Marine Palynology and Paleoceanography, Laboratory of Palaeobotany and
Palynology, Department of Earth Sciences, Faculty of Geosciences, Utrecht
University, P.O. Box 80.115, 3508 TC Utrecht, the Netherlands
Applied Geosciences Team, Netherlands Organisation for Applied Scientific
Research (TNO), Princetonlaan 6, 3584 CB, Utrecht, the Netherlands
Anja Bruls
Marine Palynology and Paleoceanography, Laboratory of Palaeobotany and
Palynology, Department of Earth Sciences, Faculty of Geosciences, Utrecht
University, P.O. Box 80.115, 3508 TC Utrecht, the Netherlands
Jörg Pross
Paleoenvironmental Dynamics Group, Institute of Earth Sciences, University
of Heidelberg, Im Neuenheimer Feld 234, 69120 Heidelberg, Germany
Marine Palynology and Paleoceanography, Laboratory of Palaeobotany and
Palynology, Department of Earth Sciences, Faculty of Geosciences, Utrecht
University, P.O. Box 80.115, 3508 TC Utrecht, the Netherlands
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In order to use ocean sediments as a recorder of past oceanographic changes, a critical first step is to stratigraphically date the sediments. The absence of microfossils with known stratigraphic ranges has always hindered dating of Southern Ocean sediments. Here we tie dinocyst ranges to the international timescale in a well-dated sediment core from offshore Antarctica. With this, we can now use dinocysts as a biostratigraphic tool in otherwise stratigraphically poorly dated sediments.
In order to use ocean sediments as a recorder of past oceanographic changes, a critical first...
