Bramertonian Stage

The Bramertonian Stage is the name for an early Pleistocene stage used in the British Isles. It precedes the Pre-Pastonian Stage (Baventian Stage). It derives its name from Bramerton Pits in Norfolk, where the deposits can be found on the surface. The exact timing of the beginning and end of the Bramertonian Stage is currently unknown. It is only known that it is equivalent to the Tiglian C1-4b Stage of Europe and early Pre-Illinoian Stage of North America. It lies somewhere in time between Marine Oxygen Isotope stages 65 to 95 and somewhere between 1.816 to 2.427 Ma (million years ago).[1][2][3][4]

During this stage, the climate was temperate with evidence for mixed oak forest in southern England and the arrival of hemlock. Evidence from East Anglia suggests sea levels were higher than they are today.

References

  1. McMillan, A.A., 2005, A provisional Quaternary and Neogene lithostratigraphic framework Great Britain. Netherland Journal of Geosciences. vol. 84, no. 2, pp, 87–107.
  2. Gibbard, P.L., S. Boreham, K.M. Cohen and A. Moscariello, 2007, Global chronostratigraphical correlation table for the last 2.7 million years v. 2007b., jpg version 844 KB. Subcommission on Quaternary Stratigraphy, Department of Geography, University of Cambridge, Cambridge, England
  3. Lisiecki, L.E., 2005, Ages of MIS boundaries. LR04 Benthic Stack Boston University, Boston, MA
  4. Lisiecki, L.E., and M.E. Raymo, 2005, A Pliocene-Pleistocene stack of 57 globally distributed benthic d18O records. Paleoceanography. vol. 20, PA1003, doi:10.1029/2004PA001071

External links

Further reading

See also

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