Articles | Volume 17, issue 3
https://doi.org/10.5194/cp-17-1051-2021
https://doi.org/10.5194/cp-17-1051-2021
Research article
 | 
18 May 2021
Research article |  | 18 May 2021

The speleothem oxygen record as a proxy for thermal or moisture changes: a case study of multiproxy records from MIS 5–MIS 6 speleothems from the Demänová Cave system

Jacek Pawlak

Viewed

Total article views: 1,773 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,193 532 48 1,773 52 46
  • HTML: 1,193
  • PDF: 532
  • XML: 48
  • Total: 1,773
  • BibTeX: 52
  • EndNote: 46
Views and downloads (calculated since 26 Oct 2020)
Cumulative views and downloads (calculated since 26 Oct 2020)

Viewed (geographical distribution)

Total article views: 1,773 (including HTML, PDF, and XML) Thereof 1,649 with geography defined and 124 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 18 Jun 2024
Download
Short summary
Presently, central Europe is under the influence of two types of climate, transitional and continental. The 60 ka long multiproxy speleothem dataset from Slovakia records the climate of the Last Interglacial cycle and its transition to the Last Glacial. The interpretation of stable isotopic composition and trace element content proxies helps to distinguish which factor had the strongest influence on the δ18O record shape: the local temperature, the humidity or the source effect.