Articles | Volume 14, issue 3
https://doi.org/10.5194/cp-14-397-2018
https://doi.org/10.5194/cp-14-397-2018
Research article
 | 
23 Mar 2018
Research article |  | 23 Mar 2018

Land–sea coupling of early Pleistocene glacial cycles in the southern North Sea exhibit dominant Northern Hemisphere forcing

Timme H. Donders, Niels A. G. M. van Helmond, Roel Verreussel, Dirk Munsterman, Johan ten Veen, Robert P. Speijer, Johan W. H. Weijers, Francesca Sangiorgi, Francien Peterse, Gert-Jan Reichart, Jaap S. Sinninghe Damsté, Lucas Lourens, Gesa Kuhlmann, and Henk Brinkhuis

Viewed

Total article views: 4,413 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
2,895 1,355 163 4,413 355 109 139
  • HTML: 2,895
  • PDF: 1,355
  • XML: 163
  • Total: 4,413
  • Supplement: 355
  • BibTeX: 109
  • EndNote: 139
Views and downloads (calculated since 20 Sep 2017)
Cumulative views and downloads (calculated since 20 Sep 2017)

Viewed (geographical distribution)

Total article views: 4,413 (including HTML, PDF, and XML) Thereof 4,167 with geography defined and 246 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 14 Dec 2024
Download
Short summary
The buildup and melting of ice during the early glaciations in the Northern Hemisphere, around 2.5 million years ago, were far shorter in duration than during the last million years. Based on molecular compounds and microfossils from sediments dating back to the early glaciations we show that the temperature on land and in the sea changed simultaneously and was a major factor in the ice buildup in the Northern Hemisphere. These data provide key insights into the dynamics of early glaciations.