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The climatic significance of coleopteran assemblages from the Eemian deposits in southern England

Published online by Cambridge University Press:  01 April 2016

G. Russell Coope*
Affiliation:
School of Geological Sciences, University of Birmingham, Edgbaston, BIRMINGHAM, B15 2TT, UK
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Abstract

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Assemblages of fossil coleoptera (beetles) have been obtained from eight sites in southern England that date from the early phase (Pinus — Quercetum mixtum — Corylus pollen assemblage zone) of the Eemian (Ipswichian) interglacial Stage. Altogether 294 different species have been identified from these sites. They represent a wide spectrum of habitat requirements; terrestrial, aquatic, carnivorous and phytophagous species and many more with subtle dependences of specialist biotopes. Almost all of them live today in central and southern Europe and some are restricted to regions well south of the British Isles.

By using mutual climatic range methods, the thermal climate of the early phase of the Eemian Interglacial has been estimated quantitatively, showing that mean July temperatures were about 4°C above those of southern England today. Mean winter temperatures were not much different from those nowadays. This phase was probably the thermal maximum of the Eemian Interglacial. Precipitation levels are difficult to quantify but were adequate to maintain flowing rivers in England throughout the year. These results are in agreement with the presence of other fossils, both plants and animals, in the same deposits.

Type
Research Article
Copyright
Copyright © Stichting Netherlands Journal of Geosciences 2000

References

Aalbersberg, G. & Litt, T., 1998. Multiproxy climate reconstructions for the Eemian and Early Weichselian. Journal of Quaternary Science 13: 367390.Google Scholar
Atkinson, T.C., Briffa, K.R. & Coope, G.R., 1987. Seasonal temperatures in Britain during the past 22,000 years, reconstructed using beetle remains. Nature 325: 587592.Google Scholar
Balachowski, A., 1950. Scolytidae. Faune de France (Paris): 320 pp.Google Scholar
Balfour Browne, F., 1950. British water beetles. Volume 2. The Ray Society (London): 394 pp.Google Scholar
Balfour Browne, F., 1958. British water beetles. Volume 3. The Ray Society (London): 210 pp.Google Scholar
Balthazar, V., 1963. Monographie der Scarabaeidae und Aphodiidae der palaearktischen und orientalischen Region, 2, Coprinae. Tschechoslowakischen Akademie der Wissenschaften (Praha): 627 pp.Google Scholar
Baraud, J., 1985. Coléoptères Scarabaeoidea, Faune du Nord de l’Afrique du Maroc au Sinaï. Lechevalier (Paris): 203205.Google Scholar
Beesley, A.R., 1988. The climatic and environmental significance of an interglacial coleopterous fauna from Itteringham, Norfolk. Unpublished M.Sc. thesis, Department of Geology, University of Birmingham.Google Scholar
Buckland, P.C. & Coope, G.R., 1991. A bibliography and literature review of Quaternary entomology. J.R. Collis Publications (University of Sheffield): 85 pp.Google Scholar
Coope, G.R., 1959. A Late Pleistocene insect fauna from Chelford, Cheshire. Proceedings of the Royal Society of London B 151: 7086.Google Scholar
Coope, G.R., 1974. Interglacial coleoptera from Bobbitshole, Ipswich, Suffolk. Journal of the Geological Society of London 130: 333340.Google Scholar
Coope, G.R., 1986a. Evidence from insect fossils for sudden and intense climatic changes during the last 45,000 years. In: Berger, W.H. & Labeyrie, L.D. (eds.): The book of abstracts and reports from the conference on: Abrupt climatic change (NATO/ NSF). Scripps Institute of Oceanography Reference Series (University of California): 9092.Google Scholar
Coope, G.R., 1986b. The invasion and colonisation of the North Atlantic islands: a palaeoecological solution to a biogeographic problem. Philosophical Transactions of the Royal Society of London B 314: 619635.Google Scholar
Coope, G.R., Lemdahl, G., Lowe, J.J. & Walkling, A., 1998. Temperature gradients in northern Europe during the last glacial-Holocene transition (14-9 14C kyr BP) interpreted from coleopteran assemblages. Journal of Quaternary Science 13: 418433.Google Scholar
Davey, N.D.W., Bridgland, D.R. & Keen, D.H., 1991. Maxey gravel pit, near Peterborough. In: Lewis, S.G., Whiteman, C.A. & Bridgland, D.R. (eds.): Central East Anglia & the Fen Basin: field guide. Quaternary Research Association (Nottingham): 185208.Google Scholar
De Rouffignac, C., Bowen, D.Q., Coope, G.R., Keen, D.H., Lister, A.M., Maddy, D., Robinson, J.E., Sykes, G.A. & Walker, M.J.C., 1995. Late Middle Pleistocene interglacial deposits at Upper Strensham, Worcestershire, England. Journal of Quaternary Science 10: 1532.Google Scholar
Dinnin, M.H., 1991. The sub-fossil occurrence of the Greater Silver Water Beetle Hydrophilus piceus (L.) at Shirley Pool, South Yorkshire. Naturalist (Hull) 116: 5759.Google Scholar
Elias, S.A., 1994. Quaternary insects and their environments. Smithsonian Institution Press (Washington/London): 284 pp.Google Scholar
Franks, J.W., Sutcliffe, A.J., Kerney, M.P. & Coope, G.R., 1958. Haunt of elephant and rhinoceros: the Trafalgar Square of 100,000 years ago - new discoveries. Illustrated London News: 11011103.Google Scholar
Gao, C., Keen, D.H., Borham, S., Coope, G.R., Pettit, M.E., Stuart, A.J. & Gibbard, P.L., 2000. Last interglacial and Devensian deposits of the River Great Ouse at Woolpack Farm, Fenstanton, Cambridgeshire, UK. Quaternary Science Reviews 19: 787810.Google Scholar
Gibbard, P.L., 1995. The Pleistocene history of the Middle Thames Valley. Cambridge University Press (Cambridge etc.): 155 pp.Google Scholar
Green, C.P., Coope, G.R., Currant, A.P., Holyoak, D.T., Ivanovich, M., Jones, R.L., Keen, D.H., McGregor, D.F.M. & Robinson, J.E., 1984. Evidence of two temperate episodes in late Pleistocene deposits at Marsworth, UK. Nature 309: 778781.CrossRefGoogle ScholarPubMed
Grichuk, V.P., 1969. An attempt to reconstruct certain elements of the climate of the northern hemisphere in the Atlantic Period of the Holocene. In: Golotsen, K. In: Neishadt, M.I. (ed.): viii kongressu INQUA (Paris): 4157.Google Scholar
Guest, J., 1996. Hydrochara caraboides (L.) (Hydrophilidae) in Cheshire. The Coleopterist 5: 19.Google Scholar
Hansen, M., 1987. The Hydrophiloidea (Coleoptera) of Fennoscandia and Denmark. Fauna Entomologica Scaninavica 18. E.J. Brill (Leiden): 254 pp.Google Scholar
Henriksen, K.L., 1933. Undersøgelser over Danmark-Skanes Kvartaere Insektfauna. Videnskabelige Meddelelser fra Danske naturhistorisk Förening i København 96: 77355.Google Scholar
Hodge, J. & Jones, R.A., 1995. New British beetles: species not in Joy’s practical handbook. British Entomological and Natural History Society (Reading): 175 pp.Google Scholar
Iversen, J., 1944. Viscum, Hedera and Ilex as climatic indicators. Geol. Foren. Forhandl. (Stockholm) 66: 463483.Google Scholar
Keen, D.H., Bateman, M.D., Coope, G.R., Field, M.H., Langford, H.E., Merry, J.S. & Mighall, T.M., 1999. Sedimentology, palaeoecology and geochronology of last interglacial deposits from Deeping St James, Lincolnshire, England. Journal of Quaternary Science 14: 411436.Google Scholar
Lindroth, C.H., 1948. Interglacial insect remains from Sweden. Årsbok Sveriges Geologiska Undersökning C42: 129.Google Scholar
Lindroth, C.H., 1986. The Carabidae (Coleoptera) of Fennoscandia and Denmark. Fauna Entomologica Scandinavica 15: 233497.Google Scholar
Lomnicki, A.M., 1894. Fauna pleistocenica insectorum Boryslaviensium (in Polish). Wydwnictwa Muzeum imienia Dzieduszyckich 4: 1116.Google Scholar
Lomnicki, A.M., 1914. The invertebrata of the mammoth shaft (in Polish). Wydawnictwa Muzeum imienia Dzieduszyckisch 15: 3789.Google Scholar
Lucht, W.H., 1987. Die Käfer Mitteleuropas; Katalog. Goecke & Evers (Krefeld):342pp.Google Scholar
Mjöberg, E., 1915. Über die Insektenreste der sogennanten “Härnögyttja” in nordlichen Schweden. Sveriges Geologiska Undersökning C268: 114.Google Scholar
Scudder, S.H., 1895. The coleoptera hitherto found fossil in Canada. Contributions to Canadian Palaeontology (Geological Survey of Canada) 2: 2756.Google Scholar
Stuart, A.J., 1979. Pleistocene occurrences of the European pond tortoise (Emys orbicularis) in Britain. Boreas 8: 359371.CrossRefGoogle Scholar
Stuart, A.J., 1982. Pleistocene vertebrates in the British Isles. Longman (London).Google Scholar
Taylor, B.J. & Coope, G.R., 1985. Arthropods in the Quaternary of East Anglia - their role as indices of local palaeoenvironments and regional palaeoclimates. Modern Geology 9: 159185.Google Scholar
Walker, M.J.C., Coope, G.R. & Lowe, J.J., 1993. The Devensian (Weichselian) Lateglacial palaeoenvironmental record from Gransmoor, East Yorkshire, England. Quaternary Science Reviews 12: 659680.Google Scholar
Walkling, A.P., 1996. Coleoptera records from the last interglacialglacial transition. Unpublished Ph.D. thesis, Department of Geography, Royal Holloway, University of London.Google Scholar
Walkling, A.P. & Coope, G.R., 1996. Climatic reconstructions from the Eemian/Early Weichselian transition in Central Europe based on the coleopteran record from Gröbern, Germany. Boreas 25: 145159.Google Scholar
West, R.G., 1957. Interglacial deposits at Bobbitshole, Ipswich. Philosophical Transactions of the Royal Society of London B241: 131.Google Scholar