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A new turban-shaped gogiid eocrinoid from the Kaili Formation (Kaili Biota), Balang, Jianhe County, Guizhou Province, China

Published online by Cambridge University Press:  11 August 2017

Ronald L. Parsley  and
Yuanlong Zhao
Ronald L. Parsley
Affiliation:
Department of Earth and Environmental Sciences, Tulane University, New Orleans, LA 70118,
Yuanlong Zhao
Affiliation:
College of Resource and Environmental Engineering of Guizhou University, Guiyang, 550003, China,
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Abstract

A rare new turban-shaped basal Middle Cambrian gogiid eocrinoid, Turbanicystis inflatus new genus and species is described from the Kaili Formation (Kaili Biota), Guizhou Province, China. It co-occurs with three other markedly different gogiids, Sinoeocrinus, Globoeocrinus, and Balangicystis, and is part of a unique Middle Cambrian community that is dominated by echinoderms.

Type
Research Article
Information
Journal of Paleontology , Volume 84 , Issue 3 , May 2010 , pp. 549 - 553
Copyright
Copyright © 2010, The Paleontological Society 

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References

Barrande, J. 1846. Notice préliminaire sur le systéme Silurien et les trilobites de la Bohême, p. 1–97. Leipzig.Google Scholar
Barrande, J. 1887. Classe des echinoderms. 1 Ordre des Cystidées. In Système Silurien du centre de la Bohême, 7: 233 p, Prague.Google Scholar
Bell, B. M. and Sprinkle, J. 1978. Totiglobus, an unusual new edrioasteroid from the Middle Cambrian of Nevada. Journal of Paleontology, 52: 243–266.Google Scholar
Broadhead, T.W. 1982. Reappraisal of the Class Eocrinoidea (Echinodermata), p. 125–131. In Lawrence, J. M. (ed.), Echinoderms: Proceedings of the International Conference, Tampa Bay. A.A. Balkema, Rotterdam.Google Scholar
Coyne, K., Qin, X., and Waite, J. 1997. Extensible collagen in mussel byssus: a natural block copolymer. Science, 277: 1830–1832.CrossRefGoogle ScholarPubMed
Durham, J. W. 1978. A Lower Cambrian eocrinoid. Journal of Paleontology, 52: 195–199.Google Scholar
Jaekel, O. 1918. Phylogenie und system der Pelmatozoen. Paläontologische Zeitschrift, 3: 1–128.Google Scholar
Lin, J-P, Ausich, W. I., Zhao, Y., and Peng, J. 2007. Taphonomy, paleoecological implications, and coloration of Cambrian gogiid echinoderms from Guizhou Province, China. Geological Magazine, 145: 17–36.CrossRefGoogle Scholar
Parsley, R. and Prokop, R. 2004. Functional morphology and paleoecology of some sessile Middle Cambrian echinoderms from the Barrandian region of Bohemia, Bulletin of Geosciences. 79: 147–156.Google Scholar
Parsley, R. L. and Zhao, Y. 2004. Functional morphology of brachioles in gogiid and other Early and Middle Cambrian Eocrinoids, pp. 479–484. In Heinzeller, T. and Nebelsick, J. (eds.), Echinoderms München. Taylor and Francis Group, London.Google Scholar
Parsley, R. and Zhao, Y. 2006. Long stalked eocrinoids in the basal Middle Cambrian Kaili Biota, Taijiang County, Guizhou Province, China. Journal of Paleontology, 80: 1058–1071.CrossRefGoogle Scholar
Sprinkle, J. 1973. Morphology and evolution of blastozoan echinoderms. Museum of Comparative Zoology, Harvard University, Cambridge, MA, Special Publication.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: 303–322.Google Scholar
Turek, V., Horny, R., and Prokop, R. 2003. Ztracená mofe uprostřed Evropy (Vanished seas in the centre of Europe), Academia (Academy of Science of the Czech Republic), Prague.Google Scholar
Ubaghs, G. 1968. Eocrinoidea, p. S455–S495. In Moore, R. C. (ed.), Treatise on Invertebrate Paleontology, Part S, Echinodermata 1 (Volume 2), Geological Society of America and University of Kansas, Lawrence and New York.Google Scholar
Walcott, C. D. 1917. Cambrian geology and paleontology IV. Fauna of the Mount Whyte Formation. Smithsonian Miscellaneous Collections, 67: 61–114.Google Scholar
Zhang, Z., Gong, X., and Chen, J. 1996. A preliminary discussion on preservation condition of Kaili Fauna, Middle Cambrian from Taijiang, Guizhou China. Acta Palaeontologica Sinica. 35: 607–612.Google Scholar
Zhao, Y., Huang, Y., and Gong, X. 1994. Echinoderm fossils of Kaili Fauna from Taijiang, Guizhou. Acta Palaeontologica Sinica, 33 (3): 305–334.Google Scholar
Zhao, Y., Yuan, J., Zhu, M., Yang, R., Guo, Q., Qian, Y., Huang, Y., and Pan, Y. 1999. A progress report on research on the early Middle Cambrian Kaili Biota, Guizhou, PRC. Acta Palaeontologica Sinica, 38 (supp): 1–14.Google Scholar
Zhao, Y., Zhu, M., Babcock, L. E., Yuan, J., Parsley, R. L., Peng, J., Yang, X., and Wang, Y. 2005. Kaili Biota: A Taphonomic Window on Diversification of Metazoans from the Basal Middle Cambrian: Guizhou, China, Acta Geologica Sinica, 79: 751–765.Google Scholar
Zhao, Y., Parsley, R. L., and Peng, J. 2008. Basal Middle Cambrian short-stalked Eocrinoids from the Kaili Biota: Guizhou Province, China. Journal of Paleontology, 82: 415–422.Google Scholar
Zhu, M., Erdtmann, B. D., and Zhao, Y. 1999. Taphonomy and paleoecology of the early Middle Cambrian Kaili Lagerstätte in Guizhou, China. Acta Palaeontologica Sinica, 38(supp.): 47–57.Google Scholar