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  • Coleoptera faunal composition in Belarus in the terminal Pleistocene
  • Remnants of Coleoptera of late glacial age have been investigated at 8 sites in Belarus. The sites are situated at varying distances from the maximum extent of the last glaciation. The palaeo-temperatures of the month of july during the lifespan
  • of the beetles are reconstructed by comparison with their present habitats. Close to the margin of the ice shield the Coleoptera fauna proved to be more diverse, even including species of the present-day northern taiga area, than in the more humid periglacial
  • Le régime alimentaire de Abax ater Vill. (Coleoptera, Carabidae). (The diet of Abax ater Vill. (Coleoptera, Carabidae))
  • Het voorkomen van schrijvertjes (Coleoptera: Gyrinidae) in Oost-en West-Vlaanderen (België). (The occurence of whirligig-beetles (Coleoptera: Gyrinidae, in East and West Flanders))
  • Distribution of Noterinae, Laccophilinae and Dytiscina (Coleoptera: dytiscidae) in East and West Flanders
  • Carabid beetle distribution along humidity-gradients in rivulet-associated grasslands (Coleoptera, Carabidae)
  • Arealsystemanalyse afrikanischer Fühlerkafer (Coleoptera, Carabidae, Paussidae). Ein Beitrag zur Rekonstruktion der Landschaftsgenese. Analyse de système de l'aire des antennates africains (Coleoptera, Carabidae, Paussidae). Contribution à la
  • Lateglacial environmental changes interpreted from fossil coleoptera from St. Bees, Cumbria, NW England in Studies in the Lateglacial of North-West Europe.
  • Coleoptera that indicate cooler conditions. During classical pollen zone III times (the Loch Lomond Stadial) the insect fauna had definite Arctic affinities and included a high proportion of obligate Arctic/Alpine species that are no longer found living
  • in the British Isles. This sequence of climatic events interpreted from fossil Coleoptera is entirely in keeping with similar data from other Lateglacial sites in Britain and Ireland.
  • Insecta Coleoptera Chironidae
  • Le régime alimentaire de huit carabidés (Coleoptera) communs en milieu forestier. (The diet of eight carabid beetles common in forests)
  • Holocene paleoclimate and paleoecology determined from fossil Coleoptera at Brampton, Ontario, Canada
  • Implications of subfossil Coleoptera for the evolution of the Mima Mounds of Southwestern Puget lowland, Washington
  • Allerød - Younger Dryas Coleoptera from western Cape Breton Island, Nova Scotia, Canada
  • Invertebrate fossils (Insecta: Trichoptera, Diptera, Coleoptera) from the Pleistocene Scarborough formation at Toronto, Ontario, and their paleoenvironmental significance
  • , topography, and ice flow. It is driven by an imposed pattern of temperature change. The model is able to predict effectively the extent and thickness of the Loch Lomond ice sheet, using a palaeotemperature curve based on Coleoptera assemblages.
  • This paper describes teeth and bone fragments recovered from the peaty deposit during a search for coleopterain remains. The paper also summarises some of the Coleoptera and plant remains previously described and comments on the ecological
  • A total of 26.826 insect larvae and pupae were collected from 13 sampling areas in a polluted brook-pond system, locally treated by aeration. 106 species were collected: 1 Ephemeroptera, 4 Coleoptera and 101 Diptera. The Chironomidae dominated
  • Late-glacial climate and ecology of a kettle section at Brampton, Ontario, Canada, as determined from fossil coleoptera
  • Late-glacial (Allerød - Younger Dryas) Coleoptera from central Cape Breton Island, Nova Scotia, Canada
  • Allemagne de l'Ouest ; Baden-Wurttemberg ; Calcicole ; Coleoptera ; Diptera ; Ecologie ; Ecologie animale ; Ecologie végétale ; Fleur entomophile ; Formation herbacée ; Géographie de l'Europe ; Hymenoptera ; Insecte butineur ; Kaiserstuhl
  • plantes entomophiles et des insectes butineurs (Hymenoptera, Lepidoptera, Diptera et Coleoptera) est présentée en détail. Les espèces prairiales commencent à fleurir fin juillet, alors que les espèces d'ourlets fleurissent au second semestre.
  • and abundant plant macrofossils. Coleoptera were represented by 24 families. Several major beetle groups indicate a riffle-and-pool stream, surrounded by marsh, with open riparian habitats and nearby trees. Two zones were recognized. The Zone 1 fauna (ca