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Polar front shift and atmospheric CO2 during the glacial maximum of the Early Paleozoic Icehouse.

Vandenbroucke, T.R.A. and Armstrong, H. A. and Williams, M. and Paris, F. and Zalasiewicz, Jan A. and Sabbe, K. and lvak, J. A. and Challands, T.J. and Verniers, J. and Servais, T. (2010) 'Polar front shift and atmospheric CO2 during the glacial maximum of the Early Paleozoic Icehouse.', Proceedings of the National Academy of Sciences of the United States of America., 107 (34). pp. 14983-14986.


Our new data address the paradox of Late Ordovician glaciation under supposedly high pCO2 (8 to 22× PAL: preindustrial atmospheric level). The paleobiogeographical distribution of chitinozoan (“mixed layer”) marine zooplankton biotopes for the Hirnantian glacial maximum (440 Ma) are reconstructed and compared to those from the Sandbian (460 Ma): They demonstrate a steeper latitudinal temperature gradient and an equatorwards shift of the Polar Front through time from 55°–70° S to ∼40° S. These changes are comparable to those during Pleistocene interglacial-glacial cycles. In comparison with the Pleistocene, we hypothesize a significant decline in mean global temperature from the Sandbian to Hirnantian, proportional with a fall in pCO2 from a modeled Sandbian level of ∼8× PAL to ∼5× PAL during the Hirnantian. Our data suggest that a compression of midlatitudinal biotopes and ecospace in response to the developing glaciation was a likely cause of the end-Ordovician mass extinction.

Item Type:Article
Keywords:Chitinozoans, Ordovician, Zooplankton biotopes, Hirnantian glaciations, Climate belts.
Full text:(AM) Accepted Manuscript
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Record Created:20 Oct 2011 12:20
Last Modified:28 Oct 2011 13:33

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