Articles | Volume 14, issue 4
https://doi.org/10.5194/cp-14-515-2018
https://doi.org/10.5194/cp-14-515-2018
Research article
 | Highlight paper
 | 
20 Apr 2018
Research article | Highlight paper |  | 20 Apr 2018

Moving beyond the age–depth model paradigm in deep-sea palaeoclimate archives: dual radiocarbon and stable isotope analysis on single foraminifera

Bryan C. Lougheed, Brett Metcalfe, Ulysses S. Ninnemann, and Lukas Wacker

Viewed

Total article views: 8,391 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
6,154 2,002 235 8,391 373 226 275
  • HTML: 6,154
  • PDF: 2,002
  • XML: 235
  • Total: 8,391
  • Supplement: 373
  • BibTeX: 226
  • EndNote: 275
Views and downloads (calculated since 29 Sep 2017)
Cumulative views and downloads (calculated since 29 Sep 2017)

Viewed (geographical distribution)

Total article views: 8,391 (including HTML, PDF, and XML) Thereof 7,865 with geography defined and 526 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Saved (final revised paper)

Latest update: 06 May 2026
Download
Short summary
Palaeoclimate reconstructions from deep-sea sediment archives provide valuable insight into past rapid climate change, but only a small proportion of the ocean is suitable for such reconstructions using the existing state of the art, i.e. the age–depth approach. We use dual radiocarbon (14C) and stable isotope analysis on single foraminifera to bypass the long-standing age–depth approach, thus facilitating past ocean chemistry reconstructions from vast, previously untapped ocean areas.
Share