Articles | Volume 16, issue 4
https://doi.org/10.5194/cp-16-1245-2020
https://doi.org/10.5194/cp-16-1245-2020
Research article
 | 
16 Jul 2020
Research article |  | 16 Jul 2020

Contrasting late-glacial paleoceanographic evolution between the upper and lower continental slope of the western South Atlantic

Leticia G. Luz, Thiago P. Santos, Timothy I. Eglinton, Daniel Montluçon, Blanca Ausin, Negar Haghipour, Silvia M. Sousa, Renata H. Nagai, and Renato S. Carreira

Download

Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (06 May 2020) by Erin McClymont
AR by Renato Carreira on behalf of the Authors (06 May 2020)  Author's response   Manuscript 
ED: Publish subject to minor revisions (review by editor) (27 May 2020) by Erin McClymont
AR by Renato Carreira on behalf of the Authors (01 Jun 2020)  Author's response   Manuscript 
ED: Publish subject to technical corrections (15 Jun 2020) by Erin McClymont
AR by Renato Carreira on behalf of the Authors (15 Jun 2020)  Author's response   Manuscript 
Download
Short summary
Two sediment cores retrieved from the SE Brazilian continental margin were studied using multiple organic (alkenones) and inorganic (oxygen isotopes in carbonate shells and water) proxies to reconstruct the sea surface temperature (SST) over the last 50 000 years. The findings indicate the formation of strong thermal gradients in the region during the last climate transition, a feature that may become more frequent in the future scenario of global water circulation changes.