1970
DOI: 10.1146/annurev.en.15.010170.000525
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Interpretations of Quaternary Insect Fossils

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Cited by 130 publications
(57 citation statements)
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“…Fossil findings show that insects also had to react to climatic changes in the past (Coope, 1970(Coope, , 1987(Coope, , 1995McGavin, 1994;Ashworth, 1997). Wilf and Labandeira (1999) observed increased damage intensity, frequency and diversity on late Paleocene host plant leaves in Southwest Wyoming.…”
Section: Horizontal Changes In the Range Of Distributionmentioning
confidence: 99%
“…Fossil findings show that insects also had to react to climatic changes in the past (Coope, 1970(Coope, , 1987(Coope, , 1995McGavin, 1994;Ashworth, 1997). Wilf and Labandeira (1999) observed increased damage intensity, frequency and diversity on late Paleocene host plant leaves in Southwest Wyoming.…”
Section: Horizontal Changes In the Range Of Distributionmentioning
confidence: 99%
“…DOI: 10.1038/sj/hdy/6800003 species can be studied by analysing pollen (eg, Huntley and Birks, 1983;Gliemeroth, 1995). For animals, sufficient remains only exist for some groups, such as beetles or terrestrial gastropods (eg, Coope, 1970Coope, , 1994Hertelendy et al, 1992); for the great majority of invertebrates, hardly any evidence of this kind is available.…”
Section: Expansions Of Treementioning
confidence: 99%
“…The climate during the last ice-age, the Wü rm, being totally different from today (eg, Frenzel et al, 1992), forced nearly all plant and animal species to change their European distribution ranges (Huntley and Birks, 1983;Gliemeroth, 1995;Hewitt, 1996Hewitt, , 1999Taberlet et al, 1998;Comes and Kadereit, 1999). Species thought to have been widely distributed throughout Central Europe during the ice-ages, only survive in alpine or tundral relict areas (Coope, 1970(Coope, , 1994Varga, 1977). Thermophilic species were restricted to the more temperate regions of the Mediterranean during glaciations (Hewitt, 1996).…”
Section: Introductionmentioning
confidence: 99%
“…There is much available evidence that evolution of new species is a slow process, compared with the human timp scale, and it is thus likely that the species assemblages of European broadleaved woodlands have originated over a long period of time (see West 1968;Coope 1970) stretching back beyond the Interglacials into the later Pliocene period at least.…”
Section: Woodland Structurementioning
confidence: 99%