Articles | Volume 18, issue 10
Research article
14 Oct 2022
Research article |  | 14 Oct 2022

Millennial variability of terrigenous transport to the central–southern Peruvian margin during the last deglaciation (18–13 kyr BP)

Marco Yseki, Bruno Turcq, Sandrine Caquineau, Renato Salvatteci, José Solis, C. Gregory Skilbeck, Federico Velazco, and Dimitri Gutiérrez


Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on cp-2021-183', Anonymous Referee #1, 12 Feb 2022
    • AC1: 'Reply on RC1', Marco Yseki, 02 Jun 2022
  • RC2: 'Comment on cp-2021-183', Anonymous Referee #2, 16 Feb 2022
    • AC2: 'Reply on RC2', Marco Yseki, 02 Jun 2022

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Publish subject to minor revisions (review by editor) (07 Jun 2022) by Claudio Latorre
AR by Marco Yseki on behalf of the Authors (09 Sep 2022)  Author's response    Author's tracked changes    Manuscript
ED: Publish as is (13 Sep 2022) by Claudio Latorre
Short summary
In the present work we reconstruct changes in river discharge and wind in Peru during the last deglaciation to understand the mechanisms that modulate changes in precipitation and winds during a period of global warming. We found that changes in river discharge and wind intensity in Peru were sensitive to high-latitude forcing (changes in the intensity of the Atlantic Meridional Overturning Circulation) and Walker circulation variations on a millennial timescale, respectively.