Skip to main content

Part of the book series: Encyclopedia of Earth Sciences Series ((EESS))

Definitions

Interstadials are regarded as the relatively short-lived periods of thermal improvement during a glacial phase, when temperatures did not reach those of the present day and, in lowland mid-latitude regions, the climax vegetation was boreal woodland (Lowe and Walker, 1997). Jessen and Milthers (1928) defined interstadials as periods that are either too short or too cold to allow the development of temperate deciduous forest of interglacial type in the same region. Interstadials are, however, not only defined on biostratigraphical grounds. In the USA, for instance, an interstadial is formally regarded as a climatic episode within a glaciation during which a secondary recession or standstill of glaciers took place (Gibbard and West, 2000).

Interstadials during the Weichselian

Many different interstadials are defined in Europe based on palynology. The interstadials that occurred during, for instance, the Weichselian Glacial have been named after the place where the interstadial...

This is a preview of subscription content, log in via an institution to check access.

Access this chapter

Chapter
USD 29.95
Price excludes VAT (USA)
  • Available as PDF
  • Read on any device
  • Instant download
  • Own it forever
eBook
USD 449.99
Price excludes VAT (USA)
  • Available as PDF
  • Read on any device
  • Instant download
  • Own it forever
Hardcover Book
USD 649.99
Price excludes VAT (USA)
  • Durable hardcover edition
  • Dispatched in 3 to 5 business days
  • Free shipping worldwide - see info

Tax calculation will be finalised at checkout

Purchases are for personal use only

Institutional subscriptions

Bibliography

  • Behre, K.E., 1989. Biostratigraphy of the last glacial period in Europe. Quaternary Sci. Rev., 8, 25–44.

    Google Scholar 

  • Bond, G., Broecker, W., Johnsen, S., McManus, J., Labeyrie, L., Jouzel, J., and Bonani, G., 1993. Correlations between climate records from North Atlantic sediments and Greenland ice. Nature, 365, 143–147.

    Google Scholar 

  • Dansgaard, W., Johnsen, S.J., Clausen, H.B., Dahl-Jensen, D., Gundestrup, N.S., Hammer, C.U., Hvidberg, C.S., Steffensen, J.P., Sveinbjörnsdottir, A.E., Jouzel, J., and Bond, G., 1993. Evidence for general instability of past climate from a 250-kyr ice-core record. Nature, 364, 218–220.

    Google Scholar 

  • de Beaulieu, J.L., and Reille, M., 1992. The last climatic cycle at La Grande Pile (Vosges, France): A new pollen profile. Quaternary Science Reviews, 11, 431–438.

    Google Scholar 

  • Jessen, K., and Milthers, V., 1928. Stratigraphical and palaeontological studies of interglacial freshwater deposits in Jutland and north-west Germany. Danmarks Geologiske Undersøgelse II, 48, 380pp.

    Google Scholar 

  • Gibbard, P.L., and West, R.G., 2000. Quaternary chronostratigraphy: The nomenclature of terrestrial sequences. Boreas, 29, 329–336.

    Google Scholar 

  • Lowe, J.J., and Walker, M.J.C., 1997. Reconstructing Quaternary Environments. London, UK: Longman, 446pp.

    Google Scholar 

  • North Greenland Ice Core Project (NGRIP) Members, 2004. High-resolution record of Northern Hemisphere climate extending into the last interglacial period. Nature, 431, 147–151.

    Google Scholar 

  • Zagwijn, W.H., 1989. Vegetation and climate during warmer intervals in the Late Pleistocene of western and central Europe. Quaternary Int., 3–4, 57–67.

    Google Scholar 

Download references

Authors

Editor information

Editors and Affiliations

Rights and permissions

Reprints and permissions

Copyright information

© 2009 Springer-Verlag

About this entry

Cite this entry

Hoek, W.Z. (2009). Interstadials. In: Gornitz, V. (eds) Encyclopedia of Paleoclimatology and Ancient Environments. Encyclopedia of Earth Sciences Series. Springer, Dordrecht. https://doi.org/10.1007/978-1-4020-4411-3_115

Download citation

Publish with us

Policies and ethics