Oxygen isotope composition of the final chamber of planktic foraminifera provides evidence of vertical migration and depth-integrated growth
Hilde Pracht,Brett Metcalfe,and Frank J. C. Peeters
Hilde Pracht
Earth and Climate Cluster, Department of Earth Sciences, Faculty of
Sciences, Vrije Universiteit Amsterdam, de Boelelaan 1085, 1081 HV,
Amsterdam, the Netherlands
Earth and Climate Cluster, Department of Earth Sciences, Faculty of
Sciences, Vrije Universiteit Amsterdam, de Boelelaan 1085, 1081 HV,
Amsterdam, the Netherlands
Laboratoire des Sciences du Climat et de l'Environnement, LSCE/IPSL,
CEA-CNRS-UVSQ, Université Paris-Saclay, 91191 Gif-sur-Yvette, France
Earth and Climate Cluster, Department of Earth Sciences, Faculty of
Sciences, Vrije Universiteit Amsterdam, de Boelelaan 1085, 1081 HV,
Amsterdam, the Netherlands
Viewed
Total article views: 3,813 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
2,455
1,290
68
3,813
48
59
HTML: 2,455
PDF: 1,290
XML: 68
Total: 3,813
BibTeX: 48
EndNote: 59
Views and downloads (calculated since 18 Apr 2018)
Cumulative views and downloads
(calculated since 18 Apr 2018)
Total article views: 2,287 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
1,440
782
65
2,287
47
53
HTML: 1,440
PDF: 782
XML: 65
Total: 2,287
BibTeX: 47
EndNote: 53
Views and downloads (calculated since 01 Feb 2019)
Cumulative views and downloads
(calculated since 01 Feb 2019)
Total article views: 1,526 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
1,015
508
3
1,526
1
6
HTML: 1,015
PDF: 508
XML: 3
Total: 1,526
BibTeX: 1
EndNote: 6
Views and downloads (calculated since 18 Apr 2018)
Cumulative views and downloads
(calculated since 18 Apr 2018)
Viewed (geographical distribution)
Total article views: 3,813 (including HTML, PDF, and XML)
Thereof 3,501 with geography defined
and 312 with unknown origin.
Total article views: 2,287 (including HTML, PDF, and XML)
Thereof 2,069 with geography defined
and 218 with unknown origin.
Total article views: 1,526 (including HTML, PDF, and XML)
Thereof 1,432 with geography defined
and 94 with unknown origin.
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.
In palaeoceanography the shells of single-celled foraminifera are routinely used as proxies to...