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
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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...
