Pastonian Stage
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The Pastonian interglacial, now called the Pastonian Stage (from Paston, Norfolk), is the name for an early or middle
Pleistocene The Pleistocene ( , often referred to as the ''Ice age'') is the geological epoch that lasted from about 2,580,000 to 11,700 years ago, spanning the Earth's most recent period of repeated glaciations. Before a change was finally confirmed in ...
stage used in the
British Isles The British Isles are a group of islands in the North Atlantic Ocean off the north-western coast of continental Europe, consisting of the islands of Great Britain, Ireland, the Isle of Man, the Inner and Outer Hebrides, the Northern Isles, ...
. It precedes the
Beestonian Stage The Beestonian Stage is an early Pleistocene stage used in the British Isles. It is named after Beeston Cliffs near West Runton in Norfolk where deposits from this stage are preserved. The Beestonian precedes the Cromerian Stage and follows the ...
and follows the
Pre-Pastonian Stage The Pre-Pastonian Stage or Baventian Stage (from Easton Bavents in Suffolk), is the name for an early Pleistocene stage used in the British Isles. It precedes the Pastonian Stage and follows the Bramertonian Stage. This stage ended 1.806 Ma (mi ...
. Unfortunately the precise age of this stage cannot yet be defined in terms of absolute dating or MIS stages. The Pre-Pastonian Stage is equivalent to the
Tiglian The Tiglian, also referred to as the Tegelen, is a temperate complex stage in the glacial history of Northern Europe. It is preceded by the Praetiglian (stage). The stage was introduced by Zagwijn in 1957 based on geological formations in Tegelen i ...
C5-6 Stage of Europe and the Pre-Illinoian I glaciation of the early Pre-Illinoian Stage of North America.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
Lisiecki, L.E., 2005
Ages of MIS boundaries.
Boston University, Boston, MA


data: .
Deciduous woodland, increased including species such as
Hornbeam Hornbeams are hardwood trees in the flowering plant genus ''Carpinus'' in the birch family Betulaceae. The 30–40 species occur across much of the temperate regions of the Northern Hemisphere. Origin of names The common English name ''hornbeam ...
(''Carpinus''),
Elm Elms are deciduous and semi-deciduous trees comprising the flowering plant genus ''Ulmus'' in the plant family Ulmaceae. They are distributed over most of the Northern Hemisphere, inhabiting the temperate and tropical-montane regions of North ...
(''Ulmus''), Hazel (''Corylus''), and Spruce (''Picea''). Towards the end of the period, there is evidence for a fall in sea levels and an increase in grassland species.


References


External links

*anonymous, 2007
''Global correlation tables for the Quaternary''
Subcommission on Quaternary Stratigraphy, Department of Geography, University of Cambridge, Cambridge, England


Further reading

*Bowen, D.Q., 1978, ''Quaternary geology: a stratigraphic framework for multidisciplinary work. '' Pergamon Press, Oxford, United Kingdom. 221 pp. *Ehlers, J., P. L. Gibbard, and J. Rose, eds., 1991, ''Glacial deposits in Great Britain and Ireland.'' Balkema, Rotterdam. 580 pp *Mangerud, J., J. Ehlers, and P. Gibbard, 2004, ''Quaternary Glaciations: Extent and Chronology 1: Part I Europe'', Elsevier, Amsterdam. *


See also

*
Ice age An ice age is a long period of reduction in the temperature of Earth's surface and atmosphere, resulting in the presence or expansion of continental and polar ice sheets and alpine glaciers. Earth's climate alternates between ice ages and gre ...
*
Glacial period A glacial period (alternatively glacial or glaciation) is an interval of time (thousands of years) within an ice age that is marked by colder temperatures and glacier advances. Interglacials, on the other hand, are periods of warmer climate betwe ...
* Last glacial period *
Timeline of glaciation There have been five or six major ice ages in the history of Earth over the past 3 billion years. The Late Cenozoic Ice Age began 34 million years ago, its latest phase being the Quaternary glaciation, in progress since 2.58 million years ago ...
Glaciology Pleistocene Interglacials {{Glaciology-stub