Articles | Volume 6, issue 2
https://doi.org/10.5194/gchron-6-291-2024
https://doi.org/10.5194/gchron-6-291-2024
Research article
 | 
01 Jul 2024
Research article |  | 01 Jul 2024

Last ice sheet recession and landscape emergence above sea level in east-central Sweden, evaluated using in situ cosmogenic 14C from quartz

Bradley W. Goodfellow, Arjen P. Stroeven, Nathaniel A. Lifton, Jakob Heyman, Alexander Lewerentz, Kristina Hippe, Jens-Ove Näslund, and Marc W. Caffee

Viewed

Total article views: 967 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
705 202 60 967 76 27 41
  • HTML: 705
  • PDF: 202
  • XML: 60
  • Total: 967
  • Supplement: 76
  • BibTeX: 27
  • EndNote: 41
Views and downloads (calculated since 07 Dec 2023)
Cumulative views and downloads (calculated since 07 Dec 2023)

Viewed (geographical distribution)

Total article views: 967 (including HTML, PDF, and XML) Thereof 920 with geography defined and 47 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 13 Dec 2024
Download
Short summary
Carbon-14 produced in quartz (half-life of 5700 ± 30 years) provides a new tool to date exposure of bedrock surfaces. Samples from 10 exposed bedrock surfaces in east-central Sweden give dates consistent with the timing of both landscape emergence above sea level through postglacial rebound and retreat of the last ice sheet shown in previous reconstructions. Carbon-14 in quartz can therefore be used for dating in landscapes where isotopes with longer half-lives give complex exposure results.