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Preface

Published online by Cambridge University Press:  04 May 2010

David L. Denlinger
Affiliation:
Columbus, Ohio
Richard E. Lee Jr.
Affiliation:
Oxford, Ohio
David L. Denlinger
Affiliation:
Ohio State University
Richard E. Lee, Jr
Affiliation:
Miami University
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Summary

Tiny, wingless snow flea freezes

overnight as stiff as tin.

Does he mind or even notice

just what sort of state he's in?

Things warm up and – leaping lizards! –

Snow flea's jumping as before,

none the worse for being frozen

on the icy Arctic shore.

(Eileen Spinelli, 2007 Snow Flea)

Although the tilt of the earth's axis is only a little over 23o, this is enough to provide the dramatic contrast between the heat of summer and the cold of winter as our planet rotates around the sun. These pronounced seasonal changes in temperature dictate the seasonal patterns that dominate the temporal patterns of life on earth. On a much shorter timescale, the daily rotation of the earth on its axis, yielding the day/night cycle, adds the important dimension of thermoperiodism that generates daily variation in the number of heat units that reach the earth's surface.

Certainly all animals are influenced by daily and seasonal cycles of temperature, but it is perhaps ectotherms, such as insects, that are most severely affected. With, at best, limited abilities to regulate their own body temperature, insects are at the mercy of the prevailing temperatures. Insects commonly use seasonal shortening in day length (photoperiod) as an environmental token to reliably signal the advent of inimical temperatures. For many insects these photoperiodic cues are used to program diapause, a period of developmental arrest used to wait out the winter months.

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Publisher: Cambridge University Press
Print publication year: 2010

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