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The pelmatozoan fauna of the High Mains Formation (Ordovician: Hirnantian) of the Craighead Inlier, Strathclyde

Published online by Cambridge University Press:  03 November 2011

S. K. Donovan
Affiliation:
Department of Geology, University of the West Indies, Mona, Kingston 7, Jamaica.
D. A. T. Harper
Affiliation:
Department of Geology, University College, Galway, Ireland.

Abstract

Faunas of disarticulated ossicles, particularly columnals, are a potentially important source of data for helping to elucidate the patterns of evolution and extinction shown by pelmatozoans in the late Ordovician. The columnal fauna of the Hirnantian High Mains Formation, Craighead Inlier, Strathclyde, includes the following morphotaxa: Cyclocyclicus (col.) foraminosus sp. nov.; Cyclocyclicus (col.) periogmos sp. nov.; Hypsinomocrinus (col.) lewisi gen. et sp. nov.; Tetragonotetragonalis (col.) girvanensis sp. nov.; and Pentagonopentagonalis (col.) sp. This is the first Hirnantian columnal fauna to be described from the North American province; it is distinctly different from Hirnantian columnal biota described from Wales and Kazakhstan.

Type
Research Article
Copyright
Copyright © Royal Society of Edinburgh 1992

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References

Ausich, W. I. 1984a. Calceocrinids from the early Silurian (Llandoverian) Brassfield Formation of southwestern Ohio. J PALEONTOL 58, 1167–85.Google Scholar
Ausich, W. I. 1984b. The genus Clidochirus from the early Silurian of Ohio (Crinoidea: Llandoverian). J PALEONTOL 58, 1341–6.Google Scholar
Ausich, W. I. 1985. New crinoids and revision of the Superfamily Glyptocrinacea (early Silurian, Ohio). J PALEONTOL 59, 793808.Google Scholar
Ausich, W. I. 1986a. Early Silurian rhodocrinitacean crinoids (Brassfield Formation, Ohio). J PALEONTOL 60, 84106.CrossRefGoogle Scholar
Ausich, W. I. 1986b. Early Silurian inadunate crinoids (Brassfield Formation, Ohio). J PALEONTOL 60, 719–35.CrossRefGoogle Scholar
Ausich, W. I. 1986c. New camerate crinoids of the suborder Glyptocrinina from the Lower Silurian Brassfield Formation (southwestern Ohio). J PALEONTOL 60, 887–97.CrossRefGoogle Scholar
Ausich, W. I. 1987. Brassfield Compsocrinina (Lower Silurian crinoids) from Ohio. J PALEONTOL 61, 552–62.CrossRefGoogle Scholar
Ausich, W. I. & Dravage, P. 1988. Crinoids from the Brassfield Formation of Adams County, Ohio. J PALEONTOL 62, 285–9.CrossRefGoogle Scholar
Ausich, W. I. & Schumacher, G. A. 1984. New Lower Silurian rhombiferan cystoid (Echinodermata, Callocystitidae) from southwestern Ohio. J PALEONTOL 58, 915.Google Scholar
Barnes, C. R. 1986. The faunal extinction event near the Ordovician-Silurian boundary: a climatically induced crisis. In Walliser, O. H. (Ed.) Global bio-events, 121–6. Berlin: Springer-Verlag.Google Scholar
Barnes, C. R. 1988. Stratigraphy and palaeontology of the Ordovician-Silurian boundary interval, Anticosti Island, Quebec, Canada. BULL BR MUS NAT HIST (GEOL) 43, 195219.Google Scholar
Bengtson, P. 1988. Open nomenclature. PALAEONTOLOGY 31, 223–7.Google Scholar
Brenchley, P. J. 1989. The late Ordovician extinction. In Donovan, S. K. (Ed.) Mass extinctions: process and evidence, 104–32. London: Belhaven Press.Google Scholar
Donovan, S. K. 1983. Evolution and biostratigraphy of pelmatozoan columnals from the Cambrian and Ordovician of Britain. Unpublished Ph.D. thesis, University of Liverpool.Google Scholar
Donovan, S. K. 1984. Stem morphology of the Recent crinoid Chladocrinus (Neocrinus) decorus. PALAEONTOLOGY 27, 825–41.Google Scholar
Donovan, S. K. 1986. Pelmatozoan columnals from the Ordovician of the British Isles, part 1. PALAEONTOGR SOC MONOGR 138 (568), 168.Google Scholar
Donovan, S. K. 1988a. Functional morphology of synarthrial articulations in the crinoid stem. LETHAIA 21, 169–75.CrossRefGoogle Scholar
Donovan, S. K. 1988b. The British Ordovician crinoid fauna. LETHAIA 21, 424.CrossRefGoogle Scholar
Donovan, S. K. 1989a. The significance of the British Ordovician crinoid fauna. MODERN GEOL 13, 243–55.Google Scholar
Donovan, S. K. 1989b. Pelmatozoan columnals from the Ordovician of the British Isles, part 2. PALAEONTOGR SOC MONOGR 142 (580), 69114.CrossRefGoogle Scholar
Donovan, S. K. 1991a. The crinoid Xenocrinus as a key element of the Hirnantia fauna. GEOL SOC AM ABSTR W PROG 23 (3), 10.Google Scholar
Donovan, S. K. 1991b. The taphonomy of echinoderms: calcareous multi-element skeletons in the marine environment. In Donovan, S. K. (Ed.) The processes of fossilization, 241–69. London: Belhaven Press.Google Scholar
Donovan, S. K. 1992a. New cladid crinoids from the late Ordovician of Scotland. PALAEONTOLOGY 35, 149–58.Google Scholar
Donovan, S. K. 1992b. A new crinoid from the Ashgill (Upper Ordovician) Threave Glen Starfish Bed. SCOTT J GEOL 28, 123–6.CrossRefGoogle Scholar
Donovan, S. K. 1992c. A Rhuddanian (Silurian, Lower Llandovery) pelmatozoan fauna from southwest Wales. GEOL J 27, 19 pp.Google Scholar
Donovan, S. K. & Veltkamp, C. J. 1993. Crinoids from the upper Ashgill (Upper Ordovician) of Wales. J PALEONTOL 67.CrossRefGoogle Scholar
Donovan, S. K. & Westhead, S. 1987. Platycrinites contractus (Gilbertson) and a new Platycrinites from the Lower Carboniferous of northern England. PROC GEOL ASS 98, 211–15.CrossRefGoogle Scholar
Donovan, S. K., Hollingworth, N. T. J. & Veltkamp, C. J. 1986. The British Permian crinoid ‘Cyathocrinites’ ramosus (Schlotheim). PALAEONTOL 29, 809–25.Google Scholar
Eckert, J. D. 1984. Early Llandovery crinoids and stelleroids from the Cataract Group (Lower Silurian) in southern Ontario, Canada. R ONTARIO MUS LIFE SCI CONTR 137, 183.Google Scholar
Eckert, J. D. 1988. Late Ordovician extinction of North American and British crinoids. LETHAIA 21, 147–67.CrossRefGoogle Scholar
Harper, D. A. T. 1981. The stratigraphy and faunas of the Upper Ordovician High Mains Formation of the Girvan district. SCOTT J GEOL 17, 247–55.CrossRefGoogle Scholar
Harper, D. A. T. 1982. The late Ordovician Lady Burn Starfish Beds of Girvan. PROC GEOL SOC GLASGOW FOR 1980–1981 (sessions 122/123), 2832.Google Scholar
Harper, D. A. T. 1988. Ordovician-Siluran junctions in the Girvan district, S.W. Scotland. BULL BR MUS NAT HIST (GEOL) 43, 4552.Google Scholar
Hiller, N. 1980. Ashgill Brachiopoda from the Glyn Ceiriog district, north Wales. BULL BR MUS NAT HIST (GEOL) 34, 109216.Google Scholar
Jeffords, R. M. 1978. Dissociated crinoid skeletal elements. In Moore, R. C. & Teichert, C. (Eds) Treatise on invertebrate paleontology, Part T, Echinodermata 2(3), T928–T937. Boulder and Lawrence: Geological Society of America and University of Kansas Press.Google Scholar
Klikushin, V. G. 1975. Mechanics of the column in the Bourgueticrinidae. PALEONTOL J 9, 121–4. [Translated from Russian.]Google Scholar
Matthews, S. C. 1973. Notes on open nomenclature and on synonymy lists. PALAEONTOLOGY 16, 713–19.Google Scholar
Moore, R. C., Jeffords, R. M. & Miller, T. H. 1968. Morphological features of crinoid columns. PALEONTOL CONTR UNIV KANS, ECHINODERMATA, ART 8, 130.Google Scholar
Owen, A. W. 1986. The uppermost Ordovician (Hirnantian) trilobites of Girvan, SW Scotland with a review of coeval trilobite faunas. TRANS R SOC EDINBURGH EARTH SCI 77, 231–9.CrossRefGoogle Scholar
Owen, A. W., Harper, D. A. T. & Rong, Jia-yu. 1991. Hirnantian trilobites and brachiopods in space and time. In Barnes, C. R. & Williams, S. H. (Eds) Ordovician geology. GEOL SURV CAN PAP 90–9, 179–90.Google Scholar
Paul, C. R. C. & Smith, A. B. 1984. The early radiation and phylogeny of echinoderms. BIOL REV 59, 443–81.CrossRefGoogle Scholar
Riddle, S. W. 1989. Functional morphology and paleoecological implications of the platycrinitid column (Echinodermata, Crinoidea). J PALEONTOL 63, 889–97.CrossRefGoogle Scholar
Ride, W. D. L., Sabrosky, C. W., Bernardi, G. & Melville, R. V. (eds). 1985. International Code of Zoological Nomenclature (3rd edition). London: International Trust for Zoological Nomenclature.Google Scholar
Jia-yu, Rong & Harper, D. A. T. 1988. A global synthesis of the latest Ordovician Hirnantian brachiopod faunas. TRANS R SOC EDINBURGH EARTH SCI 79, 383402.CrossRefGoogle Scholar
Shrake, D. L., Schumacher, G. A. & Swinford, E. M. 1988. Field guidebook to the stratigraphy, sedimentology, and paleontology of the Upper Ordovician rocks of southwestern Ohio. Tulsa: Society of Economic Paleontologists and Mineralogists.Google Scholar
Signor, P. W. III, & Lipps, J. H. 1982. Sampling bias, gradual extinction patterns and catastrophes in the fossil record. GEOL SOC AM MEM 190, 291–6.Google Scholar
Stukalina, G. A. 1968. On the systematics of the Pentamerata (Crinoidea) group. PALEONTOL J 1, 7382. [Translated from Russian.]Google Scholar
Stukalina, G. A. 1978. Tsistoidei i morskie lilii. [Cystoids and crinoids.] In Sokolov, B. S. & Yolkin, E. A. (Eds) Pogranichnie Sloi Ordovika i Silura Altae-Sayanskoi Oblasti i Tyan-Shanya. SIBIR OTDEL INST GEOL GEOG TRUDY 397, 145–64. [In Russian.]Google Scholar
Stukalina, G. A. 1979. Krinoidei Krivolutskogo, Mangazeiskogo, Dolborskogo i Ketskogo gorínzontiv. [Crinoids of the Krivolutsky, Mangazeisky, Dolbrosky and Ketsky horizons.] In Menner, V. V. (Ed.) Ordovician faunas of middle Siberia. IZDATEL NAUK TRUDY 330, 131–58. [In Russian; not seen.]Google Scholar
Stukalina, G. A. 1980. Krinoidei. [Class Crinoidea.] In Bandaletov, S. M. (Ed.) Granitsa Ordovika i Silura v Kazakhstana, 170–3. Alma-Ata: Akademiya Nauk Kazakhskoi SSR. [In Russian.]Google Scholar
Stukalina, G. A. 1980. Krinoidei. [Class Crinoidea.] In Bandaletov, S. M. (Ed.) Granitsa Ordovika i Silura v Kazakhstana, 170–3. Alma-Ata: Akademiya Nauk Kazakhskoi SSR. [In Russian.]Google Scholar
Stukalina, G. A. 1988. Studies in Paleozoic crinoid-columnals and -stems. PALAEONTOGR ABT A 204, 166.Google Scholar
Ubaghs, G. 1978. Skeletal morphology of fossil crinoids. In Moore, R. C. & Teichert, C. (Eds) Treatise on invertebrrate paleontology, Part T, Echinodermata 2(1), T58–T216. Boulder and Lawrence: Geological Society of America and University of Kansas Press.Google Scholar
Webster, G. D. 1973. Bibliography and index of Paleozoic crinoids, 1942–1968. MEM GEOL SOC AM 137, xi + 341 pp.Google Scholar
Webster, G. D. 1974. Crinoid pluricolumnal noditaxis patterns. J PALEONTOL 48, 1283–8.Google Scholar
Webster, G. D. 1977. Bibliography and index of Paleozoic crinoids, 1969–1973. GEOL SOC AM MICROFORM PUBL 8, v + 235 pp.Google Scholar
Webster, G. D. 1986. Bibliography and index of Paleozoic crinoids, 1974–1980. GEOL SOC AM MICROFORM PUBL 16, viii + 405 pp.Google Scholar
Webster, G. D. 1988. Bibliography and index of Paleozoic crinoids and coronate echinoderms 1981–1985. GEOL SOC AM MICROFORM PUBL 18, 235 pp.Google Scholar
Wilkie, I. C. 1988. Design for disaster: the ophiuroid intervertebral ligament as a typical mutable collagenous structure. In Burke, R. D., Mladenov, P. V., Lambert, P. & Parsley, R. L. (Eds) Echinoderm biology: Proceedings of the Sixth International Echinoderm Conference, Victoria, British Columbia, 23–28 August 1987, 2538. Rotterdam: A. A. Balkema.Google Scholar
Yeltysheva, R. S. 1955. Morskie lilii (stebli morskikh lilii). [Sea lilies (stems of sea lilies).] In Nikiforova, O. I. (Ed.) Polevoi atlas ordovikskoi i siluriiskoi fauny Sibirskoi platformy, 40–7. Leningrad. [In Russian.]Google Scholar
Yeltysheva, R. S. 1956. Stebli morskikh lilii i ikh klassifikatsiia. [Crinoid stems and their classification.] VEST LENINGR GOS UNIV (GEOL GEOGR) 12, 40–6. [In Russian.]Google Scholar
Yeltysheva, R. S. 1960. Ordovikskie i siluriiskie krinoidei Sibirskoi Platformy. [The Ordovician and Silurian Crinoidea of the Siberian Platform.] VSES NAUCHNO-ISSLED GEOL INST TRUDY 3, 139.Google Scholar
Yeltysheva, R. S. & Stukalina, G. A. 1963. Stebli ordovikskikh i nizhesiluriiskikh krinoidei Tsentralnogo Taimyra, Novoi Zemli i Vaigacha. [Ordovician and Lower Silurian crinoid stems from central Taimyr, Novya Zemlya and Vaygacha.] UCHEN ZAP NAUCHNO-ISSLED INST GEOL ARKT (PALEONT BIOSTRAT) 2, 2362. [In Russian.]Google Scholar