The response of insect faunas to glacial-interglacial climatic fluctuations

1994 Philosophical Transactions of the Royal Society B Biological Sciences 158 citations

Abstract

The extinction of species of small invertebrates is difficult to recognize. However, in deposits that date from the past few million years, insect fossils are remarkably common and provide objective data on the history of the organisms that constitute the biotic communities of the present day. It might have been expected that the great climatic oscillations of the glacial-interglacial cycles should have caused widespread extinctions, if their effects on the large vertebrates is taken as our model. Yet the record of Quaternary fossil insects shows no high extinction rates during this period. Constancy of species and communities of species can be demonstrated to be the norm for at least the last million or so years (= generations). The enigma of how such constancy was sustained in the face of large-scale climatic fluctuations remains a puzzle though several possible solutions are suggested. These solutions carry implications for our estimates of present and future extinction rates.

Keywords

InterglacialGlacial periodEcologyExtinction (optical mineralogy)FaunaInvertebrateClimate changeExtinction eventEctothermQuaternaryPaleontologyBiologyGeographyPopulationBiological dispersal

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Year
1994
Type
article
Volume
344
Issue
1307
Pages
19-26
Citations
158
Access
Closed

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G. Russell Coope (1994). The response of insect faunas to glacial-interglacial climatic fluctuations. Philosophical Transactions of the Royal Society B Biological Sciences , 344 (1307) , 19-26. https://doi.org/10.1098/rstb.1994.0046

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DOI
10.1098/rstb.1994.0046