Articles | Volume 13, issue 9
https://doi.org/10.5194/cp-13-1097-2017
https://doi.org/10.5194/cp-13-1097-2017
Research article
 | 
05 Sep 2017
Research article |  | 05 Sep 2017

Deglacial sea level history of the East Siberian Sea and Chukchi Sea margins

Thomas M. Cronin, Matt O'Regan, Christof Pearce, Laura Gemery, Michael Toomey, Igor Semiletov, and Martin Jakobsson

Viewed

Total article views: 5,497 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
3,125 2,127 245 5,497 482 172 216
  • HTML: 3,125
  • PDF: 2,127
  • XML: 245
  • Total: 5,497
  • Supplement: 482
  • BibTeX: 172
  • EndNote: 216
Views and downloads (calculated since 29 Mar 2017)
Cumulative views and downloads (calculated since 29 Mar 2017)

Viewed (geographical distribution)

Total article views: 5,497 (including HTML, PDF, and XML) Thereof 5,192 with geography defined and 305 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 14 Dec 2024
Download
Short summary
Global sea level rise during the last deglacial flooded the Siberian continental shelf in the Arctic Ocean. Sediment cores, radiocarbon dating, and microfossils show that the regional sea level in the Arctic rose rapidly from about 12 500 to 10 700 years ago. Regional sea level history on the Siberian shelf differs from the global deglacial sea level rise perhaps due to regional vertical adjustment resulting from the growth and decay of ice sheets.