Articles | Volume 12, issue 7
https://doi.org/10.5194/cp-12-1445-2016
https://doi.org/10.5194/cp-12-1445-2016
Research article
 | 
05 Jul 2016
Research article |  | 05 Jul 2016

Paleoclimate in continental northwestern Europe during the Eemian and early Weichselian (125–97 ka): insights from a Belgian speleothem

Stef Vansteenberge, Sophie Verheyden, Hai Cheng, R. Lawrence Edwards, Eddy Keppens, and Philippe Claeys

Viewed

Total article views: 3,717 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,879 1,703 135 3,717 146 135
  • HTML: 1,879
  • PDF: 1,703
  • XML: 135
  • Total: 3,717
  • BibTeX: 146
  • EndNote: 135
Views and downloads (calculated since 08 Feb 2016)
Cumulative views and downloads (calculated since 08 Feb 2016)

Cited

Saved (preprint)

Discussed (preprint)

Latest update: 12 Dec 2024
Download
Short summary
The use of stalagmites for last interglacial continental climate reconstructions in Europe has been successful in the past; however to expand the geographical coverage, additional data from Belgium is presented. It has been shown that stalagmite growth, morphology and stable isotope content reflect regional and local climate conditions, with Eemian optimum climate occurring between 125.3 and 117.3 ka. The start the Weichselian is expressed by a stop of growth caused by a drying climate.