Articles | Volume 16, issue 2
Biogeosciences, 16, 643–661, 2019
https://doi.org/10.5194/bg-16-643-2019
Biogeosciences, 16, 643–661, 2019
https://doi.org/10.5194/bg-16-643-2019

Research article 01 Feb 2019

Research article | 01 Feb 2019

Oxygen isotope composition of the final chamber of planktic foraminifera provides evidence of vertical migration and depth-integrated growth

Hilde Pracht et al.

Viewed

Total article views: 1,997 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,207 764 26 1,997 19 30
  • HTML: 1,207
  • PDF: 764
  • XML: 26
  • Total: 1,997
  • BibTeX: 19
  • EndNote: 30
Views and downloads (calculated since 18 Apr 2018)
Cumulative views and downloads (calculated since 18 Apr 2018)

Viewed (geographical distribution)

Total article views: 1,730 (including HTML, PDF, and XML) Thereof 1,698 with geography defined and 32 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Discussed (final revised paper)

Latest update: 25 Jul 2021
Download
Short summary
In palaeoceanography the shells of single-celled foraminifera are routinely used as proxies to reconstruct the temperature, salinity and circulation of the ocean in the past. Traditionally a number of specimens were pooled for a single stable isotope measurement; however, technical advances now mean that a single shell or chamber of a shell can be measured individually. Three different hypotheses regarding foraminiferal biology and ecology were tested using this approach.
Altmetrics
Final-revised paper
Preprint