Ld. Martin et Dl. West, THE RECOGNITION AND USE OF DERMESTID (INSECTA, COLEOPTERA) PUPATION CHAMBERS IN PALEOECOLOGY, Palaeogeography, palaeoclimatology, palaeoecology, 113(2-4), 1995, pp. 303-310
Insect trace fossils are a relatively new source of climatic and tapho
nomic data. Because insects often have narrowly defined ecological req
uirements during their life cycle, they can be an exceptional source o
f data on season of death, temperature and moisture. We have found thi
s to be true for dermestid pupation chambers and give three examples f
rom the late Pliocene of Idaho and middle-late Pleistocene of Kansas.