Articles | Volume 12, issue 6
https://doi.org/10.5194/cp-12-1281-2016
https://doi.org/10.5194/cp-12-1281-2016
Research article
 | 
02 Jun 2016
Research article |  | 02 Jun 2016

Last Glacial Maximum and deglacial abyssal seawater oxygen isotopic ratios

Carl Wunsch

Viewed

Total article views: 2,429 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,394 938 97 2,429 114 120
  • HTML: 1,394
  • PDF: 938
  • XML: 97
  • Total: 2,429
  • BibTeX: 114
  • EndNote: 120
Views and downloads (calculated since 25 Jan 2016)
Cumulative views and downloads (calculated since 25 Jan 2016)

Cited

Latest update: 28 Mar 2024
Download
Short summary
This paper examines the oxygen isotope data in several deep-sea cores. The question addressed is whether those data support an inference that the abyssal ocean in the Last Glacial Maximum period was significantly colder than it is today. Along with a separate analysis of salinity data in the same cores, it is concluded that a cold, saline deep ocean is consistent with the available data but so is an abyss much more like that found today. LGM model testers should beware.