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Thomas, D.N.
University of Wales, Bangor, UK
Fogg, G.E.
University of Wales, Bangor, UK. Deceased 2005
Convey, P.
British Antarctic Survey, Cambridge, UK
Fritsen, C.H.
Desert Research Institute, Nevada, USA
Gili, J.-M.
Institut de Ciències del Mar (CSIC), Spanish National Research Council, Spain
Gradinger, R.
University of Fairbanks, Alaska, USA
Laybourn-Parry, J.
University of Tasmania, Australia
Reid, K.
Commission for the Conservation of Antarctic Marine Living Resources, Tasmania, Australia
Walton, D.W.H.
British Antarctic Survey, Cambridge, UK
Print publication date: 2008 (this edition)
Published to Oxford Scholarship Online: May 2008 Print ISBN-13: 978-0-19-929811-2 |
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doi:10.1093/acprof:oso/9780199298112.003.0010
Abstract: The polar regions have undergone major changes in configuration of land masses and climate over millions of years. However, it is the geologically brief period beginning around 120,000 years before present (BP), including a warm interglacial followed by the Würm glaciation and then the interglacial in which we now live, which is most relevant. This chapter discusses changes during geological time: the ice ages; biological responses to long-term changes; and present-day global climate change and polar regions.
Keywords: climate change, global warming, ice age, warm interglacial, Würm glaciation,
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