Adkins, J. F. and Schrag, D. P. (2001) Pore fluid constraints on deep ocean temperature and salinity during the Last Glacial Maximum. Geophysical Research Letters, 28 (5). pp. 771-774. ISSN 0094-8276. https://resolver.caltech.edu/CaltechAUTHORS:20120828-115449235
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Abstract
Pore water records of δ^(18)O and [Cl] from ODP Site 1063A on the Bermuda Rise constrain the change in seawater δ^(18)O and salinity from the Last Glacial Maximum (LGM) to the Holocene to be 0.75±0.05‰ and 2.5±0.1% respectively. Coupled with a measured benthic foraminiferal δ^(18)O change, this result means that bottom waters were 4.6±0.8°C cooler than the Holocene at the LGM and therefore at or near the seawater freezing point. Coupled δ^(18)O and chlorinity results give an extrapolated mean ocean LGM to Holocene change in δ^(18)O of 0.95±0.09‰. These data also constrain the past southern source deep‐water salinity to be 35.76±0.04 psu, which is within error of the mean deep ocean value for this time.
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| Additional Information: | © 2001 American Geophysical Union. Received 15 March 2000; accepted 17 July 2000. | |||||||||
| Issue or Number: | 5 | |||||||||
| Record Number: | CaltechAUTHORS:20120828-115449235 | |||||||||
| Persistent URL: | https://resolver.caltech.edu/CaltechAUTHORS:20120828-115449235 | |||||||||
| Official Citation: | Adkins, J. F. and D. P. Schrag (2001), Pore fluid constraints on deep ocean temperature and salinity during the Last Glacial Maximum, Geophys. Res. Lett., 28(5), 771–774, doi:10.1029/2000GL011597. | |||||||||
| Usage Policy: | No commercial reproduction, distribution, display or performance rights in this work are provided. | |||||||||
| ID Code: | 33609 | |||||||||
| Collection: | CaltechAUTHORS | |||||||||
| Deposited By: | Aucoeur Ngo | |||||||||
| Deposited On: | 28 Aug 2012 20:52 | |||||||||
| Last Modified: | 24 Feb 2020 10:30 |
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