Articles | Volume 14, issue 7
https://doi.org/10.5194/cp-14-1015-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Special issue:
https://doi.org/10.5194/cp-14-1015-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Paleoceanography and ice sheet variability offshore Wilkes Land, Antarctica – Part 2: Insights from Oligocene–Miocene dinoflagellate cyst assemblages
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
Invited contribution by Peter K. Bijl, recipient of the EGU Arne Richter Award for Outstanding Early Career Scientists 2014.
Alexander J. P. Houben
Geological Survey of the Netherlands, Netherlands Organisation for Applied
Scientific Research (TNO), Princetonlaan 6, 3584 CB, Utrecht, the
Netherlands
Julian D. Hartman
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, Heidelberg
University, Im Neuenheimer Feld 234, 69120 Heidelberg, Germany
Ariadna Salabarnada
Instituto Andaluz de Ciencias de la Tierra, CSIC-UGR, 18100 Armilla, Spain
Carlota Escutia
Instituto Andaluz de Ciencias de la Tierra, CSIC-UGR, 18100 Armilla, Spain
Francesca Sangiorgi
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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Short summary
We document Southern Ocean surface ocean conditions and changes therein during the Oligocene and Miocene (34–10 Myr ago). We infer profound long-term and short-term changes in ice-proximal oceanographic conditions: sea surface temperature, nutrient conditions and sea ice. Our results point to warm-temperate, oligotrophic, ice-proximal oceanographic conditions. These distinct oceanographic conditions may explain the high amplitude in inferred Oligocene–Miocene Antarctic ice volume changes.
We document Southern Ocean surface ocean conditions and changes therein during the Oligocene and...
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