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(Echinodermata) of Possible Late Silurian Age from Central Newfoundland S Document généré le 1 oct. 2021 08:05 Atlantic Geology A new species of stalked crinoid (Echinodermata) of possible Late Silurian age from central Newfoundland S. K. Donovan, W. L. Dickson, W. D. Boyce et J. S. Ash Volume 33, numéro 1, spring 1997 Résumé de l'article Un nouvel emplacement de fossiles a I'interieur d'une sequence auparavant URI : https://id.erudit.org/iderudit/ageo33_1art02 attribute au groupe de l'Ordovicien moyen de Baie d'Espoir dans le centre-sud de Terre-Neuve renferme des fragments de columnales et de brachiopodes de Aller au sommaire du numéro crinoldes. Des columnales de crinoldes penta£toil6es caracteristiqucs, semblables i celles attributes a 1'Hexacrinites Austin and Austin a loges monobathrides par des auteurs russes, sont baptis6es nouvellc espece Éditeur(s) pentastellatus d''Hexacrinites!. Les columnales nodales(?) de cette espece sont pourvues d'une facette articulaire renfonede et circulaire munie d'un Atlantic Geoscience Society crenularium allant de conique a bombi, d'une areole circulaire renfoncie, d'un perilumen sureleve et d'un canal axial mince et court de section pentagonalc. ISSN Les plus anciens Hexacrinites, au sens strict, remontent au Silurien supirieur, ce qui permet de supposer qu'on a incorrectement attribu£ la strate fossilifere 0843-5561 (imprimé) a l'Ordovicien. Des ichantillons reprlsentatifs de brachiopodes du memc 1718-7885 (numérique) emplacement comprenncnt un exemple qui ressemble a plusieurs genres de pentamiroldes datant du Silurien infeiieur au Ddvonien supeiieur, notamment Découvrir la revue le Brooksina Kirk, 1922. Leur correlation avec des strates renfermant des bivalves du Silurien superieur a SO km au nord-cst signale qu'une discordance importantc pourrait se presenter au-dessus des strates fossiliferes de Citer cet article l'Ordovicien inftrieur ou moyen de m£me que des complexes d'ophiolites de l'Ordovicien inftrieur. Donovan, S. K., Dickson, W. L., Boyce, W. D. & Ash, J. S. (1997). A new species of [Traduit par la redaction] stalked crinoid (Echinodermata) of possible Late Silurian age from central Newfoundland. Atlantic Geology, 33(1), 11–17. All rights reserved © Atlantic Geology, 1997 Ce document est protégé par la loi sur le droit d’auteur. L’utilisation des services d’Érudit (y compris la reproduction) est assujettie à sa politique d’utilisation que vous pouvez consulter en ligne. https://apropos.erudit.org/fr/usagers/politique-dutilisation/ Cet article est diffusé et préservé par Érudit. Érudit est un consortium interuniversitaire sans but lucratif composé de l’Université de Montréal, l’Université Laval et l’Université du Québec à Montréal. Il a pour mission la promotion et la valorisation de la recherche. https://www.erudit.org/fr/ A tlantic Geology 11 A new species of stalked crinoid (Echinodermata) of possible Late Silurian age from central Newfoundland S.K. Donovan1, W.L. Dickson2, WD. Boyce2, and J.S. Ash2 1Department of Geology, University of the West Indies, Mona, Kingston 7, Jamaica 2Geological Survey, Newfoundland and Labrador Department of Mines and Energy, P. O. Box 8700, St. John’s, NewfoundlandA1B 4J6, Canada Date Received May 20, 1996 Date Accepted August 7, 1996 A new fossil locality within a sequence previously assigned to the Middle Ordovician Baie D’Espoir Group in south-central Newfoundland contains fragmented crinoid columnals and brachiopods. Distinctive, pentastellate crinoid columnals, similar to those assigned to the monobathrid camerate Hexacrinites Austin and Austin by Russian authors, are named Hexacrinitesl pentastellatus n. sp. Nodal(?) columnals of this species have a circular, depressed articular facet, with a conical to bowl-like crenularium, a depressed, circular areola, a raised perilumen and a short, slender axial canal of pentagonal section. The oldest Hexacrinites sensu stricto are Late Silurian, suggesting that the fossiliferous strata have been incorrectly assigned to the Ordovician. Cross-sections of bra­ chiopods from the same locality include an example that resembles several Early Silurian to Late Devonian pentameroid genera including Brooksina Kirk, 1922. Correlation with Late Silurian, bivalve-bearing strata 50 km to the north­ east would indicate that a major unconformity may occur above the fossiliferous Early and Middle Ordovician strata and the Early Ordovician ophiolite complexes. Un nouvel emplacement de fossiles a l’interieur d’une sequence auparavant attribute au groupe de l’Ordovicien moyen de Baie d’Espoir dans le centre-sud de Terre-Neuve renferme des fragments de columnales et de brachiopodes de crinoides. Des columnales de crino'ides pentaetoilees caracteristiques, semblables k celles attributes a 1’Hexacrinites Austin and Austin a loges monobathrides par des auteurs russes, sont baptisees nouvelle espece pentastellatus d’Hexacrinitesl. Les columnales nodales(?) de cette espece sont pourvues d’une facette articulaire renfoncee et circulaire munie d’un crtnularium allant de conique k bombe, d’une artole circulaire renfoncee, d’un ptrilumen sureleve et d’un canal axial mince et court de section pentagonale. Les plus anciens Hexacrinites, au sens strict, remontent au Silurien superieur, ce qui permet de supposer qu’on a incorrectement attribue la strate fossilifere a l’Ordovicien. Des tchantillons reprtsentatifs de brachiopodes-du mSme emplacement comprennent un exemple qui ressemble a plusieurs genres de pentameroides datant du Silurien inferieur au Devonien superieur, notamment le Brooksina Kirk, 1922. Leur correlation avec des strates renfermant des bivalves du Silurien superieur a 50 km au nord-est signale qu’une discordance importante pourrait se presenter au-dessus des strates fossiliferes de l’Ordovicien inferieur ou moyen de meme que des complexes d’ophiolites de l’Ordovicien inferieur. [Traduit par la redaction] I ntroduction South-central Newfoundland contains few fossil locali­ ties and until recently only some had been studied in detail. The geology of south-central Newfoundland is complex. Trilobite, brachiopod and graptolite localities have received The main components are Lower Ordovician, or older, shelf- most attention, and precise stratigraphic data generally in­ facies, quartz-rich sandstone of the Spruce Brook Forma­ dicating Early and Middle Ordovician ages have been ob­ tion that has been overthrust by ophiolites of the Late Cam­ tained (e.g., Colman-Sadd and Swinden, 1984; Boyce, 1987; brian to Early Ordovician Coy Pond and Great Bend com­ Boyce etal., 1988, 1993a; Williams, 1991, 1993; Williams plexes. Various Ordovician sedimentary and volcanic units et al., 1992). Localities containing mainly cririoids, bryozoa, are juxtaposed with the ophiolite complexes along major and corals and a few brachiopods have only rarely been ex­ faults. Silurian volcanic and sedimentary rocks locally, amined in detail. Some have been determined to be Early unconformably overlie or are in fault contact with the older Silurian in age (e.g., Williams, 1972) whereas others have strata. The assignment of ages to the various sedimentary been assumed to be Silurian (e.g., Anderson and Williams, strata and, therefore, their correlation has depended on the 1970; Williams, 1972; Blackwood, 1982) (Fig. 1). few fossil localities. Recent radiometric age determinations Recently, in the Careless Brook area, 50 km northeast on the various granitic, gabbroic and felsic volcanic rocks of fossil locality 91F001 (Fig. 1), a previously known fos­ in the area have provided new insights, and revolutionized siliferous section that had been correlated with Wenlockian the understanding of the orogenic history of the area (Dun­ brachiopod-rich strata was discovered to contain many more ning etal., 1990). fossil occurrences and a much more diverse fauna than pre- Atlantic Geology 33,11-17(1997) 0843-5561/97/010011-7S2.05/0 12 D onovan e t al. Legend Lote Silurian or younger Ss Fine-grained sandstone and minor calcareous crinoid—bearing sandstone Sc Grey pebble conglomerate interbedded with Unit Ss Middle Ordovician (or younger?) On North Steady Pond Formation, Baie d’Espoir Group: Felsic crystal and lapilli tuff; minor mafic tuff Middle Ordovician (Lote Llonvirn — Eorly Llondeilo) Of Fossiliferous limestone conglomerate, containing detritai chromite Eorly Ordovician Ophiolitic rocks — Great Bend and Coy Pond Complexes Op Mainly massive serpentinized peridotite, minor layered and sheared serpentinized peridotite and harzburgite ©m’SMeared magne'sitized peridotite and sheared shale—matrix ophiolitic melange Early Ordovician or older Os Spruce Brook Formation: interbedded grey quortzitic sandstone and grey to block shale AAA Bedding — tops unkown, known, overturned A Igneous layering — tops unknown / Cleavage — first generation / Shearing — sense unknown © Fossil locality Geological contact _. _—■ Fault Fig. 1. Geology of the area around fossil locality 91F001, Northwest Gander River area. Geology from Blackwood (1983), Colman- Sadd (1985), Colman-Sadd and Russell (1988), Dec and Colman-Sadd (1990), and Dickson (1992). Inset map shows the location of the Northwest Gander River area in central Newfoundland. viously reported. Four bivalve-rich horizons collectively yielded The bivalves together indicate a Late Silurian (Pridolian) the following taxa (Boyce et al., 1993b; Boyce and Ash, to possibly Early Devonian (Gedinnian) age (Boyce et al., 1994): 1993b; Boyce and Ash, 1994). The lower parts of the se­ quence contain a variety of fossiliferous horizons contain­ Arthropoda-?Eurypterida ing crinoids, corals, bryozoa, articulate
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