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Secondary tiering on crinoids from the Waldron Shale (Silurian: Wenlockian) of Indiana

Published online by Cambridge University Press:  14 July 2015

Shanan E. Peters  and
Kennard B. Bork
Shanan E. Peters
Affiliation:
Department of Geology and Geography, Denison University, Granville, Ohio 43023,
Kennard B. Bork
Affiliation:
Department of Geology and Geography, Denison University, Granville, Ohio 43023,
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Abstract

Superbly preserved specimens of Eucalyptocrinites tuberculatus from the Waldron Shale (Silurian, Wenlockian) of Indiana have been found with epibionts attached in living position to their stems. The rhynchonellid brachiopod Stegerhynchus indianense, the tabulate coral Favosites forbesi, the annelids? Spirorbis and Cornulites, bryozoans, and rarely the ichnogenus Tremichnus utilized living crinoids as secondary tiering surfaces. Crinozoans also attached to upright crinoid columns, and their holdfasts are the most abundant epibionts on pluricolumnals. Eucalyptocrinites crassus individuals contributed to the success of their epibionts by providing stable attachment surfaces elevated up to one meter above the sediment-water interface. Although crinoid-epibiont relationships are frequently blurred by taphonomic processes, articulated crinoid specimens and encrusters on pluricolumnals suggest that secondary tiering was a significant paleoecological element in the Waldron Shale.

Type
Research Article
Information
Journal of Paleontology , Volume 72 , Issue 5 , September 1998 , pp. 887 - 894
Copyright
Copyright © The Paleontological Society 

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References

Archer, A. W., and Feldman, H. R. 1989. Microbioherms of the Waldron Shale (Silurian, Indiana): implications for organic framework in Silurian reefs of the Great Lakes area. Palaios, 1:133–140.CrossRefGoogle Scholar
Ausich, W. I., and Bottjer, D. J. 1982. Tiering in suspension-feeding communities on soft substrata throughout the Phanerozoic. Science, 216:173–174.CrossRefGoogle ScholarPubMed
Baumiller, T. K., and Ausich, W. I. 1992. The broken-stick model as a null hypothesis for crinoid stalk taphonomy and as a guide to the distribution of connective tissue in fossils. Paleobiology, 18:288–298.CrossRefGoogle Scholar
Bottjer, D. J., and Ausich, W. I. 1986. Phanerozoic development of tiering in soft substrata suspension-feeding communities. Paleobiology, 12:400–420.CrossRefGoogle Scholar
Brett, C. E. 1981. Terminology and functional morphology of attachment structures in pelmatozoan echinoderms. Lethaia, 4:343–370.CrossRefGoogle Scholar
Brett, C. E. 1985. Tremichnus: a new ichnogenus of circular-parabolic pits in fossil echinoderms. Journal of Paleontology, 59:615–635.Google Scholar
Brett, C. E., and Baird, G. C. 1993. Taphonomic approaches to temporal resolution in stratigraphy: examples from Paleozoic marine mudrocks, p. 250–274. In Kidwell, S. M. and Behrensmeyer, A. K. (eds.), Taphonomic Approaches to Time Resolution in Fossil Assemblages. Paleontological Society Short Course Number 6.Google Scholar
Brett, C. E., and Eckert, J. D. 1982. Paleoecology of a well-preserved crinoid colony from the Silurian Rochester Shale in Ontario. Life Science Contribution, Royal Ontario Museum, 131, 20 p.Google Scholar
Bromley, R. G., and Surlyk, F. 1973. Borings produced by brachiopod pedicles, fossil and Recent. Lethaia, 6:349–365.CrossRefGoogle Scholar
Conkin, J. E., Conkin, B. M., Brown, J. H. III, Kubacko, J., and Fernane, E. 1992. The Middle Silurian Louisville Limestone of northwestern Kentucky and southern Indiana. University of Louisville Studies in Paleontology and Stratigraphy, 19, 62 p.Google Scholar
Feldman, H. R. 1986. Spatial distribution and taphonomy of fauna and paleoenvironmental parameters of the Waldron Shale (Silurian) in southeastern Indiana. Unpublished , , 249 p.Google Scholar
Feldman, H. R. 1989. Taphonomic processes in the Waldron Shale, Silurian, southern Indiana. Palaios, 4:144–156.CrossRefGoogle Scholar
Grant, R. E. 1963. Unusual attachment of a Permian linoproductid brachiopod. Journal of Paleontology, 37:134–140.Google Scholar
Grant, R. E. 1968. Structural adaptation in two Permian linoproductid genera, Salt Range, West Pakistan. Journal of Paleontology, 37:134–140.Google Scholar
Hall, J. 1863. Notice on some new species of fossils from a locality of the Niagara Group in Indiana. Transactions of the Albany Institute, p. 195–278.Google Scholar
Hall, J. 1881. Species of fossils found in the Niagara Group at Waldron, Indiana. Indiana Department of Geology and Natural History Eleventh Annual Report, p. 218–425.Google Scholar
Halleck, M. S. 1973. Crinoids, hardgrounds, and community succession: The Silurian Waldron-Laurel contact in southern Indiana. Lethaia, 6:239–252.CrossRefGoogle Scholar
Liddell, W. D., and Brett, C. E. 1982. Skeletal overgrowths among epizoans from the Silurian (Wenlockian) Waldron Shale. Paleobiology, 8:67–78.CrossRefGoogle Scholar
McGee, P. E., and Watkins, R. 1994. Epibiont tiering on Silurian crinoids in the Waldron Shale, Indiana. Geological Society of America Abstracts with Programs, 26(7):59.Google Scholar
Meyer, D. L., and Ausich, W. I. 1983. Biotic interactions among Recent and fossil crinoids, p. 377–427. In Tevesz, M. J. S. and McCall, P. L. (eds.), Biotic interactions in Recent and fossil benthic communities. Plenum Press, New York.CrossRefGoogle Scholar
Morris, R. W., and Felton, S. T. 1993. Symbiotic association of crinoids, platyceratid gastropods, and Cornulites in the Upper Ordovician (Cincinnatian) of the Cincinnati, Ohio Region. Palaios, 8:465–476.CrossRefGoogle Scholar
Richards, R. P. 1972. Autecology of Richmondian brachiopods (Late Ordovician of Indiana and Ohio). Journal of Paleontology, 46:386–405.Google Scholar
Richards, R. P. 1974. Ecology of the Cornulitidae. Journal of Paleontology, 48:514–523.Google Scholar
Rudwick, M. J. S. 1970. Living and Fossil Brachiopods. Hutchinson University Library, Hutchinson and Co. Ltd., London, 199 p.Google Scholar
Sandy, M. R. 1996. Oldest record of peduncular attachment of brachiopods to crinoid stems, Upper Ordovician, Ohio, U.S.A. Journal of Paleontology, 70:532–534.Google Scholar
Shaver, R. H., and Sunderman, J. A. 1989. Silurian seascapes: water depth, clinothems, reef geometry, and other motifs—a critical review of the Silurian reef model. Geological Society of America Bulletin, 101:939–951.2.3.CO;2>CrossRefGoogle Scholar
Taylor, W. L., and Brett, C. E. 1996. Taphonomy and paleoecology of echinoderm lagerstätten from the Silurian (Wenlockian) Rochester Shale. Palaios, 11:118–140.CrossRefGoogle Scholar
Watkins, R. 1991. Guild structure and tiering in a high-diversity Silurian community, Milwaukee, County, Wisconsin. Palaios, 6:465–478.CrossRefGoogle Scholar