Reorganization of Southern Ocean Plankton Ecosystem at the Onset of Antarctic Glaciation
Reorganization of Southern Ocean Plankton Ecosystem at the Onset of Antarctic Glaciation
The circum-Antarctic Southern Ocean is an important region for global marine food webs and carbon cycling because of sea-ice formation and its unique plankton ecosystem. However, the mechanisms underlying the installation of this distinct ecosystem and the geological timing of its development remain unknown. Here, we show, on the basis of fossil marine dinoflagellate cyst records, that a major restructuring of the Southern Ocean plankton ecosystem occurred abruptly and concomitant with the first major Antarctic glaciation in the earliest Oligocene (~33.6 million years ago). This turnover marks a regime shift in zooplankton-phytoplankton interactions and community structure, which indicates the appearance of eutrophic and seasonally productive environments on the Antarctic margin. We conclude that earliest Oligocene cooling, ice-sheet expansion, and subsequent sea-ice formation were important drivers of biotic evolution in the Southern Ocean.
341-344
Houben, A.J.P.
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Bijl, P.K.
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Pross, J.
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Bohaty, S.M.
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Passchier, S.
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Stickley, C.E.
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Rohl, U.
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Sugisaki, S.
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Tauxe, L.
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van de Flierdt, T.
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Olney, M.
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Sangiorgi, F.
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Sluijs, A.
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Escutia, C.
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Brinkhuis, H.
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19 April 2013
Houben, A.J.P.
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Bijl, P.K.
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Pross, J.
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Bohaty, S.M.
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Passchier, S.
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Stickley, C.E.
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Rohl, U.
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Sugisaki, S.
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Tauxe, L.
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van de Flierdt, T.
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Olney, M.
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Sangiorgi, F.
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Sluijs, A.
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Escutia, C.
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Brinkhuis, H.
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Houben, A.J.P., Bijl, P.K., Pross, J., Bohaty, S.M., Passchier, S., Stickley, C.E., Rohl, U., Sugisaki, S., Tauxe, L., van de Flierdt, T., Olney, M., Sangiorgi, F., Sluijs, A., Escutia, C. and Brinkhuis, H.
(2013)
Reorganization of Southern Ocean Plankton Ecosystem at the Onset of Antarctic Glaciation.
Science, 340 (6130), .
(doi:10.1126/science.1223646).
Abstract
The circum-Antarctic Southern Ocean is an important region for global marine food webs and carbon cycling because of sea-ice formation and its unique plankton ecosystem. However, the mechanisms underlying the installation of this distinct ecosystem and the geological timing of its development remain unknown. Here, we show, on the basis of fossil marine dinoflagellate cyst records, that a major restructuring of the Southern Ocean plankton ecosystem occurred abruptly and concomitant with the first major Antarctic glaciation in the earliest Oligocene (~33.6 million years ago). This turnover marks a regime shift in zooplankton-phytoplankton interactions and community structure, which indicates the appearance of eutrophic and seasonally productive environments on the Antarctic margin. We conclude that earliest Oligocene cooling, ice-sheet expansion, and subsequent sea-ice formation were important drivers of biotic evolution in the Southern Ocean.
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Published date: 19 April 2013
Organisations:
Paleooceanography & Palaeoclimate
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Local EPrints ID: 353311
URI: http://eprints.soton.ac.uk/id/eprint/353311
ISSN: 0036-8075
PURE UUID: 7f7c4ade-2c41-436d-a5b6-52dfd738f820
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Date deposited: 04 Jun 2013 15:47
Last modified: 15 Mar 2024 03:27
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Contributors
Author:
A.J.P. Houben
Author:
P.K. Bijl
Author:
J. Pross
Author:
S. Passchier
Author:
C.E. Stickley
Author:
U. Rohl
Author:
S. Sugisaki
Author:
L. Tauxe
Author:
T. van de Flierdt
Author:
M. Olney
Author:
F. Sangiorgi
Author:
A. Sluijs
Author:
C. Escutia
Author:
H. Brinkhuis
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