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Eoparisocrinid crinoids from the Middle Ordovician (Galena Group) of northern Iowa and southern Minnesota

Published online by Cambridge University Press:  20 May 2016

James C. Brower*
Affiliation:
Heroy Geology Laboratory, Syracuse University, Syracuse, New York 13244-1070

Abstract

Two species of eoparisocrinid crinoids from the Middle Ordovician Galena Group of northern Iowa and southern Minnesota are described, namely Eoparisocrinus crossmani n. sp. and E. grandei n. sp. The post-larval development of Eoparisocrinus crossmani is examined. Crinoid arms grow by addition of new plates at their distal tips in conjunction with calcite deposition on old plates. New branches appear where axillary plates are initiated. Consequently, the growth rates for number of brachials and length of food-gathering system compared to crown volume are much faster than if the animals were isometric. The number of food particles collected is related to the number of food-catching tube-feet, which can be estimated if the length of the arms and height of the covering plates are known. The size of the largest food item is constrained by the food groove width. Thus, food-gathering capacity is the number of food-catching tube-feet multiplied by food groove width. The food-gathering capacity increases more rapidly than if the animal grew isometrically, and the ratio of food-gathering capacity: crown volume only declines slightly over the known growth range. All Ordovician cladid crinoids examined follow nearly identical ontogenetic trajectories. The ecological niche of a stalked crinoid is related to four basic parameters: stem length, food groove width, tube-foot spacing, and branch density. Stem length limits the highest elevation above the seafloor. The column of E. crossmani becomes longer during ontogeny due to the formation of new columnals and height growth of old ones. Consequently, individuals gradually “move up” until the adult elevation of about 50 mm is reached. The growth rates of stem length relative to crown size are slow in the youngest and mature animals but rapid in juveniles. The food grooves become wider throughout growth so that older crinoids ate larger food particles than younger ones. The food groove width increases less rapidly than if the shape were constant, because distal plates and branches are more narrow and have more slender food grooves than proximal plates. Growth curves for food groove width versus stem length and elevation were generated for E. crossmani and other crinoids that commonly occur in the same beds. Together, elevation and food particle size define the main dimensions of the niche. The various taxa are more or less separated by different food groove widths at most comparable elevations. This pattern minimizes ecological overlap and probably competition between the different species. The tube-foot spacing of E. crossmani is constant regardless of size, which suggests that it employed the same type of feeding mechanism throughout post-larval ontogeny. The arm branches of adults gradually become less densely spaced relative to the area of water filtered than in juveniles.

Type
Research Article
Copyright
Copyright © The Paleontological Society 

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References

Ausich, W. I. 1980. A model for differentiation in lower Mississippian crinoid communities. Journal of Paleontology, 54:273288.Google Scholar
Ausich, W. I. 1986. Early Silurian inadunate crinoids (Brassfield Formation, Ohio). Journal of Paleontology, 60:719735.Google Scholar
Bassler, R. S. 1938. Pelmatozoa Palaeozoica, Pt. 83, p. 1194. In Quenstedt, W.(ed.), Fossilium Catalogus, I: Animalia. W. Junk, The Hague.Google Scholar
Bather, F. A. 1890. British fossil crinoids: II. The classification of the Inadunata Fistulata (cont'd). Annals and Magazine of Natural History, Series 6, 5:373388, 485–186.Google Scholar
Bather, F. A. 1893. The Crinoidea of Gotland, Part 1, The Crinoidea Inadunata. Kongl Svenska Vetenskaps Akademiens Handlinger, Bandet, 25(2):1200.Google Scholar
Bather, F. A. 1899. A phylogenetic classification of the Pelmatozoa. British Association for the Advancement of Science, Report for 1898:916922.Google Scholar
Billings, W. R. 1885. Two new species of crinoids. Transactions, Ottawa Field Naturalists' Club, 6(2):127129.Google Scholar
Brower, J. C. 1973. Crinoids from the Girardeau Limestone (Ordovician). Palaeontographica Americana, 7:261499.Google Scholar
Brower, J. C. 1974. Ontogeny of camerate crinoids. University of Kansas Paleontological Contributions, Paper, 72:153.Google Scholar
Brower, J. C. 1978. Postlarval ontogeny of fossil crinoids, camerates, p. T244T263. In Moore, R. C. and Teichert, C. 1978 (ed.), Treatise on Invertebrate Paleontology, Pt. T, Echinodermata 2. Geological Society of America and University of Kansas Press, Lawrence.Google Scholar
Brower, J. C. 1987. The relations between allometry, phylogeny and functional morphology in some calceocrinid crinoids. Journal of Paleontology, 61:9991032.Google Scholar
Brower, J. C. 1992a. Cupulocrinid crinoids from the Middle Ordovician (Galena Group, Dunleith Formation) of northern Iowa and southern Minnesota. Journal of Paleontology, 66:99128.CrossRefGoogle Scholar
Brower, J. C. 1992b. Hybocrinid and disparid crinoids from the Middle Ordovician (Galena Group, Dunleith Formation) of northern Iowa and southern Minnesota. Journal of Paleontology, 66:973993.Google Scholar
Brower, J. C. 1994. Camerate crinoids from the Middle Ordovician (Galena Group, Dunleith Formation) of northern Iowa and southern Minnesota. Journal of Paleontology, 68:570599.Google Scholar
Brower, J. C., and Strimple, H. L. 1983. Ordovician calceocrinids from northern Iowa and southern Minnesota. Journal of Paleontology, 57:12611281.Google Scholar
Brower, J. C., and Veinus, J. 1975. Ontogeny of Hybocrinus punctatus (Miller and Gurley), an Ordovician crinoid. Mathematical Geology, 7:129147.CrossRefGoogle Scholar
Brower, J. C., and Veinus, J. 1978. Middle Ordovician crinoids from the Twin Cities area of Minnesota. Bulletins of American Paleontology, 74(304):372506.Google Scholar
Brower, J. C., and Veinus, J. 1982. Phylogeny of primitive calceocrinids. University of Kansas Paleontological Contributions, Monograph, 1:90110.Google Scholar
Byrne, M., and Fontaine, A. R. 1981. The feeding behaviour of Florometra serratissma (Echinodermata: Crinoidea). Canadian Journal of Zoology, 59:1118.Google Scholar
Byrne, M., and Fontaine, A. R. 1983. Morphology and function of the tube-feet of Florometra serratissma (Echinodermata: Crinoidea). Zoomorphology, 102:175187.CrossRefGoogle Scholar
Causton, D. R. 1977. A Biologist's Mathematics. Edward Arnold, London, 326 p.Google Scholar
Clark, A. H. 1921. A monograph of the existing crinoids, Volume 1, the comatulids, Pt. 2. U.S. National Museum, Bulletin 82, 795 p.Google Scholar
Draper, N., and Smith, H. 1981. Applied Regression Analysis, 2nd edition. John Wiley & Sons, New York, 709 p.Google Scholar
Hall, J. 1882. Descriptions of the species of fossils found in the Niagara Group at Waldron, Indiana. Indiana Department of Geology and Natural History, Annual Report 11:217345.Google Scholar
Haugh, B. N. 1979. Late Ordovician channel-dwelling crinoids from southern Ontario, Canada. American Museum Novitates, Number 2665, 25 p.Google Scholar
Holland, N. D., Strickler, J. R., and Leonard, A. B. 1986. Particle interception, transport and rejection by the feather star Oligometra serripinna (Echinodermata: Crinoidea), studied by frame analysis of videotapes. Marine Biology, 93:111126.CrossRefGoogle Scholar
Jobson, L., and Paul, C. R. C. 1979. Compagicrinus fenestratus, a new Lower Ordovician inadunate crinoid from North Greenland. Rapport Grønlands geologiske Undersøglese, 91:7181.Google Scholar
Kammer, T. W. 1985. Aerosol filtration theory applied to Mississippian deltaic crinoids. Journal of Paleontology, 59:551560.Google Scholar
Kammer, T. W., and Ausich, W. I. 1987. Aerosol suspension feeding and current velocities: distributional controls for late Osagean crinoids. Paleobiology, 13:379395.Google Scholar
Kolata, D. R., Brower, J. C., and Frest, T. J. 1987. Upper Mississippi Valley Champlainian and Cincinnatian echinoderms. Minnesota Geological Survey, Report of Investigations, 35:179181.Google Scholar
Kolata, D. R., Strimple, H. L., and Levorson, C. O. 1977. Revision of the Ordovician carpoid family Iowacystidae. Palaeontology, 20:529557.Google Scholar
Leonard, A. B. 1989. Functional response in Antedon mediterranea (Lamarck) (Echinodermata: Crinoidea): the interaction of prey concentration and current velocity on a passive suspension-feeder. Journal of Experimental Marine Biology and Ecology, 127:81103.Google Scholar
Leonard, A. B., Strickler, J. R., and Holland, N. D. 1988. Effects of current speed on suspension feeding in Oligometra serripinna (Echinodermata: Crinoidea). Marine Biology, 97:111125.Google Scholar
Levorson, C. O., and Gerk, A. J. 1972a. A preliminary stratigraphic study of the Galena Group in Winneshiek, County, Iowa. Iowa Academy of Science Proceedings, 79:6375.Google Scholar
Levorson, C. O., and Gerk, A. J. 1972b. Revision of Galena stratigraphy. Geological Society of Iowa Field Trip Guidebook for 1972, 10 p.Google Scholar
Levorson, C. O., and Gerk, A. J. 1975. Field recognition of subdivision of the Galena Group within Winneshiek County. Guidebook for Field Gathering in Iowa, Minnesota, and Wisconsin Academies of Science, 1975:117.Google Scholar
Levorson, C. O., and Gerk, A. J. 1983. Field recognition of stratigraphic position within the Galena Group of northeast Iowa (limestone facies), p. C1C11. In Delgado, D. J. (ed.), Ordovician Galena Group of the Upper Mississippi Valley—deposition, diagenesis, and paleoecology. Society of Economic Paleontologists and Mineralogists, Great Lakes Section, 13th Annual Field Conference, 1983, Guidebook.Google Scholar
Levorson, C. O., Sloan, R. E., and Bisagno, L. A. 1987. General section of the Middle and Late Ordovician strata of northeastern Iowa. Minnesota Geological Survey, Report of Investigations, 35:2539.Google Scholar
Meyer, D. L. 1979. Length and spacing of the tube feet in crinoids (Echinodermata) and their role in suspension feeding. Marine Biology, 51:361369.Google Scholar
Meyer, D. L. 1982. Food and feeding mechanisms: Crinozoa, p. 2542. In Jangoux, M. and Lawrence, J. M. (eds.), Echinoderm Nutrition. A. A. Balkema, Rotterdam.Google Scholar
Meyer, D. L., and Ausich, W. I. 1983. Biotic interactions among Recent and among fossil crinoids, p. 377427. In Tevesz, M. J. S. and McCall, P. L. (eds.), Biotic Interactions in Recent and Fossil Benthic Communities. Plenum Press, New York and London.Google Scholar
Meyer, D. L., LaHaye, C. A., Holland, N. D., Arneson, A. C., and Strickler, J. R. 1984. Time-lapse cinematography of feather stars (Echinodermata: Crinoidea) on the Great Barrier Reef, Australia: demonstrations of posture changes, locomotion, spawning and possible predation by fish. Marine Biology, 78:179184.Google Scholar
Miller, J. S. 1821. A Natural History of the Crinoidea or Lily-Shaped Animals, with Observation on the Genera Asteria, Euryale, Comatula, and Marsupites. Bryan & Company, Bristol, 150 p.Google Scholar
Moore, R. C. 1962. Ray structures of some inadunate crinoids. University of Kansas Paleontological Contributions, Echinodermata, Article 5, 47 p.Google Scholar
Moore, R. C., and Laudon, L. R. 1943. Evolution and classification of Paleozoic crinoids. Geological Society of America, Special Paper 46, 167 p.Google Scholar
Parsley, R. L. 1970. Revision of the North American Pleurocystitidae (Rhombifera–Cystoidea). Bulletins of American Paleontology, 28(260):135213.Google Scholar
Paul, C. R. C. 1967. The functional morphology and mode of life of the cystoid Pleurocystites E. Billings, 1854. Zoological Society of London, Symposium, 20:105121.Google Scholar
Paul, C. R. C. 1984. British Ordovician cystoids, Pt. 2. Palaeontographical Society, London, Monograph, 136 (563):65152.Google Scholar
Springer, F. 1911. On a Trenton echinoderm fauna at Kirkfield, Ontario. Canada Geological Survey, Memoir 15-P:150.Google Scholar
Springer, F. 1926. American Silurian crinoids. Smithsonian Publication, 2871:1143, 167–239.Google Scholar
Templeton, J. S., and Willman, H. B. 1963. Champlainian Series (Middle Ordovician) in Illinois. Illinois State Geological Survey Bulletin, 89:1260.Google Scholar
Ubaghs, G. 1969. Aethocrinus moorei Ubaghs, n. gen., n. sp., le plus ancien crinoïde dicyclique connu. University of Kansas Paleontological Contributions, Paper 38, 25 p.Google Scholar
Ubaghs, G. 1978. Skeletal morphology of fossil crinoids, p. T58T216. In Moore, R. C. and Teichert, C.1978 (eds.), Treatise on Invertebrate Paleontology, Pt. T, Echinodermata 2. Geological Society of America and University of Kansas Press, Lawrence.Google Scholar
Wachsmuth, C., and Springer, F. 1885. Revision of the Palaeocrinoidea, Pt. 3, Sec. 1. Discussion of the classification and relations of the brachiate crinoids, and conclusion of the generic descriptions. Academy of Natural Sciences, Philadelphia, Proceedings for 1885:223364(1–162).Google Scholar
Weller, S. 1900. The paleontology of the Niagara Limestone in the Chicago Area, the Crinoidea. Chicago Academy of Sciences, Bulletin 4, Part I of the Natural History Survey, 153 p.Google Scholar