Hostname: page-component-7bb8b95d7b-w7rtg Total loading time: 0 Render date: 2024-09-13T06:12:23.079Z Has data issue: false hasContentIssue false

New and revised occurrences of Ordovician crinoids from southwestern Europe

Published online by Cambridge University Press:  14 July 2015

William I. Ausich
Affiliation:
Department of Geological Sciences, 155 South Oval Mall, The Ohio State University, Columbus 43210-1397,
Artur A. Sá
Affiliation:
Departamento de Geologia, Universidade de Trás-os-Montes e Alto Douro, 5001-911 Vila Real, Portugal,
Juan C. Gutiérrez-Marco
Affiliation:
Instituto de Geologia Económica (CSIC-UCM), Facultad de Ciencias Geológicas, 28040 Madrid, Spain,

Abstract

A comprehensive treatment of Ordovician crinoids from southwestern Europe is presented, including taxa based on articulated crowns and stems. This summary incorporates new material, new localities, and a revision of some southwestern Europe occurrences. The first record of an Ordovician crinoid from Portugal, Delgadocrinus oportovinum n. gen. and sp., is reported, and this is the oldest known crinoid from the Iberian Peninsula (Arenigian/Oretanian boundary, early Darriwilian). Geographic and temporal ranges of several crinoids are revised from peri-Gondwanan areas in southwestern Europe and northern Africa or modified with new Iberian material. The Spanish range of Heviacrinus melendezi Gil Cid et al., 1996 is extended down into the lower upper Oretanian, and Merocrinus millanae Ausich et al., 2002 is restricted to the upper lower Dobrotivian. The stratigraphic position of Ortsaecrinus cocae Gil Cid et al., 1999b is restricted to the early middle Berounian, and the range of Visocrinus castelli Ausich et al., 2002 is restricted to the late middle Berounian (see Fig. 2). New topotype material of Morenacrinus silvani Ausich et al., 2002 is reported that furthers understanding of the occurrence this taxon, which was previously only positively known from the holotype.

Type
Research Article
Copyright
Copyright © The 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

Aceñolaza, G. F. and Gutiérrez-Marco, J. C. 1998. Estructuras de fijación de pelmatozoos (equinodermos) en el Ordovícico Medio de la Zona Centroibérica española. Coloquios de Paleontología, 49:2340.Google Scholar
Álvaro, J. J. and Colchen, M. 2002. Earliest Ordovician pelmatozoan holdfasts from western Europe: The Oryctoconus problem revisited. Eclogae Geologicae Helvetiae, 95:451459.Google Scholar
Arroyo, F. and Lara, R. 2002. Catálogo de las especies de equinodermos s.l. del Ordovícico español. Coloquios de Paleontología, 53:87108.Google Scholar
Ausich, W. I. 1998. Early phylogeny and subclass division of the Crinoidea (phylum Echinodermata). Journal of Paleontology, 72:499510.CrossRefGoogle Scholar
Ausich, W. I., Gil Cid, M. D., and Domínguez Alonso, P. 2002. Ordovician [Dobrotivian (Llandeilian Stage) to Ashgill] crinoids (phylum Echinodermata) from the Montes de Toledo and Sierra Morena, Spain with implications for the paleogeography of Peri-Gondwana. Journal of Paleontology, 76:975992.2.0.CO;2>CrossRefGoogle Scholar
Barrande, J. 1899. Systeme Silurien du centre de la Bohême, Volume VII, Classe des Echinodermes, Pt. 2, Famille des Crinoides. Rivnac, Prague, 216 p.Google Scholar
Bather, F. A. 1899. A phylogenetic classification of the Pelmatozoa. British Association for the Advancement of Science, report for 1898:916923.Google Scholar
Bengtson, P. 1988. Open nomenclature. Palaeontology, 31:223227.Google Scholar
Botquelen, A., Le Menn, J., and Loi, J. 2006. Echinodermes de l'Ordovicien supérieur (Ashgill) de Sardaigne et d'Algérie. Geobios, 39:1323.CrossRefGoogle Scholar
Botting, J. P. 2003. Llanvirn (Middle Ordovician) echinoderms from Llandegley rocks, central Wales. Palaeontology, 46:685708.CrossRefGoogle Scholar
Carneiro, A. 2005. The museum of the Geological Survey of Portugal: The role of the ‘Bilobites’ collection in a 19th-century palaeoichnological controversy. In Beretta, M. (ed.), From Private to Public, Natural Collections and Museums, New York, Science History Publications, Sagamore Beach, Massachusetts.Google Scholar
Chauvel, J. and Le Menn, J. 1973. Echinodermes de l'Ordovicien supérieur de Coat-Carrec, Argol (Finistère). Bulletin de la Societé Géologique et Minéralogique de Bretagne (C), 4:3961.Google Scholar
Chauvel, J. and Le Menn, J. 1979. Sur quelques Echinodermes (Cystoïdes et Crinoïdes) de l'Ashgill d'Aragon (Espagne). Géobios, 12:549587.CrossRefGoogle Scholar
Chauvel, J., Meléndez, B., and Le Menn, J. 1975. Les Echinodermes (Cysto'ides et Crinoïdes) de l'Ordovicien supérieur de Luesma (Sud de l'Aragon, Espagne). Estudios Geológicos, 31:351364.Google Scholar
Cocks, L. R. M. 2000. The Early Palaeozoic geography of Europe. Journal of the Geological Society, London, 157:110.CrossRefGoogle Scholar
Cocks, L. R. M. 2001. Ordovician and Silurian geography. Journal of the Geological Society, London, 158:197210.CrossRefGoogle Scholar
Cope, J. C. W. and Donovan, S. K. 2005. Parablastoid holdfasts from the Lower Ordovician of South Wales. Geological Journal, 40:295300.CrossRefGoogle Scholar
Courtessole, R., Marek, L., Pillet, J., Ubaghs, G., and Vizcaïno, D. 1983. Calymenina, Echinodermata et Hyolitha de l'Ordovicien inféieur de la Montagne Noire (France méridionale). Mémoire de la Société d'Etudes Scientifiques de l'Aude, 1983:162.Google Scholar
Couto, H. and Gutiérrez-Marco, J. C. 1999. Nota sobre algunos Diploporita (Echinodermata) de las pizarras de la Formación Valongo (Ordovícico Medio, Portugal). Temas Geológico-Mineros ITGE, 26:541545.Google Scholar
Couto, H., Piçarra, J. M., and Gutiérrez-Marco, J. C. 1997. El Paleozoico del Anticlinal de Valongo (Portugal), p. 270290. In Grandal d'Anglade, A., Gutiérrez-Marco, J. C., and Santos Fidalgo, L. (eds.), Comunicaciones XIII Jornadas de Paleontología y V Reunión Internacional PIGC 351, A Coruña., Madrid.Google Scholar
Delgado, J. F. N. 1908. Système Silurique du Portugal. Étude de Stratigraphie Paléontologique. Memoire de la Commission du Service Géologique du Portugal, 245 p.Google Scholar
Domínguez Alonso, P., Gil Cid, M. D., and Silván Pobes, E. 1994. Primer crinoide (Disparida Iocrinidae) descrito para el Ordovícico medio de los Montes de Toledo, p. 6466. In Fernández López, S. (ed.), Comunicaciones de las X Jornadas de Paleontología, Madrid.Google Scholar
Donovan, S. K. 1986. Pelmatozoan columnals from the Ordovician of the British Isles, Pt. 1, Monograph of the Palaeontographical Society London, 138:168.Google Scholar
Donovan, S. K. 1989. Pelmatozoan columnals from the Ordovician of the British Isles, Pt. 2, Monograph of the Palaeontographical Society London, 142:69114.CrossRefGoogle Scholar
Donovan, S. K. 1995. Pelmatozoan columnals from the Ordovician of the British Isles, Pt. 3, Monograph of the Palaeontographical Society London, 149:115193.CrossRefGoogle Scholar
Donovan, S. K. and Savill, J. J. 1988. Ramseyocrinus (Crinoidea) from the Arenig of Morocco. Journal of Paleontology, 62:283285.CrossRefGoogle Scholar
Fortey, R. A. and Cocks, L. R. M. 2003. Palaeontological evidence bearing on global Ordovician–Silurian continental reconstructions. Earth-Science Reviews, 61:245307.CrossRefGoogle Scholar
Finney, S. 2005. Global series and stages for the Ordovician System: A progress report. Geologica Acta, 3(4):309316.Google Scholar
Gibbons, W. and Moreno, T. 2002. Introduction and overview, p. 16. In Gibbons, W. and Moreno, T. (eds.), The Geology of Spain. Geological Society, London.Google Scholar
Gil Cid, M. D., Domínguez Alonso, P., and Silván Pobes, E. 1996. Reconstrucción y modo vida de Heviacrinus melendezi nov. gen. nov. sp. (Disparida Iocrinidae), primer crinoide descrito para el Ordovícico medio de los Montes de Toledo (España). Revista de la Sociedad Geológica de España, 9:1927.Google Scholar
Gil Cid, M. D., Domínguez Alonso, P., and Silván Pobes, E. 1998. Coralcrinus sarachagae gen. nov. sp. nov., primer crinoide (Disparida, Inadunata) descrito en el Ordovícico medio de Sierra Morena. Coloquios de Paleontología, 49:115128.Google Scholar
Gil Cid, M. D., Domínguez Alonso, P., and Silván Pobes, E. 1999a. Coralcrinus sarachagae gen. nov. sp. riov., primer crinoide (Disparida, Inadunata) descrito en el Ordovícico medio de Sierra Morena.” Respuesta. Coloquios de Paleontología, 50:217.Google Scholar
Gil Cid, M. D., Domínguez Alonso, P., Torres, M., and Jiménez, I. 1999b. A mathematical tool to analyze radially symmetrical organisms and its application to a new camerate from the Upper Ordovician of south western Spain. Geobios, 32:861867.Google Scholar
Gil Cid, M. D., Arroyo, F., Lara, R., Rodrigues, N. P. C., and Torices, A. 2002. Taphonomic features on the marine assemblages in the Lower Palaeozoic (Cambrian-Ordovician) from the SW of Spain, p. 257267. In de Renzi, M., Pardo Alonzo, M. V., Belinchón, M., Peñalver, E., Montoya, P., and Márquez-Aliaga, A. (eds.), Current Topics on Taphonomy and Fossilization. Publicaciones Ayuntamiento de Valencia, Valencia.Google Scholar
Gutiérrez-Marco, J. C. 1999. Coralcrinus sarachagae gen. nov. sp. nov., primer crinoide (Disparida, Inadunata) descrito en el Ordovícico medio de Sierra Morena,” original de M. D. Gil Cid, P. Domínguez Alonso y E. Silván Pobes. Discusión. Coloquios de Paleontología, 50:209215.Google Scholar
Gutiérrez-Marco, J. C., Chauvel, J., Meléndez, B., and Smith, A. B. 1984. Los equinodermos (Cystoidea, Homalozoa, Stelleroidea, Crinoidea) del Paleozoico inferior de los Montes de Toledo y Sierra Morena (España). Estudios Geológicos, 40:421453.CrossRefGoogle Scholar
Gutiérrez-Marco, J. C., Aramburu, C., Arbizu, M., Méndez-Bedia, I., Rábano, I., and Villas, E. 1996. Rasgos estratigráficos de la sucesión del Ordovícico Superior en Portilla de Luna (Zona Cantábrica, noroeste de España). Geogaceta, 20:1114.Google Scholar
Gutiérrez-Marco, J. C., Robardet, M., Rábano, I., Sarmiento, G. N., San José Lancha, M. A., Herranz Araújo, P., and Pieren Pidal, A. P. 2002. Ordovician, p. 3149. In Gibbons, W. and Moreno, T. (eds.), The Geology of Spain. The Geological Society, London.CrossRefGoogle Scholar
Lefebvre, B. and Fatka, O. 2003. Palaeogeographical and palaeoecological aspects of the Cambro–Ordovician radiation of echinoderms in Gondwanan Africa and peri-Gondwanan Europe. Palaeogeography, Palaeoclimatology, Palaeoecology, 195:7397.CrossRefGoogle Scholar
Le Menn, J. and Meléndez, B. 1988. Nouvelle interprétation des échinodermes de Collado de Tosas (Gerona, Espagne). Estudios Geológicos, 44:473476.CrossRefGoogle Scholar
Le Menn, J. and Spjeldnaes, N. 1996. Un nouveau crinoïde Dimerocrinitidae (Camerata, Diplobathrida) de l'Ordovicien supérieur du Maroc: Rosfacrinus robustus nov. gen., nov. sp. Geobios, 29:341351.CrossRefGoogle Scholar
Matthews, S. C. 1973. Notes on open nomenclatura and on synonymy lists. Palaeontology, 16:713719.Google Scholar
Miller, J. S. 1821. A Natural History of the Crinoidea or Lily-Shaped Animals, with Observations on the Genera Asteria, Euryale, Comatula and Marsupites. Bryan, Bristol, 150 p.Google Scholar
Moore, R. C. 1939. The use of fragmentary crinoidal remains in stratigraphic paleontology. Denison University Bulletin, Journal of the Scientific Laboratories, 33:165250.Google Scholar
Moore, R. C. and Jeffords, R. M. 1968. Classification and nomenclature of fossil crinoids based on studies of dissociated parts of their columns. University of Kansas Paleontological Contributions, Echinodermata Article, 9:186.Google Scholar
Moore, R. C. and Laudon, L. R. 1943. Evolution and classification of Paleozoic crinoids. Geological Society of America Special Papers, 46, 153 p.Google Scholar
Moore, R. C. and Teichert, C. (eds.). 1978. Treatise on Invertebrate Paleontology, Pt. T, Echinodermata 2. 3 vols. Geological Society of America and University of Kansas Press, Lawrence, 1027 p.Google Scholar
Paris, F. 1998. Early Palaeozoic palaeobiogeography of northern Gondwana region. Acta Universitatis Carolinae–Geologica, 42:473483.Google Scholar
Paris, F. and Robardet, M. 1990. Early Paleozoic palaeobiogeography of the Variscan regions. Tectonophysics, 177:193213.CrossRefGoogle Scholar
Paul, C. R. C. and Cope, J. C. W. 1982. A parablastoid from the Arenig of South Wales. Palaeontology, 25:499507.Google Scholar
Prokop, R. J. and Petr, V. 1999. Echinoderms in the Bohemian Ordovician. Journal of the Czech Geological Society, 44:6368.Google Scholar
Robardet, M. and Gutiérrez-Marco, J. C. 1990. Sedimentary and faunal domains in the Iberian Peninsula during Lower Paleozoic times, p. 383395. In Dalmayer, R. D. and Martínez García, E. (eds.), Pre-Mesozoic Geology of Iberia. Springer-Verlag, Berlin.CrossRefGoogle Scholar
Sdzuy, K., Hammann, W., and Villas, E. 2001. The Upper Tremadoc fauna from Vogtendorf and the Bavarian Ordovician of the Frankenwald (Germany). Senckenbergiana Lethaea, 81:207261.CrossRefGoogle Scholar
Seilacher, A. and Macclintock, C. 2005. Crinoid anchoring strategies for soft-bottom dwelling. Palaios, 20:224240.CrossRefGoogle Scholar
Silván Pobes, E., Gil Cid, M. D., Domínguez Alonso, P., and Escribano Ródenas, M. 1998. More about Spanish Ordovician crinoids, p. 196. In Mooi, R. and Telford, M. (eds.), Echinoderms: San Francisco. Balkema, Rotterdam.Google Scholar
Stukalina, G. A. 1986. Zakonomernosti Istoricheskogo Rasvitiya Crinoidey v Rannem i Srednem Paleozoe SSSR. Nauka, Leningrad, 142 p.Google Scholar
Stukalina, G. A. 1988. Studies in Paleozoic crinoid-columnals and stems. Palaentographica Abteilung A, 204:166.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. 1972. More about Aethocrinus moorei Ubaghs, the oldest known dicyclic crinoid. Journal of Paleontology, 46:773775.Google Scholar
Ubaghs, G. 1978. Skeletal morphology of fossil crinoids, p. T58T216. In Moore, R. C. and Teichert, C. (eds.), Treatise on Invertebrate Paleontology, Pt. T, Echinodermata 2. Geological Society of America and University of Kansas Press, Lawrence.Google Scholar
Ulrich, E. O. 1925. New classification of the Heterocrinidae, p. 82101. In Foerste, A. F., Upper Ordovician faunas of Ontario and Quebec. Canada Geological Survey Memoir, 138.Google Scholar
Vinassa de Regny, P. 1942. Fossili ordoviciani sardi. Parte II. Atti degli Reale Accademia d'Italia, Memorie Scienze Fisiche, Matematiche e Naturale, 12:10251055.Google Scholar
Vizcaïno, D. and Lefebvre, B. 1999. Les Echinodermes du Paléozoïque inférieur de Montagne Noire: Biostratigraphie et paléobiodiversité. Geobios, 32:353364.CrossRefGoogle Scholar
Von Raumer, J., Stampfli, G. M., Borel, G. D., and Bussy, F. 2002. The organization of pre-Variscan basement areas at the north-Gondwanan margin. International Journal of Earth Sciences, 91:3552.CrossRefGoogle Scholar
Wachsmuth, C. and Springer, F. 1879-1886. Revision of the Palaeocrinoidea. Philadelphia Academy of Natural Sciences Proceedings, 1885:225364(1-138).Google Scholar
Wright, D. K. 1983. Crinoid ossicles in Upper Ordovician benthic marine assemblages from Snowdonia, North Wales. Palaeontology, 26:585603.Google Scholar
Yeltyschewa, R. S. 1955. Morskie lilii, p. 4347In Nikiforova, O. I. (ed.), Polevoy Atlas Ordovikskoy i Silurskoy Fauni Sibirskoy Platformiy. Gosgeoltehizdat, Moskva.Google Scholar
Yeltyschewa, R. S. and Stukalina, G. A. 1963. Stebli Ordovikskikh i nizhnesiluriy skikh krinoidey Tsentralnogo Taymyra, Novoy Zemli i Baygacha. Uchenye zapiski Nauk Izvestiya Institut Geologii Arctic Paleontologiya i Biostratigrafiya Izdatel'stvo, 2:2362.Google Scholar