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Revision of lyracystid eocrinoids from the Middle Cambrian of South China and Western Laurentia

Published online by Cambridge University Press:  14 July 2015

James Sprinkle
Affiliation:
1Department of Geological Sciences, Jackson School of Geosciences, University of Texas, Austin, Texas 78712-0254 USA,
Ronald L. Parsley
Affiliation:
2Department of Earth and Environmental Sciences, Tulane University, New Orleans, Louisiana 70118 USA,
Yuanlong Zhao
Affiliation:
3Institute of Paleontology and Biomineralization, School of Resources and Environment, Guizhou University, Guiyang, China 550003,
Jin Peng
Affiliation:
3Institute of Paleontology and Biomineralization, School of Resources and Environment, Guizhou University, Guiyang, China 550003,

Abstract

The Middle Cambrian eocrinoid genera Lyracystis Sprinkle and Collins, 2006, from western Laurentia and Balangicystis Parsley and Zhao, 2006, from South China, described in the same year, have turned out to be closely related genera assigned to the Family Lyracystidae. Both have erect, lyre-shaped, arm-like, brachiolebearing, feeding appendages, here termed exothecal ambulacra, that are not homologous to crinoid arms. They also have a long, multiplated stalk to elevate the theca and feeding appendages well above the sea floor, making them among the highest tiered echinoderm suspension feeders known from the Middle Cambrian. The long stalk was either inserted a short distance into the muddy sediment, or attached to rare skeletal fragments lying on the sea floor. Both genera seem well adapted to quiet-water or slow-current conditions in deeper water (150-200 m) on the outer shelf or upper slope of their respective continents.

Type
Research Article
Copyright
Copyright © The Paleontological Society 

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References

Baumiller, T. K. 1992. Importance of hydrodynamic lift to crinoid autecology, or could crinoids function as kites? Journal of Paleontology, 66:658665.CrossRefGoogle Scholar
Branson, E. B. and Peck, R. E.. 1940. A new cystoid from the Ordovician of Oklahoma. Journal of Paleontology, 14:8992.Google Scholar
Broadhead, T. W. 1982. Reappraisal of Class Eocrinoidea (Echinodermata), p. 125131. In Lawrence, J. M. (ed.), International Echinoderms Conference, Tampa Bay. A.A. Balkema, Rotterdam.Google Scholar
Guensburg, T. E. and Sprinkle, J.. 2000 (2001). Ecologic radiation of Cambro-Ordovician echinoderms, p. 428444. In Zhuravlev, A. Y. and Riding, R. (eds.), The Ecology of the Cambrian Radiation. Columbia University Press, New York.CrossRefGoogle Scholar
Jaekel, O. 1918. Phylogenie und system der Pelmatozoen. Palaontologische Zeitschrift, 3:1128.CrossRefGoogle Scholar
Lin, J.-P., Ausich, W. I., Zhao, Y.-L., and Peng, J.. 2008. Taphonomy, paleoecological implications, and colouration of Cambrian gogiid echinoderms from Guizhou Province, China. Geological Magazine, 145:1736.CrossRefGoogle Scholar
Parsley, R. L. 1982. Eumorphocystis, p. 280288. In Sprinkle, J. (ed.), Echinoderm Faunas from the Bromide Formation (Middle Ordovician) of Oklahoma. University of Kansas Paleontological Contributions, Monograph 1.Google Scholar
Parsley, R. L. and Prokop, R. J.. 2004. Functional morphology and paleoecology of some sessile Middle Cambrian echinoderms from the Barrandian region of Bohemia. Czech Geological Survey Bulletin of Geosciences, 79:147156.Google Scholar
Parsley, R. L. and Zhao, Y.-L.. 2006. Long stalked eocrinoids in the basal Middle Cambrian Kaili Biota, Taijiang County, Guizhou Province, China. Journal of Paleontology, 80:10581071.CrossRefGoogle Scholar
Sprinkle, J. 1973. Morphology and Evolution of Blastozoan Echinoderms. Harvard University Museum of Comparative Zoology, Special Publication, 283 p.Google Scholar
Sprinkle, J. 1976. Biostratigraphy and paleoecology of Cambrian echinoderms from the Rocky Mountains. Brigham Young University Geology Studies, 23(2):6173.Google Scholar
Sprinkle, J. 1992. Radiation of Echinodermata, p. 375398. In Lipps, J. H. and Signor, P. W. (eds.), Origin and Early Evolution of the Metazoa. Plenum Press, New York.CrossRefGoogle Scholar
Sprinkle, J. 1995. Do eocrinoids belong to the Cambrian or to the Paleozoic Evolutionary Fauna?, p. 397400. In Cooper, J. D., Droser, M. L., and Finney, S. C. (eds.), Ordovician Odyssey: Short Papers for the Seventh International Symposium on the Ordovician System. Pacific Section-Society for Sedimentary Geology (SEPM), Book 77.Google Scholar
Sprinkle, J. and Collins, D.. 2006. New eocrinoids from the Burgess Shale, southern British Columbia, Canada, and the Spence Shale, northern Utah, USA. Canadian Journal of Earth Sciences, 43:303322.CrossRefGoogle Scholar
Sumrall, C. D. 1997. The role of fossils in the phylogenetic reconstruction of Echinodermata, p. 267288. In Waters, J. A. and Maples, C. G. (eds.), Geobiology of Echinoderms. Paleontological Society Papers, Vol. 3.Google Scholar
Sumrall, C. D. and Wray, G. A.. 2007. Ontogeny in the fossil record: diversification of body plans and the evolution of “aberrant” symmetry in Paleozoic echinoderms. Paleobiology, 33:149163.CrossRefGoogle Scholar
Zhao, Y.-L., Huang, Y.-Z., and Gong, X.-Y.. 1994. Echinoderm fossils of Kaili Fauna from Taijiang, Guizhou. Acta Palaeontologica Sinica, 33(3):305324. (In Chinese)Google Scholar
Zhao, Y.-L., Parsley, R. L., and Peng, J.. 2007. Early Cambrian eocrinoids from Guizhou Province, South China. Palaeogeography, Palaeoclimatology, Palaeoecology, 254:317327.CrossRefGoogle Scholar
Zhao, Y.-L., Parsley, R. L., and Peng, J.. 2008. Basal Middle Cambrian short-stalked eocrinoids from the Kaili Biota: Guizhou Province, China. Journal of Paleontology, 82:415422.CrossRefGoogle Scholar
Zhao, Y.-L., Yang, R.-D., Yuan, J.-L., Zhu, M.-Y., Guo, Q.-J., Yang, X.-L., and Tai, T.-S.. 2001. Cambrian stratigraphy at Balang, Guizhou Province, China: Candidate section for a global unnamed series and stratotype section for the Taijiangian Stage, p. 189208. In Peng, S.-C., Babcock, L. E., and Zhu, M.-Y. (eds.), Cambrian System of South China. (Palaeoworld, No. 13). Press of University of Science and Technology of China, Hefei.Google Scholar
Zhao, Y.-L., Yuan, J.-L., Zhu, M.-Y., Yang, R.-D., Guo, Q.-J., Qian, Y., Huang, Y.-Z., and Pan, Y.. 1999. A progress report on research on the early Middle Cambrian Kaili Biota, Guizhou, PRC. Acta Palaeotologica Sinica, 38(Supplement):114. (In Chinese)Google Scholar
Zhao, Y.-L., Zhu, M.-Y., Babcock, L. E., Yuan, J.-L., Parsley, R. L., Peng, J., Yang, X.-L., and Wang, Y.. 2005. Kaili Lagerstätte—a new Middle Cambrian Burgess Shale-type lagerstätten. Geology of Guizhou, 13:105114.Google Scholar
Zhu, M.-Y., Erdtmann, B. D., and Zhao, Y.-L.. 1999. Taphonomy and paleoecology of the early Middle Cambrian Kaili Lagerstätte in Guizhou, China. Acta Palaeotologica Sinica, 38(Supplement):4757.Google Scholar