Download Continental Trace Fossils (SEPM Short Course Notes 51) by Stephen T. Hasiotis PDF

By Stephen T. Hasiotis

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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.

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