Cambridge Quaternary
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Scan day: 03 February 2014 UTC
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Description: Collaborators from several departments engaged in study of paleogeography, Quaternary history and stratigraphy, geoarcheology, palynology, paleontology, and related topics. Describes research, personnel, facilities, and activities.
The Quaternary, the last 2.6 million years of geological time, saw major climatic changes which caused ice sheets to advance intotemperate latitudes. Repeated glacial episodes caused significant fluctuations in sea level, major geographical changes and major plant and animal population migrations. Sedimentary sequences record these changes in great detail and are central to unravelling past events.
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| Page title: | Cambridge Quaternary |
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