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

Viewed

Total article views: 1,028 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
748 226 54 1,028 26 35 37
  • HTML: 748
  • PDF: 226
  • XML: 54
  • Total: 1,028
  • Supplement: 26
  • BibTeX: 35
  • EndNote: 37
Views and downloads (calculated since 25 Sep 2023)
Cumulative views and downloads (calculated since 25 Sep 2023)

Viewed (geographical distribution)

Total article views: 1,028 (including HTML, PDF, and XML) Thereof 985 with geography defined and 43 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 29 Jun 2024
Download
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.