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FAUNAL ASSEMBLAGES AND DISTRIBUTIONAL SHIFTS OF COLEOPTERA DURING THE LATE PLEISTOCENE IN CANADA AND THE NORTHERN UNITED STATES

Published online by Cambridge University Press:  31 May 2012

Alan V. Morgan  and
Anne Morgan
Alan V. Morgan
Affiliation:
University of Waterloo, Waterloo, Ontario N2L 3G1
Anne Morgan
Affiliation:
University of Waterloo, Waterloo, Ontario N2L 3G1
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Abstract

A faunal list of 362 sub-fossil Coleoptera obtained from 33 published and 24 unpublished sites of Pleistocene age in Canada and the neighbouring United States is given. A table indicates the distribution of families, with the number of species encountered, through discrete intervals of Pleistocene time. Seven species representing members of the Carabidae, Hydrophilidae, Staphylinidae, and Scolytidae have been used to illustrate distribution changes through the last interglacial/glacial/present interglacial cycle. The maximum distance so far recorded is a shift of over 9000 km for Anotylus gibbulus (Epp.), a staphylinid, found fossil in Toronto during the last interglacial, and today recorded only from Eurasia and Asia. A number of other species whose modern ranges are confined to northwestern North America have been found fossil in the Great Lakes – St. Lawrence region, over 4000 km distant. A similar shift is noted in species which today are found only in the eastern Canadian Arctic. Aspects of ice build up, marginal conditions outside the Laurentide Ice Sheet limits, Pleistocene climates, paleoecology, and sub-fossil insect localities are used to formulate hypotheses about three refugia around the perimeter of the Late Wisconsinan ice.

Type
Articles
Information
The Canadian Entomologist , Volume 112 , Issue 11 , 01 November 1980 , pp. 1105 - 1128
Copyright
Copyright © Entomological Society of Canada 1980

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References

Andrews, J. T. 1968. Late-Pleistocene history of the Isortoq Valley North-Central Baffin Island, Canada. pp. 118–133in Sporck, J. A. (Ed.), Mélanges de Géographie offerts à M. Omer Tulippe, I. Editions J. Duculot, S. A., Gembloux.Google Scholar
Armstrong, J. E. and Clague, J. J.. 1977. Two major Wisconsin stratigraphic units in southwest British Columbia. Can. J. earth Sci. 14(7): 1471–1480.CrossRefGoogle Scholar
Arnett, R. H. 1973. The beetles of the United States: A manual for identification. Am. Ent. Inst., Ann Arbor.Google Scholar
Ashworth, A. C. 1977. A late Wisconsinan coleopterous assemblage from southern Ontario and its environmental significance. Can. J. earth Sci. 14(7): 1625–1634.CrossRefGoogle Scholar
Ashworth, A. C. 1980. Environmental implications of a beetle assemblage from the Gervais Formation (Early Wisconsinan?), Minnesota. Quat. Res. 13: 200–212.CrossRefGoogle Scholar
Ashworth, A. C. and Brophy, J. A.. 1972. Late Quaternary fossil beetle assemblage from the Missouri Coteau, North Dakota. Bull. geol. Soc. Am. 83(10): 2981–2988.CrossRefGoogle Scholar
Ashworth, A. C., Clayton, L., and Bickley, W. B.. 1972. The Mosbeck site: A paleoenvironmental interpretation of the Late Quaternary history of Lake Agassiz based on fossil insect and mollusk remains. Quat. Res. 2: 176–188.CrossRefGoogle Scholar
Blake, W. Jr. 1974. Studies of glacial history in Arctic Canada II: Interglacial peat deposits on Bathurst Island. Can. J. earth Sci. 11(8): 1025–1042.CrossRefGoogle Scholar
Blake, W. Jr. and Matthews, J. V. Jr. 1979. New data on an interglacial peat deposit near Makinson Inlet, Ellesmere Island, District of Franklin. Geol. Surv. Can. (Current Research Pt. A) 79-1A: 157–164.Google Scholar
Bright, D. E. 1976. The bark beetles of Canada and Alaska, Coleoptera: Scolytidae. The insects and arachnids of Canada, Pt. 2. Can. Dep. Agric. Publ. 1576.Google Scholar
Brown, W. J. 1937. The Coleoptera of Canada's eastern Arctic. Can. Ent. 69: 106–111.CrossRefGoogle Scholar
Campbell, J. M. 1978. A revision of the North American Omaliinae (Coleoptera: Staphylinidae). Mem. ent. Soc. Can. 106. 87 pp.Google Scholar
Coleman, S. 1894. Interglacial fossils from the Don Valley, Toronto. Am. Geol. 13: 18–95.Google Scholar
Coope, G. R. 1968. Insect remains from silts below till at Garfield Heights, Ohio. Bull. geol. Soc. Am. 79: 753–756.CrossRefGoogle Scholar
Coope, G. R. 1970. Interpretation of Quaternary insect fossils. A. Rev. Ent. 15: 97–120.CrossRefGoogle Scholar
Coope, G. R. 1975. Mid-Weichselian climatic changes in western Europe, re-interpreted from coleopteran assemblages. pp. 101–108in Suggate, R. P. and Cresswell, M. M. (Eds.). Roy. Soc. N.Z.Google Scholar
Coope, G. R. 1977. Quaternary Coleoptera as aids in the interpretation of environmental history. pp. 55–68in Shotton, F. W. (Ed.), British Quaternary Studies: Recent Advances. Clarendon Press, Oxford.Google Scholar
Coope, G. R. 1979. Late Cenozoic fossil Coleoptera: evolution, biogeography, and ecology. Ann. Rev. Ecol. Syst. 10: 247–267.CrossRefGoogle Scholar
Coope, G. R., Shotton, F. W., and Strachan, I.. 1961. A Late Pleistocene fauna and flora from Upton Warren, Worcestershire. Phil. Trans. Roy. Soc. Lond. (B) 244(714): 379–421.Google Scholar
Deevey, E. S. 1949. Biogeography of the Pleistocene. Bull. geol. Soc. Am. 60: 1315–1416.CrossRefGoogle Scholar
Elias, S. A. 1980. Paleoenvironmental interpretations of Holocene insect fossil assemblages from three sites in arctic Canada. Unpub. Ph.D. Thesis, Univ. of Colorado. 331 pp.Google Scholar
Flint, R. F. 1971. Glacial and Quaternary Geology. Wiley, New York.Google Scholar
Gates, W. L. 1976. Modelling the Ice-Age climate. Science 191: 1138–1144.CrossRefGoogle ScholarPubMed
Hammond, P., Morgan, Anne, and Morgan, A. V.. 1979. On the gibbulus Group of Anotylus, and fossil occurrences of Anotylus gibbulus (Staphylinidae). Syst. Ent. 4: 215–221.CrossRefGoogle Scholar
Henriksen, K. L. 1933. Undersøgelser over Danmark — Skanes kvartaere insecktfauna. Vidensk. Meddr dansk. naturh. Foren. 96: 77–325.Google Scholar
Hopkins, D. M., Giterman, R. E., and Matthews, J. V. Jr. 1976. Interstadial mammoth remains and associated pollen and insect fossils, Kotzebue Sound area, northwestern Alaska. Geology 4(3): 169–172.2.0.CO;2>CrossRefGoogle Scholar
Howden, H. F. 1963. Speculations on some beetles, barriers and climates during the Pleistocene and Pre-Pleistocene periods in some nonglaciated portions of North America. Syst. Zool. 12: 178–201.CrossRefGoogle Scholar
Howden, H. F. 1966. Some possible effects of the Pleistocene on the distributions of North American Scarabaeidae. Can. Ent. 98: 1177–1190.CrossRefGoogle Scholar
Howden, H. F. 1969. Effects of the Pleistocene on North American insects. A. Rev. Ent. 14: 39–56.CrossRefGoogle Scholar
Lamb, H. H. 1977. Climatic analysis. pp. 341–350in The Changing Environmental Conditions in Great Britain and Ireland during the Devensian (Past) Cold Stage. Phil. Trans. Roy. Soc. Lond. (B) 280: 103–374.Google Scholar
Lindroth, C. H. 1942. Ett subfossilfynd av Calosoma sycophanta L. Biol. Rev. 2: 1–7.Google Scholar
Lindroth, C. H. 1948. Interglacial insect remains from Sweden. Arsbok Sver. geol. Unders. (C) 42: 1–29.Google Scholar
Lindroth, C. H. 1957. The faunal connections between Europe and North America. Almquist and Wiksell, Stockholm, and Wiley New York.CrossRefGoogle Scholar
Lindroth, C. H. 1963 a. The ground-beetles of Canada and Alaska (3). Opusc. ent. Suppl. 24.Google Scholar
Lindroth, C. H. 1963 b. The fauna history of Newfoundland. Opusc. ent. Suppl. 23.Google Scholar
Matthews, J. V. Jr. 1968. A paleoenvironmental analysis of three Late Pleistocene coleopterous assemblages from Fairbanks, Alaska. Quaest. ent. 4: 202–224.Google Scholar
Matthews, J. V. Jr. 1974 a. Quaternary environments at Cape Deceit (Seward Peninsula, Alaska): Evolution of a tundra ecosystem. Bull. geol. Soc. Am. 85: 1353–1384.2.0.CO;2>CrossRefGoogle Scholar
Matthews, J. V. Jr. 1974 b. Wisconsin environment of interior Alaska: Pollen and macrofossil analysis of a 27 m core from the Isabella Basin (Fairbanks, Alaska). Can. J. earth Sci. 11(6): 828–841.CrossRefGoogle Scholar
Matthews, J. V. Jr. 1975 a. Insects and plant macrofossils from two Quaternary exposures in the Old Crow — Porcupine Region, Yukon Territory, Canada. Arctic and Alpine Res. 7(3): 249–259.CrossRefGoogle Scholar
Matthews, J. V. Jr. 1975 b. Incongruence of macrofossil and pollen evidence: a case from the Late Pleistocene of the northern Yukon coast. Geol. Surv. Can. Pap. 75-1 (b): 139–146.Google Scholar
Matthews, J. V. Jr. 1977. Coleoptera fossils: Their potential value for dating and correlation of late Cenozoic sediments. Can. J. earth Sci. 14(10): 2339–2347.CrossRefGoogle Scholar
Miller, R. F. 1980. Palaeoentomological analysis of a postglacial site in northwestern New York State. Unpub. M.Sc. Thesis, Univ. of Waterloo. 107 pp.Google Scholar
Mjoberg, E. 1916. Über die insektenreste der sogen: Märnögyttja im nordlichen Schweden. Arsbok Sver. geol. Unders. (C) 268.Google Scholar
Morgan, Anne. 1972. The fossil occurrence of Helophorus arcticus Brown (Coleoptera: Hydrophilidae) in Pleistocene deposits of the Scarborough Bluffs, Ontario. Can. J. Zool. 50: 555–558.CrossRefGoogle Scholar
Morgan, Anne. 1973. Late Pleistocene environmental changes indicated by fossil insect faunas of the English Midlands. Boreas 2: 173–212.CrossRefGoogle Scholar
Morgan, A. V. 1972. Late Wisconsinan ice-wedge polygons near Kitchener, Ontario, Canada. Can. J. earth Sci. 9(9): 607–617.CrossRefGoogle Scholar
Morgan, A. V. and Morgan, Anne. 1977. The age and distribution of fossil ice-wedge polygon networks in southwestern Ontario, Canada. Abstracts X INQUA Congress, Birmingham, U.K., 308.Google Scholar
Morgan, A. V. and Morgan, Anne. 1979. The fossil Coleoptera of the Two Creeks Forest Bed, Wisconsin. Quat. Res. 12: 226–240.CrossRefGoogle Scholar
Morgan, A. V. and Morgan, Anne. 1980. Beetle bits — the science of paleoentomology. Geosci. Can. 7(1): 22–38.Google Scholar
Morgan, A. V. and Morgan, Anne. Paleoentomological methods of reconstructing paleoclimate with reference to interglacial and interstadial insect faunas of southern Ontaro: in Quaternary Paleoclimate, Mahaney, W. C. (Ed.). Geoabstracts (in press).Google Scholar
Morlan, R. E. and Matthews, J. V.. 1978. New dates for early man. Geos 1: 2–5.Google Scholar
Pengelly, W. 1870. On the submerged forest at Blackpool, near Dartmouth, South Devon. Geol. Mag. 7(4): 164–167.Google Scholar
Pierce, W. D. 1946. Fossil arthropods of California. 11. Descriptions of the dung beetles (Scarabaeidae) of the tar pits. Bull. So. Calif. Acad. Sci. 45(3): 119–131.Google Scholar
Pierce, W. D. 1947. Fossil arthropods of California. 13. A progress report on the Rancho La Brea asphaltum studies. Bull. So. Calif. Acad. Sci. 46(3): 136–138.Google Scholar
Pierce, W. D. 1954. Fossil arthropods of California. 18. The Tenebrionidae – Tentyriinae of the asphalt deposits. Bull. So. Calif. Acad. Sci. 53(1): 35–45.Google Scholar
Prest, V. K. 1970. Quaternary geology of Canada. pp. 676–764in Douglas, R. J. W. (Ed.), Geology and Ecolomic Minerals of Canada. Dept. E.M.R. and Info. Can., Ottawa.CrossRefGoogle Scholar
Prest, V. K., Terasmae, J., Matthews, J. V. Jr., and Lichti-Federovich, S.. 1976. Late Quaternary history of Magdalen Islands, Quebec. Mar. Seds. 12: 39–59.Google Scholar
Ross, H. H. 1953. On the origin and composition of the nearctic insect fauna. Evolution 7: 145–158.CrossRefGoogle Scholar
Ross, H. H. 1965. Pleistocene events and insects. pp. 583–595in Wright, H. E. and Frey, D. G. (Eds.). Princeton Univ. Press.Google Scholar
Schwert, D. P. 1978. Paleoentomological analyses of two postglacial sites in eastern North America. Unpub. Ph.D. Thesis, Univ. of Waterloo. 250 pp.Google Scholar
Schwert, D. P. and Morgan, A. V.. 1980. Paleoenvironmental implications of a Late Glacial insect assemblage from northwestern New York. Quat. Res. 13: 93–110.CrossRefGoogle Scholar
Scudder, S. H. 1877. Description of two species of Carabidae found in the interglacial deposits of Scarboro Hts., in Toronto, Canada. U.S. geol. geog. Surv. of the Territories (Hayden) B3: 763–764.Google Scholar
Scudder, S. H. 1890. The fossil insects of North America (2). U.S. geol. Surv. Rep. 8.Google Scholar
Scudder, S. H. 1895. The Coleoptera hitherto found fossil in Canada. Geol. Surv. Can. Contrib. to Can. Paleo. 2: 27–56.Google Scholar
Scudder, S. H. 1900. Additions to the coleopterous fauna of the interglacial clays of the Toronto district. Geol. Surv. Can. Contrib. to Can. Paleo. 2: 67–92.Google Scholar
Stuiver, M., Heusser, C. J., and Yang, I. C.. 1978. North American glacial history extended to 75,000 years ago. Science 200: 16–21.CrossRefGoogle ScholarPubMed
Thiele, H. 1977. Carabid Beetles in Their Environments. Springer-Verlag, New York. 369 pp.CrossRefGoogle Scholar
Thorkelsson, T. 1935. A fossiliferous interglacial layer at Eillidaarvogur Reykjavík. Greinar (Soc. Sci. Island) 1(1): 78–91.Google Scholar
Williams, N. and Morgan, A. V.. 1977. Fossil caddisflies (Insecta: Trichoptera) from the Don Formation, Toronto, Ontario and their use in paleoecology. Can. J. Zool. 55(3): 519–527.CrossRefGoogle Scholar
Zeuner, F. 1934. Szaránozaki z warstw dyluwijalnych Staruni. Die orthopteren aus der diluvialen nashornschicht von Starunia (Polische Karpathen). Starunia 3: 1–17.Google Scholar