Encyclopedia of Paleoclimatology and Ancient Environments

2009 Edition
| Editors: Vivien Gornitz

Beetles as Quaternary and Late Tertiary Climate Indicators

  • G. Russell Coope
Reference work entry
DOI: https://doi.org/10.1007/978-1-4020-4411-3_22

Insect remains are particularly abundant in freshwater sediments that have remained waterlogged since their deposition. Most of the remains are of beetles (Coleoptera) because of their robust exoskeletons, but many other orders of insect are also preserved. Beetle species from the Quaternary and late Tertiary can be shown to be identical to their present day representatives. Most past assemblages of beetles can be shown to resemble modern communities closely. It can therefore be safely assumed that physiological stability accompanied their demonstrable morphological constancy. Thus, paleoecological and paleoclimatic inferences can be made on the basis of the past presence of particular beetle species. Many beetle species have changed their geographical ranges by thousands of kilometers even within the limited timespan of the last glacial/interglacial cycle. For instance the most abundant dung beetle in the British Isles during the middle Weichselian (Wisconsin) glaciation is now...

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  1. Atkinson, T.C., Briffa, K.R., and Coope, G.R., 1987. Seasonal temperatures in Britain during the past 22,000 years, reconstructed using beetle remains. Nature, 325, 587–592.CrossRefGoogle Scholar
  2. Coope, G.R., 1959. A Late Pleistocene insect fauna from Chelford, Cheshire. Proc. R. Soc. London, B151, 70–86.Google Scholar
  3. Coope, G.R., 1986. The invasion and colonisation of the North Atlantic islands: A palaeoecological solution to a biogeographic problem. Philos. Trans. R. Soc. London, B314, 619–635.Google Scholar
  4. Coope, G.R., 2000. Middle Devensian (Weichselian) coleopteran assemblages from Earith, Cambridgshire (UK) and their bearing on the interpretation of “Full glacial” floras and faunas. J. Quaternary Sci., 15, 779–788.CrossRefGoogle Scholar
  5. Coope, G.R., 2002. Changes in thermal climate in northwestern Europe during Marine Oxygen Isotope Stage 3, estimated from fossil insect assemblages. Quaternary Res., 57, 401–409.CrossRefGoogle Scholar
  6. Coope, G.R., Gibbard, P.L., Hall, R.C., Preece, R.C., Robinson, J.E., and Sutcliffe, A.J., 1997. Climatic and environmental reconstructions based on fossil assemblages from Middle Devensian (Weichselian) deposits of the River Thames at South Kensington, Central London. Quaternary Sci. Rev., 16, 1163–1195.CrossRefGoogle Scholar
  7. Coope, G.R., Lemdahl, G., Lowe, J.J., and Walkling, A., 1998. Temperature gradients in Northern Europe during the last glacial-transition (14–9, 14C kyr BP) interpreted from coleopteran remains. J. Quaternary Sci., 13, 418–433.CrossRefGoogle Scholar
  8. Elias, S.A., 2000. Mutual climatic range reconstructions of seasonal temperatures based on late Pleistocene fossil beetle assemblages in Eastern Beringia. Quaternary Sci. Rev., 20, 77–91.CrossRefGoogle Scholar
  9. Elias, S.A., and Matthews, J.V. Jr., 2002. Arctic North-American seasonal temperatures from the latest Miocene to the Early Pleistocene based on mutual climatic range analysis of fossil beetle assemblages. Can. J. Earth Sci., 39, 911–920.CrossRefGoogle Scholar

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© Springer-Verlag 2009

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  • G. Russell Coope

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