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

By Stephen T. Hasiotis

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Klappa, C. F. 1980. Rhizoliths in terrestrial carbonates: Classification, recognition, genesis and significance. , 27:613-629. Kocurek, G. 1981. Significance of interdune deposits and bounding surfaces in aeolian dune sands. , 28:753-780. Kraus, M. J. 1987. Integration of channel and floodplain suites, II. Vertical relations of alluvial paleosols. Journ. Sed. , 57:602-612. Lockley, M. G. 1991. Tracking dinosaurs: A new look at an ancient world. Cambridge University Press, New York, 238 p. 49 Lockley, M.

In modern settings, backfilled burrows rarely, if ever, are visible in the substrate. ) associated with the burrow (Hasiotis, 1997a). Crevasse-Splay Subenvironment Crevasse-splay complexes contain overprinted ichna of hydrophilic (high water table) and terraphilic (low water table) organisms. These depositional complexes are short-lived and dominant from the proximal to the distal floodplain, depending on flooding intensity. When crevasse-splay sediments are deposited, they are generally saturated.

And Harris, J. , eds. Laetoli: A Pliocene site in northern Tanzania. Sarjeant, W. A. S. ). 1983. Terrestrial Trace Fossils. Hutchinson Ross Publishing Company, Benchmark Papers in Geology, 76:415 p. Schaller, F. 1968. Soil Animals. University Michigan Press, Ann Arbor, 144 p. Scott, A. C. 1992. Trace fossils of plant-arthropod interactions, p. 197-223. In C. G. Maples, and R. R. ), Trace Fossils: Their paleobiological aspects, Paleontological Society Short Course, Number 5. , 1953. Uber die Methoden der Palichnologie, 1, Studien von Palichnologie.

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