Articles | Volume 16, issue 1
https://doi.org/10.5194/cp-16-141-2020
https://doi.org/10.5194/cp-16-141-2020
Research article
 | 
16 Jan 2020
Research article |  | 16 Jan 2020

Reconstructing seasonality through stable-isotope and trace-element analyses of the Proserpine stalagmite, Han-sur-Lesse cave, Belgium: indications for climate-driven changes during the last 400 years

Stef Vansteenberge, Niels J. de Winter, Matthias Sinnesael, Sophie Verheyden, Steven Goderis, Stijn J. M. Van Malderen, Frank Vanhaecke, and Philippe Claeys

Viewed

Total article views: 4,352 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
3,089 1,179 84 4,352 231 102 103
  • HTML: 3,089
  • PDF: 1,179
  • XML: 84
  • Total: 4,352
  • Supplement: 231
  • BibTeX: 102
  • EndNote: 103
Views and downloads (calculated since 11 Jul 2019)
Cumulative views and downloads (calculated since 11 Jul 2019)

Viewed (geographical distribution)

Total article views: 4,352 (including HTML, PDF, and XML) Thereof 3,747 with geography defined and 605 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 20 Nov 2024
Download
Short summary
We measured the chemical composition (trace-element concentrations and stable-isotope ratios) of a Belgian speleothem that deposited annual layers. Our sub-annual resolution dataset allows us to investigate how the chemistry of this speleothem recorded changes in the environment and climate in northwestern Europe. We then use this information to reconstruct climate change during the 16th and 17th century on the seasonal scale and demonstrate that environmental change drives speleothem chemistry.