Articles | Volume 11, issue 10
https://doi.org/10.5194/cp-11-1297-2015
https://doi.org/10.5194/cp-11-1297-2015
Research article
 | 
06 Oct 2015
Research article |  | 06 Oct 2015

Parallelisms between sea surface temperature changes in the western tropical Atlantic (Guiana Basin) and high latitude climate signals over the last 140 000 years

O. Rama-Corredor, B. Martrat, J. O. Grimalt, G. E. López-Otalvaro, J. A. Flores, and F. Sierro

Viewed

Total article views: 3,269 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,925 1,149 195 3,269 416 168 164
  • HTML: 1,925
  • PDF: 1,149
  • XML: 195
  • Total: 3,269
  • Supplement: 416
  • BibTeX: 168
  • EndNote: 164
Views and downloads (calculated since 02 Apr 2015)
Cumulative views and downloads (calculated since 02 Apr 2015)

Cited

Saved (final revised paper)

Saved (final revised paper)

Latest update: 23 Nov 2024
Download
Short summary
The alkenone sea surface temperatures in the Guiana Basin show a rapid transmission of the climate variability from arctic to tropical latitudes during the last two interglacials (MIS1 and MIS5e) and warm long interstadials (MIS5d-a). In contrast, the abrupt variability of the glacial interval does follow the North Atlantic climate but is also shaped by precessional changes. This arctic to tropical decoupling occurs when the Atlantic meridional overturning circulation is substantially reduced.