NIOZ Royal Netherlands Institute for Sea Research, Department of Ocean
Systems, 1790 AB, Den Burg, and Utrecht University, the Netherlands
Earth and Climate Cluster, Department of Earth Sciences, Faculty of
Science, VU University Amsterdam, de Boelelaan 1085, 1081 HV, Amsterdam,
the Netherlands
Earth and Climate Cluster, Department of Earth Sciences, Faculty of
Science, VU University 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
Wouter Feldmeijer
Earth and Climate Cluster, Department of Earth Sciences, Faculty of
Science, VU University Amsterdam, de Boelelaan 1085, 1081 HV, Amsterdam,
the Netherlands
now at: Nebest B.V., Marconiweg 2, 4131 PD, Vianen, the Netherlands
Maarten A. Prins
Earth and Climate Cluster, Department of Earth Sciences, Faculty of
Science, VU University Amsterdam, de Boelelaan 1085, 1081 HV, Amsterdam,
the Netherlands
Jasmijn van 't Hoff
Earth and Climate Cluster, Department of Earth Sciences, Faculty of
Science, VU University Amsterdam, de Boelelaan 1085, 1081 HV, Amsterdam,
the Netherlands
now at: Institute of Geology and Mineralogy, University of Cologne,
Zuelpicher Str. 49a, 50674 Cologne, Germany
Gerald M. Ganssen
Earth and Climate Cluster, Department of Earth Sciences, Faculty of
Science, VU University Amsterdam, de Boelelaan 1085, 1081 HV, Amsterdam,
the Netherlands
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Total article views: 6,366 (including HTML, PDF, and XML)
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Here, mid-ocean seasonality is resolved through time, using differences in the oxygen isotope composition between individual shells of the commonly used (sub)polar planktonic foraminifera species in ocean-climate reconstruction, N. pachyderma and G. bulloides. Single-specimen isotope measurements during the deglacial period revealed a surprising bimodality, the cause of which was investigated.
Here, mid-ocean seasonality is resolved through time, using differences in the oxygen isotope...
