By Stephen T. Hasiotis
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Extra info for Continental Trace Fossils (SEPM Short Course Notes 51)
Kocurek, 1981). An important note is that when erg systems encroach areas of high water tables, wet interdunes may be abundant early in the record of that system. , 1978; Collinson, 1986b). , Ardo, 1957; Hill and Hunter, 1976; Fouch and Dean, 1982; Skiba and Wainwright, 1984; Cloudsley-Thompson, 1987; McLachlan, 1991). These dune fields are ecologically differentiated into three groups: (1) transitional zone dunes, (2) coastal-bound dunes (slipfaces affected by spray, fog, and large storms), and (3) terrabound dunes and interdunes (affected by fog and precipitation).
Kent, D. , Witte, W. , and Schlische, R. 1996. High-resolution stratigraphy of the Newark rift basin (early Mesozoic, eastern North America). Geological Society of America Bulletin, 108:40-77. Pemberton, S. G. 1992. Applications of ichnology to petroleum exploration: A core workshop. SEPM Core Workshop No. 17, 429 p. Pemberton, S. , MacEachern, J. , and Frey, R. W. 1992. Trace fossil facies models. In Walker, R. G. and James, N. , Facies Models, Geological Association of Canada, Geoscience Canada Reprint Series 1, p.
Effects of soil temperature and moisture on the vertical distribution of European chafer larvae. Ann. Ent. Soc. , 53:666-670. Silvey, J. K. G. 1936. An investigation of the burrowing inner-beach insects of some fresh-water lakes. Mich. Acad. Sci. , 21:655-696. Skiba, U. and Wainwright, M. 1984. Nitrogen transformation in coastal sands and dune soils. Journ. , 7:1-8. Smith, R. M. H. 1987. Helical burrow casts of therapsid origin from the Beaufort Group (Permian) of South Africa. Palaeogeography, Palaeoclimatology, Palaeoecology, 60:155-170.