Articles | Volume 11, issue 6
https://doi.org/10.5194/cp-11-905-2015
https://doi.org/10.5194/cp-11-905-2015
Technical note
 | Highlight paper
 | 
17 Jun 2015
Technical note | Highlight paper |  | 17 Jun 2015

Technical Note: How accurate can stalagmite formation temperatures be determined using vapour bubble radius measurements in fluid inclusions?

F. Spadin, D. Marti, R. Hidalgo-Staub, J. Rička, D. Fleitmann, and M. Frenz

Viewed

Total article views: 7,555 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
4,266 2,050 1,239 7,555 205 188
  • HTML: 4,266
  • PDF: 2,050
  • XML: 1,239
  • Total: 7,555
  • BibTeX: 205
  • EndNote: 188
Views and downloads (calculated since 09 Sep 2014)
Cumulative views and downloads (calculated since 09 Sep 2014)

Cited

Saved (final revised paper)

Saved (final revised paper)

Saved (preprint)

Latest update: 15 Nov 2024
Download
Short summary
Fluid inclusions inside stalagmites retain information on the cave temperature at the time they formed and thus can be used to reconstruct the continental climate of the past. A method for extracting this information based on a thermodynamic model and size measurements of femtosecond-laser-induced vapour bubbles is presented. Applying our method to stalagmites taken from the Milandre cave in the Swiss Jura Mountains demonstrate that palaeotemperatures can be determined with an accuracy of ±1°C.