Hostname: page-component-84b7d79bbc-l82ql Total loading time: 0 Render date: 2024-07-26T20:07:53.171Z Has data issue: false hasContentIssue false
  • English
  • Français

Trace Fossils in Quaternary, Bahamian-Style Carbonate Environments: The Modern to Fossil Transition

Published online by Cambridge University Press:  17 July 2017

H. Allen Curran
H. Allen Curran*
Affiliation:
Department of Geology, Smith College, Northampton, Massachusetts 01063
Get access Rights & Permissions [Opens in a new window]

Extract

Tracemaking organisms are common and diverse components of the fauna and flora of tropical, shallow-marine and coastal carbonate environments. In the shallow subtidal zone, the burrowing activity of callianassid shrimp commonly is the dominant process in the modification of original depositional fabrics (Tudhope and Scoffin, 1984; Tedesco and Wanless, 1991). Both borers and burrowers have great potential to leave their mark in tropical carbonate sediments and rocks and to become part of the fossil record.

Type
Research Article
Information
Short Courses in Paleontology , Volume 5: Trace Fossils , 1992 , pp. 105 - 120
Copyright
Copyright © 1992 Paleontological Society 

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Basan, P.B. 1978. Introduction, p. 1–12. In Basan, P.B. (ed.), Trace Fossil Concepts. Society of Economic Paleontologists and Mineralogists Short Course Notes, No. 5.Google Scholar
Braithwaite, C.J.R., and Talbot, M.R. 1972. Crustacean burrows in the Seychelles, Indian Ocean. Palaeogeography, Palaeoclimatology, Palaeoecology, 11:265–285.Google Scholar
Bromley, R.G. 1990. Trace Fossils. Unwin Hyman, London, 280 p.Google Scholar
Curran, H.A. 1984. Ichnology of Pleistocene carbonates on San Salvador, Bahamas. Journal of Paleontology, 58:146–159.Google Scholar
Curran, H.A., 1990. Trace fossils as sea-level indicators: Examples from the Bahamas and Bermuda, p. 115–116. Abstracts—papers—13th International Sedimentological Congress, Nottingham.Google Scholar
Curran, H.A., and Dill, R.F. 1991. The stratigraphy and ichnology of a submarine cave in the Exuma Cays, Bahamas, p. 57–64. In Bain, R.J. (ed.), Proceedings of the Fifth Symposium on the Geology of the Bahamas. Bahamian Field Station, San Salvador Island.Google Scholar
Curran, H.A., and White, B. 1987. Trace fossils in carbonate upper beach rocks and eolianites: Recognition of the backshore to dune transition, p. 243–254. In Curran, H.A. (ed.), Proceedings of the Third Symposium on the Geology of the Bahamas. CCFL Bahamian Field Station, Ft. Lauderdale, Florida.Google Scholar
Curran, H.A., and White, B. 1991. Trace fossils of shallow subtidal to dunal ichnofacies in Bahamian Quaternary carbonates. Palaios, 6:498–510.Google Scholar
Ekdale, A.A., Bromley, R.G., and Pemberton, S.G. 1984. Ichnology: The Use of Trace Fossils in Sedimentology and Stratigraphy. SEPM Short Course No. 15, Society of Economic Paleontologists and Mineralogists, Tulsa, 317 p.Google Scholar
Förster, R., and Barthel, K.W. 1978. On recent and fossil Thalassina (Decapoda, Crustacea) and their burrows. Neues Jahrbuch für Geologie and Paläontolgie, Monatshefte, 5:291–306.Google Scholar
Frey, R.W., and Mayou, T.V. 1971. Decapod burrows in Holocene barrier island beaches and washover fans, Georgia. Senckenbergiana Maritima, 3:53–77.Google Scholar
Frey, R.W., and Pemberton, S.G. 1987. The Psilonichnus ichnocoenose, and its relationship to adjacent marine and nonmarine ichnocoenoses along the Georgia coast. Bulletin of Canadian Petroleum Geology, 35:333–357.Google Scholar
Frey, R.W., Howard, J.D., and Pryor, W.A. 1978. Ophiomorpha: Its morphologic, taxonomic, and environmental significance. Palaeogeography, Palaeoclimatology, Palaeoecology, 23:199–299.Google Scholar
Frey, R.W., Curran, H.A., and Pemberton, S.G. 1984. Tracemaking activities of crabs and their significance: the ichnogenus Psilonichnus . Journal of Paleontology, 58:333–350.Google Scholar
Garrett, P. 1977. Biological communities and their sedimentary record, p. 124–158. In Hardie, L.A. (ed.), Sedimentation on the Modern Carbonate Tidal Flats of Northwest Andros Island, Bahamas. The John Hopkins University Studies in Geology, No. 22.Google Scholar
Griffis, R.B., and Suchanek, T.H. 1991. A model of burrow architecture and trophic modes in thalassinidean shrimp (Decapoda: Thalassinidea). Marine Ecology Progress Series, 79:171–183.Google Scholar
Halley, R.B., and Evans, C.C. 1983. The Miami Limestone: A Guide to Selected Outcrops and Their Interpretation. Miami Geological Society, Miami, 67 p.Google Scholar
Jones, B., and Pemberton, S.G. 1989. Sedimentology and ichnology of a Pleistocene unconformity-bounded, shallowing-upward carbonate sequence: the Ironshore Formation, Salt Creek, Grand Cayman. Palaios, 4:343–355.Google Scholar
Miller, M.F., Ekdale, A.A., and Picard, M.D. (eds.). 1984. Trace Fossils and Paleoenvironments: Marine Carbonate, Marginal Marine Terrigenous and Continental Terrigenous Settings. Journal of Paleontology 58:283–593.Google Scholar
Pemberton, S.G., and Jones, B. 1988. Ichnology of the Pleistocene Ironshore Formation, Grand Cayman Island, British West Indies. Journal of Paleontology, 62:495–505.Google Scholar
Perkins, R.D. 1977. Depositional framework of Pleistocene rocks in South Florida, p. 141–198. In Enos, P., and Perkins, R.D. (eds.), Quaternary Sedimentation in South Florida. Geological Society of America Memoir 147.Google Scholar
Shinn, E. A. 1968. Burrowing in Recent lime mud sediments of Florida and the Bahamas. Journal of Paleontology, 42:879–894.Google Scholar
Tedesco, L.P., and Wanless, H.R. 1991. Generation of sedimentary fabrics and facies by repetitive excavation and storm infilling of burrow networks, Holocene of South Florida and Caicos Platform, B.W.I. Palaios, 6:326–343.Google Scholar
Tudhope, A.W. and Scoffin, T.P. 1984. The effects of Callianassa bioturbation on the preservation of carbonate grains in Davies Reef Lagoon, Great Barrier Reef, Australia. Journal of Sedimentary Petrology, 54:1091–1096.Google Scholar
Wanless, H.R., Tedesco, L.P., and Tyrrell, K.M. 1988. Production of subtidal tubular and surficial tempestites by Hurricane Kate, Caicos Platform, British West Indies. Journal of Sedimentary Petrology, 58:739–750.Google Scholar
White, B., and Curran, H.A. 1987. Coral reef to eolianite transition in the Pleistocene rocks of Great Inagua Island, Bahamas, p. 165–179. In Curran, H.A. (ed.), Proceedings of the Third Symposium on the Geology of the Bahamas. CCFL Bahamian Field Station, Ft. Lauderdale, Florida.Google Scholar
White, B., and Curran, H.A. 1988. Mesoscale physical sedimentary structures and trace fossils in Holocene carbonate eolianites from San Salvador Island, Bahamas. Sedimentary Geology, 55:163–184.Google Scholar
Wolcott, T.G., and Wolcott, D.L. 1990. Wet behind the gills. Natural History. 10/90:47–54.Google Scholar