solely reflect changes in water mass distributions. To quantify the distribution of Glacial North Atlantic Water, we perform a glacial water mass decomposition where the sparsity of data, geometrical constraints, and nonconservative tracer effects are taken into account, and the extrapolation for the unknown water mass end-members is guided by the modern-day circulation. Under the assumption that the glacial sources of remineralized material are similar to that of the modern day, we find a steady solution consistent with 241 δ13C, 87 Cd/Ca, and 174 δ18O observations and their respective uncertainties. The water mass decomposition indicates that the core of Glacial North Atlantic Water shoals and southern source water extends in greater quantities into the abyssal North Atlantic, as previously inferred. The depth of the deep northern-southern water mass interface and the volume of North Atlantic Water, however, are not grossly different from that of the modern day. Under this scenario, the vertical structure of glacial δ13C and Cd/Ca is primarily due to the greater accumulation of nutrients in lower North Atlantic Water, which may be a signal of the hoarding of excess carbon from the atmosphere by the glacial Atlantic." @default.
• W2156865657 created "2016-06-24" @default.
• W2156865657 creator A5055887885 @default.
• W2156865657 date "2014-03-01" @default.
• W2156865657 modified "2023-10-16" @default.
• W2156865657 title "How much did Glacial North Atlantic Water shoal?" @default.
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• W2156865657 cites W1493417715 @default.
• W2156865657 cites W1551039347 @default.
• W2156865657 cites W1566711135 @default.
• W2156865657 cites W1598311721 @default.
• W2156865657 cites W1609491364 @default.
• W2156865657 cites W1611443029 @default.
• W2156865657 cites W1613947429 @default.
• W2156865657 cites W1857545922 @default.
• W2156865657 cites W1948647628 @default.
• W2156865657 cites W1964806567 @default.
• W2156865657 cites W1968670244 @default.
• W2156865657 cites W1968860571 @default.
• W2156865657 cites W1968988439 @default.
• W2156865657 cites W1970025133 @default.
• W2156865657 cites W1975461564 @default.
• W2156865657 cites W1975790343 @default.
• W2156865657 cites W1977775988 @default.
• W2156865657 cites W1980512123 @default.
• W2156865657 cites W1980799929 @default.
• W2156865657 cites W1982300900 @default.
• W2156865657 cites W1983017748 @default.
• W2156865657 cites W1989141253 @default.
• W2156865657 cites W1990753866 @default.
• W2156865657 cites W2001072306 @default.
• W2156865657 cites W2002897543 @default.
• W2156865657 cites W2004160802 @default.
• W2156865657 cites W2006631544 @default.
• W2156865657 cites W2007796259 @default.
• W2156865657 cites W2013278565 @default.
• W2156865657 cites W2013996164 @default.
• W2156865657 cites W2018069199 @default.
• W2156865657 cites W2019151728 @default.
• W2156865657 cites W2025799639 @default.
• W2156865657 cites W2028443916 @default.
• W2156865657 cites W2028588371 @default.
• W2156865657 cites W2031630167 @default.
• W2156865657 cites W2032396158 @default.
• W2156865657 cites W2034575670 @default.
• W2156865657 cites W2037847042 @default.
• W2156865657 cites W2041010189 @default.
• W2156865657 cites W2042189564 @default.
• W2156865657 cites W2042476750 @default.
• W2156865657 cites W2045471824 @default.
• W2156865657 cites W2050469687 @default.
• W2156865657 cites W2051226623 @default.
• W2156865657 cites W2054552587 @default.
• W2156865657 cites W2055647265 @default.
• W2156865657 cites W2058718049 @default.
• W2156865657 cites W2067277521 @default.
• W2156865657 cites W2068029317 @default.
• W2156865657 cites W2068120253 @default.
• W2156865657 cites W2070594612 @default.
• W2156865657 cites W2071664164 @default.
• W2156865657 cites W2071846684 @default.
• W2156865657 cites W2073558207 @default.
• W2156865657 cites W2075798101 @default.
• W2156865657 cites W2078192666 @default.
• W2156865657 cites W2078674388 @default.
• W2156865657 cites W2079643039 @default.
• W2156865657 cites W2080665863 @default.
• W2156865657 cites W2088709166 @default.
• W2156865657 cites W2090767277 @default.
• W2156865657 cites W2093142430 @default.
• W2156865657 cites W2093722277 @default.
• W2156865657 cites W2096419447 @default.
• W2156865657 cites W2107372061 @default.
• W2156865657 cites W2109624245 @default.
• W2156865657 cites W2112049438 @default.
• W2156865657 cites W2112428814 @default.
• W2156865657 cites W2118387673 @default.
• W2156865657 cites W2122249284 @default.
• W2156865657 cites W2127150857 @default.
• W2156865657 cites W2135465384 @default.
• W2156865657 cites W2143973246 @default.
• W2156865657 cites W2146762973 @default.
• W2156865657 cites W2147652131 @default.
• W2156865657 cites W2151763413 @default.
• W2156865657 cites W2915433281 @default.
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• W2156865657 doi "https://doi.org/10.1002/2013pa002557" @default.
• W2156865657 hasPublicationYear "2014" @default.
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