Articles | Volume 20, issue 4
https://doi.org/10.5194/cp-20-817-2024
https://doi.org/10.5194/cp-20-817-2024
Research article
 | 
08 Apr 2024
Research article |  | 08 Apr 2024

Holocene environmental and climate evolution of central west Patagonia as reconstructed from lacustrine sediments of Meseta Chile Chico (46.5° S, Chile)

Carolina Franco, Antonio Maldonado, Christian Ohlendorf, A. Catalina Gebhardt, María Eugenia de Porras, Amalia Nuevo-Delaunay, César Méndez, and Bernd Zolitschka

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2023-2156', Anonymous Referee #1, 27 Oct 2023
  • RC2: 'Comment on egusphere-2023-2156', Anonymous Referee #2, 14 Nov 2023

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
ED: Publish subject to minor revisions (review by editor) (04 Jan 2024) by Julie Loisel
AR by Carolina Franco Mora on behalf of the Authors (24 Jan 2024)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (05 Feb 2024) by Julie Loisel
AR by Carolina Franco Mora on behalf of the Authors (10 Feb 2024)  Manuscript 
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Short summary
We present a continuous record of lake sediments spanning the Holocene from central west Patagonia. By examining various indicators like elemental composition and grain size data, we found that, around ~5500 years ago, the way sediments settled in the lake changed. On a regional scale, our results suggest that rainfall, influenced by changes in the Southern Hemisphere Westerly Winds, played a key role in shaping the environment of the region for the past ~10 000 years.