Articles | Volume 18, issue 1
Clim. Past, 18, 167–181, 2022
https://doi.org/10.5194/cp-18-167-2022
Clim. Past, 18, 167–181, 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 et al.

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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 cp-2021-86', Anonymous Referee #1, 23 Aug 2021
    • AC1: 'Reply on RC1', Sophie Warken, 02 Nov 2021
  • RC2: 'Comment on cp-2021-86', Anonymous Referee #2, 05 Sep 2021
    • AC2: 'Reply on RC2', Sophie Warken, 02 Nov 2021

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Publish subject to minor revisions (review by editor) (15 Dec 2021) by Dominik Fleitmann
AR by Sophie Warken on behalf of the Authors (15 Dec 2021)  Author's response    Author's tracked changes    Manuscript
ED: Publish as is (04 Jan 2022) by Dominik Fleitmann
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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.