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Early Ordovician agnostoid trilobites from the southern Montagne Noire, France

Published online by Cambridge University Press:  20 May 2016

M. Franco Tortello
Affiliation:
Departamento Paleozoología Invertebrados, Museo de Ciencias Naturales, Paseo del Bosque s/n°, 1900 La Plata, Argentina Laboratoire de Paléontologie et Paléogéographie du Paléozoïque, UMR 8014 CNRS, Université des Sciences et Technologies de Lille, UFR Sciences de la Terre, 59655 Villeneuve d'Ascq, France,
Daniel Vizcaïno
Affiliation:
7, rue Jean-Baptiste Chardin, Maquens, 11090 Carcassonne, France,
J. Javier Álvaro
Affiliation:
Laboratoire de Paléontologie et Paléogéographie du Paléozoïque, UMR 8014 CNRS, Université des Sciences et Technologies de Lille, UFR Sciences de la Terre, 59655 Villeneuve d'Ascq, France, Departamento Ciencias de la Tierra, Universidad de Zaragoza, 50009 Zaragoza, Spain,

Abstract

New collections rich in agnostoid trilobites were recovered from Lower Ordovician strata of the southern Montagne Noire, France. The faunas occur in the La Gardie/Val d'Homs, Saint–Chinian, La Maurerie, and Landeyran formations, coinciding with deposition in muddy outer-platform settings. Many previously described species are revised and their stratigraphic ranges emended. The studied agnostoids include Geragnostus cf. sidenbladhi (Linnarsson), G. aff. sidenbladhi, G. crassus Tjernvik, G. splendens (Holub), G. cf. explanatus Tjernvik, G. boutouryensis Howell, G. occitanus Howell, Geragnostus sp., Trinodus corpulentus Howell, Homagnostoides ferralsensis (Munier-Chalmas and Bergeron), Corrugatagnostus coulobresensis n. sp., Corrugatagnostus sp., Leiagnostus miqueli Sdzuy, and Leiagnostus sp. The record from the upper part of the Saint–Chinian Formation suggests a late Tremadocian age, whereas an early Arenigian age is indicated for the upper part of the La Maurerie Formation. Although the agnostoid record generally reinforces the peri-Gondwanan character of the Lower Ordovician shelly faunas from the Montagne Noire, some agnostoid species are independent of specific paleogeographic boundaries.

Type
Research Article
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Copyright © The Paleontological Society 

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References

Abdullaev, R. N., and Khaletskaya, O. N. 1970. Lower Palaeozoic of the Chatkalskogo ridge: Ordovician trilobites and graptolites of the Pskemskogo ridge. Akademiia Nauk Uzbekskoi SSR, Institut Geologii i Geofiziki, Tashkent, 104 p., 8 pls. (In Russian) Google Scholar
Ahlberg, P. 1988a. A revision of the Ordovician agnostid trilobite Leiagnostus Jaekel 1909. Geologiska Föreningens i Stockholm Förhandlingar, 110:363370.Google Scholar
Ahlberg, P. 1988b. Agnostid trilobites from the Ordovician of Jämtland, Sweden. Geologiska Föreningens i Stockholm Förhandlingar, 110:267278.CrossRefGoogle Scholar
Ahlberg, P. 1989a. The type species of the Ordovician agnostid trilobite Geragnostus Howell, 1935. Paläontologische Zeitschrift, 63:309317.Google Scholar
Ahlberg, P. 1989b. Agnostid trilobites from the Lower Ordovician Komstad Limestone Formation of Killeröd, Scania, Sweden. Palaeontology, 32:553570.Google Scholar
Ahlberg, P. 1990. Agnostid trilobites from the Ordovician of the Siljan district, Sweden. Geologiska Föreningens i Stockholm Förhandlingar, 112:145156.Google Scholar
Ahlberg, P. 1992. Agnostid trilobites from the lower Ordovician of southern Sweden. Transactions of the Royal Society of Edinburgh: Earth Sciences, 83:539570.CrossRefGoogle Scholar
Álvaro, J. J., González-Gómez, C., and Vizcaïno, D. 2003. Paleogeographic patterns of the Cambrian–Ordovician transition in the southern Montagne Noire (France): Preliminary results. Bulletin de la Société géologique de France, 174:2331.Google Scholar
Álvaro, J. J., Lefebvre, B., and Vizcaïno, D. 2001. Catalogue of the fossil species defined in the Lower Paleozoic of the southern Montagne Noire. Annales de la Société Géologique du Nord (2c série), 8:227232.Google Scholar
Angelin, N. P. 1854. Palaeontologia Scandinavica. I, Crustacea formationis transitionis. Fascicule 2, Stockholm, p. 2192, pls. 25–41.Google Scholar
Apollonov, M. K., and Chugaeva, M. N. 1984. Trilobites, pls. 127. In Apollonov, M. K., Chugaeva, M. N., and Dubinina, S. V. (eds.), Trilobites and Conodonts from the Batyrbay Section (Uppermost Cambrian–Lower Ordovician) in Malyi Karatau Range (Atlas of the Palaeontological Plates). Nauka Kazakh SSR, Alma Ata.Google Scholar
Babin, C., Courtessole, R., Mélou, M., Pillet, J., Vizcaïno, D., and Yochelson, E. L. 1982. Brachiopodes (articulés) et mollusques (bivalves, rostroconches, monoplacophores, gastéropodes) de l'Ordovicien inférieur (Trémadocien–Arénigien) de la Montagne Noire (France méridionale). Mémoire de la Société d'Etudes Scientifiques de l'Aude, 63 p., 15 pls.Google Scholar
Balashova, E. A. 1961. Some Tremadocian trilobites from the Aktyubinsk province. Trudy Instituta Geologii i Geofizikii Akademiia Nauk SSSR, 18:102145. (In Russian) Google Scholar
Bancroft, B. B. 1949. Upper Ordovician trilobites of zonal value in south-east Shropshire. Proceedings of the Royal Society of London, series B, 136:291315, pls. 9–11.Google Scholar
Barrande, J. 1868. Silurische Fauna aus der Umgebung von Hof in Bayern. Neues Jahrbuch für Mineralogie, Geologie und Paläontologie, 1868:641696, pls. 6, 7.Google Scholar
Barrande, J. 1872. Système Silurien du centre de la Bohême. Recherches Paléontologiques, Suplémment au Vol. 1 (Trilobites, Crustacés Divers et Poissons). Prague, 647 p., 37 pls.Google Scholar
Bérard, P. 1986. Trilobites de l'Ordovicien inférieur des Monts de Cabrières (Montagne Noire, France). Mémoires du Centre d'Etudes et de Recherches Géologiques et Hydrologiques, 24:1220.Google Scholar
Bergeron, J. 1888a. Sur la présence de la faune primordiale (Paradoxidien) dans les environs de Ferrals-les-Montagnes (Hérault). I. Etude stratigraphique. II. Etude paléontologique (en collaboration avec M. Munier-Chalmas). Comptes Rendus de l'Académie des Sciences, 106.Google Scholar
Bergeron, J. 1888b. Note sur la présence de la faune primordiale (Paradoxidien) dans les environs de Ferrals-les-Montagnes (Hérault). Bulletin de la Société géologique de France, 3e série, 16:282285.Google Scholar
Bergeron, J. 1889. Etude géologique du massif ancien situé au Sud du Plateau Central. Annales des Sciences Géologiques, 22:1362.Google Scholar
Beyrich, E. 1845. Über Einige Böhmischer Trilobiten. Berlin, 47 p., 1 pl.Google Scholar
Boeck, C. P. B. 1838. Uebersicht der bisher in Norwegen gefundenen Formen der Trilobiten-Familie, p. 138145. In Keihan, B. M. (ed.), Gaea Norvegica, 1, Christiania.Google Scholar
Callaway, C. 1877. On a new area of Upper Cambrian rocks in south Shropshire, with a description of a new fauna. Quarterly Journal of the Geological Society of London, 33:652672, pl. 24.Google Scholar
Capéra, J. C., Courtessole, R., and Pillet, J. 1975. Biostratigraphie de l'Ordovicien inférieur de la Montagne Noire (France méridionale) Trémadocien inférieur. Bulletin de la Société d'Histoire Naturelle de Toulouse, 111:337380.Google Scholar
Capéra, J. C., Courtessole, R., and Pillet, . 1978. Contribution à l'étude de l'Ordovicien inférieur de la Montagne Noire. Biostratigraphie et révision des Agnostida. Annales de la Société Géologique du Nord, 98:6788.Google Scholar
Clark, T. H. 1924. The Paleontology of the Beekmantown Series at Levis, Quebec. Bulletins of American Paleontology, 10:1134.Google Scholar
Courtessole, R., and Pillet, J. 1975. Contribution à l'étude des faunes trilobitiques de l'Ordovicien inférieur de la Montagne Noire. Les Eulominae et les Nileidae. Annales de la Société Géologique du Nord, 95:251272, pls. 24–27.Google Scholar
Courtessole, R., and Pillet, J. 1978. La faune des couches à Shumardia du Trémadocien supérieur de la Montagne Noire. Bulletin de la Société d'Histoire Naturelle de Toulouse, 114:176186.Google Scholar
Courtessole, R., Pillet, J., and Vizcaïno, D. 1981. Nouvelles données sur la biostratigraphie de l'Ordovicien inférieur de la Montagne Noire. Révision des Taihungshaniidae, de Megistaspis (Ekeraspis) et d'Asaphopsoides (Trilobites). Mémoire de la Société d'Etudes Scientifiques de l'Aude, 32 p.Google Scholar
Courtessole, R., Pillet, J., Vizcaïno, D., and Eschard, R. 1985. Etude biostratigraphique et sédimentologique des formations arenacées de l'Arenigien du Saint–Chinianais oriental (Hérault), versant sud de la Montagne Noire (France méridionale). Mémoire de la Société d'Etudes Scientifiques de l'Aude, 99 p.Google Scholar
Dalman, J. W. 1827. Om Paleaderner, eller de så kallade Trilobiterna. Kongliga Svenska Vetenskaps-Akademiens Handlingar, 1826(2):113162,226–294, pls. 1–6.Google Scholar
Dean, W. T. 1966. The Lower Ordovician stratigraphy and trilobites of the Landeyran valley and the neighbouring district of the Montagne Noire, southwestern France. Bulletin of the British Museum (Natural History), Geology, 12:245353.Google Scholar
Dean, W. T. 1971. The Lower Palaeozoic stratigraphy and faunas of the Taurus Mountains near Beysehir, Turkey. II. The trilobites of the Seydisehir Formation (Ordovician). Bulletin of the British Museum (Natural History), Geology, 20(1), 24 p., 5 pls.Google Scholar
Ebbestad, J. O. R. 1999. Trilobites of the Tremadoc Bjorkåsholmen Formation in the Oslo Region, Norway. Fossils and Strata, 47:1118.Google Scholar
Fortey, R. A. 1980. The Ordovician trilobites of Spitsbergen. III. Remaining trilobites of the Valhallfonna Formation. Norsk Polarinstitutt Skrifter, 171:1163.Google Scholar
Fortey, R. A., and Owens, R. M. 1978. Early Ordovician (Arenig) stratigraphy and faunas of the Carmarthen district, southwest Wales. Bulletin of the British Museum (Natural History), Geology, 30(3):225294.Google Scholar
Fortey, R. A., and Owens, R. M. 1987. The Arenig Series in South Wales: stratigraphy and palaeontology. Bulletin of the British Museum (Natural History), Geology, 41:69307.Google Scholar
Fortey, R. A., and Owens, R. M. 1991. A trilobite fauna from the highest Shineton Shales in Shropshire, and the correlation of the latest Tremadoc. Geological Magazine, 128:437464.Google Scholar
Goldfuss, G. A. 1843. Systematische Übersicht der Trilobiten und Beschreibung einiger neuer Arten derselben. Neues Jahrbuch für Mineralogie, Geognostische und Geologische Petrefakten-Kunde, 1843:537567.Google Scholar
Hammann, W. 1977. Neue Calymenacea (Trilobita) aus dem Ordovizium von Spanien. Senckenbergiana Lethaea, 58:9197.Google Scholar
Harrington, H. J., and Leanza, A. F. 1957. Ordovician trilobites of Argentina. Department of Geology, University of Kansas, Special Publication, 1:1276.Google Scholar
Hawle, I., and Corda, A. J. C. 1847. Prodrom einer Monographie der bohmischen Trilobiten. Abhandlungen Koeniglichen Boehmischen Gesellschaft der Wissenschaften. J. G. Calve, Prague, 176 p., 7 pl.Google Scholar
Hicks, H. 1873. On the Tremadoc rocks in the neighborhood of St. David's. Quarterly Journal of the Geological Society of London, 29:3952, pls. 3–5.Google Scholar
Holub, K. 1908. Príspevek ku poznání fauny pásma Dd1. Rozpravy Ceské Akademie Ved Císare Frantiska Josefa Vedy, Slovesnost a Umeni, Trídy 2, Metematico-prírodovedecke, 17(10):119, 1 pl.Google Scholar
Holub, K. 1912. Additional remarks on the fauna from the Euloma horizon in the Rokycany area. Rozpravy České Akademie, 2, 21(33):12, 2 pls.Google Scholar
Howell, B. F. 1935. Cambrian and Ordovician trilobites from Hérault, southern France. Journal of Paleontology, 9:222238.Google Scholar
Jaanusson, V. 1956. Untersuchungen über baltoskandische Asaphiden. III. Über die Gattungen Megistaspis n. nom. und Homalopyge n. gen. Bulletin of the Geological Institutions of the University of Uppsala, 36:5977, figs. 1–3, pl. 1.Google Scholar
Jaekel, O. 1909. Über die Agnostiden. Zeitschrift der Deutschen Geologischen Gesellschaft, 61:380401.Google Scholar
Kobayashi, T. 1934. Journal of the Faculty of Sciences, Imperial University of Tokyo (section II), 3:521585, pls. 1–8.Google Scholar
Kobayashi, T. 1936. Three contributions to the Cambro–Ordovician faunas. I: The Dikelocephalininae (nov.), its distribution, migration and evolution. II: Notes on some Ordovician faunas of Tasmania. III: Brief remarks on the Cambro–Ordovician of Karakorum. Japanese Journal of Geology and Geography, 13:163184.Google Scholar
Kobayashi, T. 1937. The Cambro–Ordovician shelly faunas of South America. Journal of the Faculty of Science, Imperial University of Tokyo, section 2, 4:369522, 8 pls.Google Scholar
Kobayashi, T. 1939. On the agnostids (Part I). Journal of the Faculty of Sciences, Imperial University of Tokyo (section II), 5:69198.Google Scholar
Kobayashi, T. 1940. Lower Ordovician fossils from Caroline Creek, near Latrobe, Mersey River district, Tasmania. Papers Proceedings Royal Society of Tasmania for 1939:6776, pl. 12.Google Scholar
Kobayashi, T., and Hamada, T. 1978. Upper Ordovician trilobites from the Langkawi Islands, Malaysia. Geology and Palaeontology of Southeast Asia, 19:127.Google Scholar
Koroleva, M. N. 1982. Trilobity Ordovika Severo-Vostochnogo Kazakhstana. Nedra, Moskva, 192 p., 26 pls.Google Scholar
Lake, P. 1906. British Cambrian trilobites. Monograph of the Palaeontographical Society, Part 1(1906):128, pls. 1, 2.Google Scholar
Linnarsson, J. G. O. 1869. Om Vestergötlands Cambriska och Siluriska aflagringar. Kongliga Svenska Vetenskaps–Akademiens Handlingar, 8(2):189, pls. 1, 2.Google Scholar
Lochman, C., and Duncan, D. 1944. Early Upper Cambrian faunas of central Montana. Geological Society of America Special Papers, 54:1181, pls. 1–19.Google Scholar
Lu, Y. 1964. Trilobita, p. 2653. In Bian, Zhu, Yu, Wang, and Ji, Bian (eds.), A Handbook of the Index Fossils from South China. Nanjing Institute of Geology and Palaeontology, Academia Sinica, Beijing. (In Chinese) Google Scholar
Lu, Y. 1975. Ordovician trilobite faunas of central and southwestern China. Palaeontologica Sinica, n. s. B, 11:1463.Google Scholar
Marek, L. 1961. The trilobite family Cyclopygidae Raymond in the Ordovician of Bohemia. Vydal Ústredni Ústav Gologický, 28:185.Google Scholar
M'Coy, F. 1846. A Synopsis of the Silurian Fossils of Ireland. Dublin, 72 p., 5 pls.Google Scholar
M'Coy, F. 1849. On the classification of some British fossil Crustacea with notices of some new forms in the University collection at Cambridge. Annals and Magazine of Natural History, series 2, 4:161179, 330–335, 392, 414.Google Scholar
Miquel, J. 1912. Nouvel essai sur la géologie des terrains primaires du département de l'Hérault. Classification des terrains siluriens. Bulletin de la Société d'Etudes Scientifiques de Béziers, 34:148.Google Scholar
Nielsen, A. T. 1997. A review of Ordovician agnostid genera (Trilobita). Transactions of the Royal Society of Edinburgh, Earth Sciences, 87:463501.Google Scholar
Novák, O. 1883. Zur Kenntnis der böhmischen Trilobiten. Beitraege zur Palaeontologie Oesterreich-Ungans und des Orients, 3:2363, pls. 8–12.Google Scholar
Öpik, A. A. 1967. The Mindyallan Fauna of northwestern Queensland. Bureau of Mineral Resources, Geology and Geophysics Bulletin, 74, 1:1404.Google Scholar
Owen, A. W., and Parkes, M. A. 2000. Trilobite faunas of the Duncannon Group: Caradoc stratigraphy, environments and palaeobiogeography of the Leinster Terrane, Ireland. Palaeontology, 43:219269.Google Scholar
Palmer, A. R. 1955. Upper Cambrian Agnostidae of the Eureka District, Nevada. Journal of Paleontology, 29:86101.Google Scholar
Pek, I. 1977. Agnostid trilobites of the central Bohemian Ordovician. Sborník Geologickych Ved, Geologie, 1977(19):744, pls. 1–12.Google Scholar
Peng, S. 1990a. Tremadoc stratigraphy and trilobite faunas of northwestern Hunan. 1. Trilobites from the Nantsinkwan Formation of the Yangtze Platform. Beringeria, 2:353.Google Scholar
Peng, S. 1990b. Tremadoc stratigraphy and trilobite faunas of northwestern Hunan. 2. Trilobites from the Panjiazui Formation and the Madaoyu Formation in Jiangnan Slope Belt. Beringeria, 2:55171.Google Scholar
Perner, J. (ed.). 1918. Trilobiti pásma D-dly z okoli Prazského (Die Trilobiten der Zone D-dly von Prag und Umgebung). Palaeontograhica Bohemiae, 9:155.Google Scholar
Pompeckj, J. F. 1901. Aus dem Tremadoc der Montagne Noire (Süd-Frankreich). Neues Jahrbuch für Mineralogie, Geologie und Paläontologie, 1:18.Google Scholar
Prantl, F., and Pribyl, A. 1950. On the genus Symphisurus Goldfuss and allied forms from the Ordovician of Bohemia (Trilobitae). Letters et Sciences de Bohême (Praha), 12(1948):116, 2 pls.Google Scholar
Rábano, I., Pek, I., and Vanek, J. 1985. New Agnostina (Trilobita) from the Llanvirn (Ordovician) of Spain. Estudios Geológicos, 41:439445.CrossRefGoogle Scholar
Raymond, P. E. 1905. Trilobites of the Chazy Limestone. Annals of the Carnegie Museum (Pittsburgh), 3:328396, pls. 10–14.CrossRefGoogle Scholar
Raymond, P. E. 1912. Notes on parallelism among the Asaphidae. Transactions of the Royal Society of Canada Proceedings, section 4, series 3, 5:111120.Google Scholar
Reed, F. R. C. 1931. A review of the British species of Asaphidae, Pt. 2. Annals and Magazine of Natural History (London), series 10, 7:441472.Google Scholar
Remane, J. 2003. Chronostratigraphic correlations: Their importance for the definition of geochronologic units. Palaeogeography, Palaeoclimatology, Palaeoecology, 3081:112.Google Scholar
Robison, R. A. 1964. Late Middle Cambrian faunas from western Utah. Journal of Paleontology, 38:510566.Google Scholar
Rushton, A. W. A. 1988. Tremadoc trilobites from the Skiddaw Group in the English Lake District. Palaeontology, 31:677698.Google Scholar
Rushton, A. W. A., and Hughes, C. P. 1981. The Ordovician trilobite fauna of the Great Paxton Borehole, Cambridgeshire. Geological Magazine, 118:623646.Google Scholar
Salter, J. W. 1864. A monograph of British Trilobites, Pt. 1. Monograph of the Palaeontographical Society, p. 180, pls. 1–6.Google Scholar
Salter, J. W. 1866. A monograph of British Trilobites, Pt. 3. Monograph of the Palaeontographical Society, p. 129176, pls. 15–25.Google Scholar
Sars, M. 1835. Ueber einige oder unvollständig bekännte Trilobiten. Isis, Jena, Leipzig, 28(4):333343, pl. 9.Google Scholar
Sdzuy, K. 1955. Die Fauna der Leimitz–Schiefer (Tremadoc). Abhandlungen der Senckenbergischen naturforschenden Gesellschaft, 492:174.Google Scholar
Sdzuy, K. 1958. Fossilien aus dem Tremadoc der Montagne Noire. Senckenbergiana Lethaea, 39(3–4):255285.Google Scholar
Shergold, J. H. 1972. Late Upper Cambrian trilobites from the Gola Beds, western Queensland. Bulletin of the Bureau of Mineral Resources, Geology and Geophysics, 112, 127 p., 19 pls.Google Scholar
Shergold, J. H. 1975. Late Cambrian and Early Ordovician trilobites from the Burke River Structural Belt, western Queensland, Australia. Bulletin of the Bureau of Mineral Resources, Geology and Geophysics, 153(1), 251 p.Google Scholar
Shergold, J. H., Laurie, J. R., and Sun, X. 1990. Classification and review of the trilobite Order Agnostida Salter, 1864: An Australian perspective. Report of the Bureau of Mineral Resources, Geology and Geophysics, 296:193.Google Scholar
Shirley, J. 1936. Some British trilobites of the family Calymenidae. Quarterly Journal of the Geological Society of London, 92:384422, pls. 29–31.Google Scholar
Stubblefield, C. J., and Bulman, O. M. B. 1927. The Shineton Shales of the Wrekin district: With notes on their development in other parts of Shropshire and Herefordshire. Quarterly Journal of the Geological Society of London, 83:96146, pls. 3–5.Google Scholar
Sun, Yun-zhu. 1931. Ordovician trilobites of central and southern China. Palaeontologia Sinica, B, 7:1243.Google Scholar
Thoral, M. 1935. Contribution à l'étude Paléontologique de l'Ordovicien Inférieur de la Montagne Noire et Révision Sommaire de la Faune Cambrienne de la Montagne Noire. Imprimerie de la Charité, Montpellier, 362 p.Google Scholar
Thoral, M. 1941. Stratigraphie et faciès de l'Arenig languedocien. Annales des Sciences Naturelles de l'Université de Lyon, section C, 2:99149.Google Scholar
Tjernvik, T. E. 1956. On the Early Ordovician of Sweden. Bulletin of the Geological Institutions of the University of Uppsala, 36(2–3):107284, pls. 1–11.Google Scholar
Tortello, M. F. 1996. Trilobites agnóstidos del Tremadociano superior alto (Ordovícico Inferior) del noroeste argentino. Memorias del XII Congreso Geológico Boliviano, Tarija, 1:203209.Google Scholar
Tortello, M. F., and Esteban, S. B. 1995. Un trilobite agnóstido en el Ordovícico de la región de Bordo Atravesado (Cuesta de Miranda), Provincia de La Rioja, Argentina. VI Congreso Argentino de Paleontología y Bioestratigrafía, Trelew, Actas, p. 271275.Google Scholar
Tortello, M. F., and Esteban, S. B. 2003. Lower Ordovician stratigraphy and trilobite faunas from the southern Famatina Range, La Rioja, Argentina. Special Papers in Palaeontology, 70:213239.Google Scholar
Vanek, J. 1965. Die Trilobiten des mittelböhmischen Tremadoc. Senckenbergiana Lethaea, 46(4–6):263308.Google Scholar
Vizcaïno, D., and Álvaro, J. J. 2003 (for 2002). Adequacy of the Lower Ordovician trilobite record in the southern Montagne Noire (France): Biases for biodiversity documentation. Transactions of the Royal Society of Edinburgh: Earth Sciences, 93:393401.Google Scholar
Vizcaïno, D., Álvaro, J. J., and Lefebvre, B. 2001. The Lower Ordovician of the southern Montagne Noire. Annales de la Société Géologique du Nord (2e série), 8(4):213220.Google Scholar
Walcott, C. D. 1924. Cambrian Geology and Paleontology V, 2: Cambrian and Lower Ozarkian trilobites. Smithsonian Miscellaneous Collections, 75(2):5360, pls. 9–14.Google Scholar
Whittard, W. F. 1955. The Ordovician trilobites of the Shelve inlier, west Shropshire, Pt. 1. Monograph of the Palaeontographical Society, 109(470):140, pls. 1–4.Google Scholar
Whittard, W. F. 1961. The Ordovician trilobites of the Shelve inlier, west Shropshire, Pt. 5. Monograph of the Palaeontographical Society, 114(1):163196, pls. 22–25.CrossRefGoogle Scholar
Whittard, W. F. 1966. The Ordovician trilobites of the Shelve inlier, west Shropshire, Pt. 8. Monograph of the Palaeontographical Society, 114(1):265306, pls. 46–50.Google Scholar
Whittington, H. B. 1965. Trilobites of the Ordovician Table Head Formation, western Newfoundland. Bulletin of the Museum of Comparative Zoology, 132:275441, pls. 1–68.Google Scholar
Whittington, H. B., Chang, W. T., Dean, W. T., Fortey, R. A., Jell, P. A., Laurie, J. R., Palmer, A. R., Repina, L. N., Rushton, A. W. A., and Shergold, J. H. 1997. Systematic descriptions of the class Trilobita, p. 331481. In Kaesler, R. L. (ed.), Treatise on Invertebrate Paleontology. Pt. O. Arthropoda, 1, Trilobita (revised). Vol. 1. Geological Society of America and University of Kansas Press, Lawrence.Google Scholar
Zhou, Tianmei, Yiren, Liu, Xiansong, Meng, and Zhenhua, Sun. 1977. Trilobita, p. 140266. In Palaeontological Atlas of Central and South China. Vol. 1. Geological Publishing House, Beijing. (In Chinese) Google Scholar
Zhou, Zhiyi. 1987. Notes on Chinese Ordovician agnostids. Acta Palaeontologica Sinica, 26:639661.Google Scholar