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Sinusoidal trail formed by a Recent biting midge (Family Ceratopogonidae): trace fossil implications

Published online by Cambridge University Press:  14 July 2015

Robert Metz
Robert Metz*
Affiliation:
Department of Geology and Meteorology, Kean College of New Jersey, Union 07083
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Abstract

A Recent sinusoidal trail made by a biting midge (family Ceratopogonidae, genus ?Bezzia) moving on the surface of wet mud along the edge of a freshwater pond has been observed. The trail is similar to the trace fossil Cochlichnus Hitchcock, 1858. The wave length, wave amplitude, and overall form and shape of this modern trail compares favorably to Eocene wave-like trails attributed to nematodes. Consequently, a ceratopogonid larva is believed responsible for at least some of those fossil trails.

Type
Research Article
Information
Journal of Paleontology , Volume 61 , Issue 2 , March 1987 , pp. 312 - 314
Copyright
Copyright © The Paleontological Society 

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References

Carpenter, F. M. 1953. The geological history and evolution of insects. American Scientist, 41:256–270.Google Scholar
Crimes, T. P. and Anderson, M. M. 1985. Trace fossils from Late Precambrian–Early Cambrian strata of southeastern Newfoundland (Canada): temporal and environmental implications. Journal of Paleontology, 59:310–343.Google Scholar
Eagar, R. M. C. et al. 1985. Trace fossil assemblages and their occurrence in Silesian (Mid-Carboniferous) deltaic sediments of the Central Pennine Basin, England, p. 99–149. In Curran, H. A. (ed.), Biogenic Structures: Their Use in Interpreting Depositional Environments. Society of Economic Paleontologists and Mineralogists Special Publication, No. 35.Google Scholar
Emerson, B. K. 1898. Geology of old Hampshire County, Massachusetts. United States Geological Survey, Monograph 29, 790 p.Google Scholar
Hakes, W. G. 1976. Trace fossils and depositional environment of four clastic units, Upper Pennsylvanian megacyclothems, northeast Kansas. University of Kansas Paleontological Contributions, article 63, 46 p.Google Scholar
Hanley, J. H., Steidtman, J. R. and Toots, H. 1971. Trace fossils from the Casper Sandstone (Permian) southern Laramie Basin, Wyoming and Colorado. Journal of Sedimentary Petrology, 41:1065–1068.Google Scholar
Hitchcock, E. 1858. Ichnology of New England. A Report on the Sandstone of the Connecticut Valley, Especially Its Footprints. W. White, Boston, 220 p.Google Scholar
Moussa, M. T. 1966. Insect tracks? Entomology Society of America Bulletin, 12:377.Google Scholar
Moussa, M. T. 1968. Fossil tracks from the Green River Formation (Eocene) near Soldier Summit, Utah. Journal of Paleontology, 42:1433–1438.Google Scholar
Moussa, M. T. 1970. Nematode fossil trails from the Green River Formation (Eocene) in the Uinta Basin, Utah. Journal of Paleontology, 44:304–307.Google Scholar
Stanley, K. O. and Fagerstrom, J. A. 1974. Miocene invertebrate trace fossils from a braided river environment, western Nebraska, U.S.A. Palaeogeography, Palaeoclimatology, Palaeoecology, 15:63–82.CrossRefGoogle Scholar
Tarr, W. A. 1935. Concretions in the Champlain Formation of the Connecticut River Valley. Geological Society of America Bulletin, 46:1493–1534.CrossRefGoogle Scholar
Tevesz, M. J. S. and McCall, P. L. 1982. Geological significance of aquatic nonmarine trace fossils, p. 257–285. In McCall, P. L. and Tevesz, M. J. S. (eds.), Animal-Sediment Relations. Plenum, New York.CrossRefGoogle Scholar
Webby, B. D. 1970. Late Precambrian trace fossils from New South Wales. Lethaia, 3:79–109.CrossRefGoogle Scholar