Articles | Volume 18, issue 1
https://doi.org/10.5194/cp-18-167-2022
https://doi.org/10.5194/cp-18-167-2022
Research article
 | 
01 Feb 2022
Research article |  | 01 Feb 2022

Last glacial millennial-scale hydro-climate and temperature changes in Puerto Rico constrained by speleothem fluid inclusion δ18O and δ2H values

Sophie F. Warken, Therese Weißbach, Tobias Kluge, Hubert Vonhof, Denis Scholz, Rolf Vieten, Martina Schmidt, Amos Winter, and Norbert Frank

Viewed

Total article views: 2,270 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,648 581 41 2,270 215 23 33
  • HTML: 1,648
  • PDF: 581
  • XML: 41
  • Total: 2,270
  • Supplement: 215
  • BibTeX: 23
  • EndNote: 33
Views and downloads (calculated since 30 Jul 2021)
Cumulative views and downloads (calculated since 30 Jul 2021)

Viewed (geographical distribution)

Total article views: 2,270 (including HTML, PDF, and XML) Thereof 2,087 with geography defined and 183 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 28 Mar 2024
Download
Short summary
The analysis of fluid inclusions from a Puerto Rican speleothem provides quantitative information about past rainfall conditions and temperatures during the Last Glacial Period, when the climate was extremely variable. Our data show that the region experienced a climate that was generally colder and drier. However, we also reconstruct intervals when temperatures reached nearly modern values, and convective activity was comparable to or only slightly weaker than the present day.