Reorganization of Southern Ocean Plankton Ecosystem at the Onset of Antarctic Glaciation-Reference-Cited by-同舟云学术

Reorganization of Southern Ocean Plankton Ecosystem at the Onset of Antarctic Glaciation

Published:2013-04-19 Issue:6130 Volume:340 Page:341-344
ISSN:0036-8075
Container-title:Science
language:en
Short-container-title:Science

Author:

Houben Alexander J. P.¹,Bijl Peter K.¹,Pross Jörg²³,Bohaty Steven M.⁴,Passchier Sandra⁵,Stickley Catherine E.⁶,Röhl Ursula⁷,Sugisaki Saiko⁸,Tauxe Lisa⁸,van de Flierdt Tina⁹,Olney Matthew¹⁰,Sangiorgi Francesca¹,Sluijs Appy¹,Escutia Carlota¹¹,Brinkhuis Henk¹,

Affiliation:

1. Department of Earth Sciences, Laboratory of Palaeobotany and Palynology (LPP), Faculty of Geosciences, Utrecht University, Budapestlaan 4, 3584 CD Utrecht, Netherlands.

2. Paleoenvironmental Dynamics Group, Institute of Geosciences, Goethe University Frankfurt, Altenhöferallee 1, 60438 Frankfurt, Germany.

3. Biodiversity and Climate Research Centre, Senckenberganlage 25, 60325 Frankfurt, Germany.

4. Ocean and Earth Science, University of Southampton, National Oceanography Centre, European Way, Southampton SO14 3ZH, UK.

5. Department of Earth and Environmental Studies, Montclair State University, 1 Normal Avenue, Montclair, NJ 07043, USA.

6. Department of Geology, University of Tromsø, Breivika, N-9037 Tromsø, Norway.

7. MARUM Center for Marine Environmental Sciences, University of Bremen, Leobener Straße, 28359 Bremen, Germany.

8. Scripps Institution of Oceanography, University of California at San Diego, 8635 Kennel Way, La Jolla, CA 92093–0220, USA.

9. Department of Earth Science and Engineering, Imperial College London, Exhibition Road, SW7 2AZ, London, UK.

10. Department of Geology, University of South Florida, 4202 East Fowler Avenue, Tampa, FL 33620, USA.

11. Instituto Andaluz de Ciencias de la Terra, Avenida de las Palmeras, 4, 18100 Armilla (Granada), Spain.

Abstract

Southern Change Antarctica has been mostly covered by ice since the inception of large-scale continental glaciation during the Oligocene, which profoundly altered the isotopic and mineralogical records of the sediments surrounding the continent. Houben et al. (p. 341 ) found records of the corresponding living systems in the fossil marine dinoflagellate cysts, which revealed that a microplankton ecosystem, similar to the one that exists today, appeared simultaneously with the first major Antarctic glaciation approximately 34 million years ago.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

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