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Smith, Longridge, Grey, Zhang, Liang Lethaia 2014 REFERENCES FOR DATA SOURCES Arkell, W. J., B. Kummel and C. W. Wright. 1957. Mesozoic Ammonoidea. Pp. L80-L465 in W. J. Arkell et al. Mollusca 4, Cephalopoda, Ammonoidea. Part L of R. C. Moore, ed. Treatise on invertebrate paleontology. Geological Society of America, New York, and University of Kansas, Lawrence. Arthur, A.J., P.L. Smith, J.W.H. Monger and H.W. Tipper. 1993 Mesozoic stratigraphy and Jurassic paleontology west of Harrison Lake, southwestern British Columbia. Geological Survey of Canada Bulletin 441: 62 p. Blau, J., C. Meister, R. Schlatter and R. Schmidt-Effing. 2001. Ammonites from the Lower Jurassic (Sinemurian) of Tenango de Doria (Sierra Madre Oriental, Mexico). Part I: Erbenites n. g., a new Asteroceratinae. Neues Jahrbuch fur Geologie und Palaeontologie Monat Shefte 3:175-183. Bloos, G. 1994. Frühe Arietitidae (Ammonoidea) aus dem Hettangium (Angulata-Zone, Unt. Lias) von Württemberg (SW-Deutschland). Stuttgarter Beiträge zur Naturkunde, Serie B (Geologie und Pälaontologie) 219:1-67, 4 pls. Buckman, S. S. 1918. Jurassic Chronology: I - Lias. Quarterly Journal of the Geological Society of London 73:257–327. Callomon, J. H. and R. B. Chandler. 1990. A review of the ammonite horizons of the Aalenian – Lower Bajocian Stages in the Middle Jurassic of southern England. In S. Cresta and G. Pavia, coords. Memoire descrittive della Carta Geologica D’Italia XL:85-112. Callomon, J. H. and J.K. Wright 1989 Cardioceratid and Kosmoceratid ammonites from the Callovian of Yorkshire. Palaeontology 32: 88-96. Canavari, M. 1882. Beiträge zur Fauna des unteren Lias von Spezia. Palaeontographica 29:125- 192, pls 15-21. Corna, M. and J.-L. Dommergues. 1995. Les ammonites du Sinémurien de Mandelot (Cote- D’Or, France). Approches biostratigraphique, morphologique et ontogénétique. Geobios 28:17-47. ____, ____, C. Meister and R. Mouterde. 1997. Sinémurien. In E. Cariou and P. Hantzpergue, coords. Groupe Français d’Études du Jurassique, biostratigraphie du Jurassique ouest-européen et méditerranéen. Zonations parallèles et distribution des invertébrés et microfossiles. Bulletin des Centres de Recherches-Exploration Production d’Elf-Aquitaine Mémoire 17:pl. 2. Cresta, S. 2002. Accardia; Alocolytoceras; Calliphylloceras; Lytoceras; Megalytoceras; Paviaites; Phylloceras; Planammatoceras; Tatroceras. In G. Pavia and S. Cresta, eds. Revision of Jurassic ammonites of the Gemmellaro collections. Quaderni del Museo Geologico "G.G. Gemmellaro" 6: 27, 42-44, 70-71, 92, 100-103, 181-182, 186-187, 190-191. Dagis, A. A. 1968. Toarcian ammonites (Dactylioceratidae) of Northern Siberia. Doklady Akademii Nauk SSSR, 108 p., 12 pls. (In Russian) Dommergues, J.-L., C. Meister and F. Böhm. 1995. New data on Austroalpine Liassic ammonites from the Adnet Quarries and adjacent areas (Oberösterreich, Northern Calcareous Alps). Jahrbuch der Geologischen Bundesanstalt A 138:161-205. ____, ____ and R. Mouterde. 1997. Pliensbachian. In E. Cariou and P. Hantzpergue (Coords.), Groupe Français d’Études du Jurassique, biostratigraphie du Jurassique ouest-européen et méditerranéen. Zonations parallèles et distribution des invertébrés et microfossiles. Bulletin des Centres de Recherches-Exploration Production d’Elf-Aquitaine Mémoire, 17:pls. 6-7. Donovan, D. T. and G. F. Forsey. 1973. Systematics of Lower Liassic Ammonitina. University of Kansas Paleontological Contributions 64, 18 p., 4 pls. ____ and F. Surly. 2003. Lower Jurassic (Pliensbachian) ammonites from Bornholm, Baltic Sea, Denmark. Geological Survey of Denmark and Greenland Bulletin 1:555–583. Elmi, S. and R. Mouterde. 1997. Les faunes de Czernyeiceras (Hammatoceratinae, Ammonitina) à la limite du Toarcien et de L’Aalénien. Université Catholique de Lyon 10:103-116. ____, L. Rulleau, J. Gabilly and R. Mouterde. 1997. Toarcien. In E. Cariou and P. Hantzpergue (Coords.), Groupe Français d’Études du Jurassique, biostratigraphie du Jurassique ouest- européen et méditerranéen. Zonations parallèles et distribution des invertébrés et microfossiles. Bulletin des Centres de Recherches-Exploration Production d’Elf-Aquitaine Mémoire, 17:pl. 11. Faraoni, P., A. Marini, G. Pallini and F. Venturi. 1994. Pp. 247-297. Nuove faune ad ammonite delle zone ad E. mirabilis ed H. serpentinus nella Valle del F. Bosso (PS) e loro reflessi sulla biostratigrafia del limite Domeriano-Toarciano in Appennino. Studi Geologici Camerti volume speciale, “Biostratigrafia dell’Italia centrale”. Fauré, P. 2002. Le Lias des Pyrénées. Actes du Laboratoire de Géologie Sédimentaire et Paléontologie de l’Université Paul-Sabatier Toulouse, Strata II, 39, 761 p., 25 pls. Fernandez-Lopez, S. and R. Mouterde. 1994. Miscellanea del Servizio Geologico Nazionale 5:117-159. Frebold, H. 1951. Contributions to the paleontology and stratigraphy of the Jurassic System in Canada. Geological Survey of Canada Bulletin 18, 54 p. ____. 1964. Illustrations of Canadian fossils, Jurassic of Western and Arctic Canada. Geological Survey of Canada Paper 63-4, 107 p. ____. 1967. Hettangian ammonite faunas of the Taseko Lakes area, British Columbia. Geological Survey of Canada Bulletin, 158, 35 p., 9 pls. Galácz, A. 1994. Lokuticeras nov. gen. – a new genus for a Mediterranean Bajocian (Middle Jurassic) stephanoceratid ammonite group. Miscellanea del Servizio Geologico Nazionale 5:161-175. ____, B. Géczy and M. Monostori. 2008. Csernye revisited: New ammonite finds and ostracods from the Lower Jurassic Pliensbachian/Toarcian boundary beds in Bakonycsernye, Transdanubian Hungary. Geologica Pannonica 36:187-225. Géczy, B. and C. Meister. 2007. Les ammonites du Sinémurien et du Pliensbachien inférieur de la montagne du Bakony (Hongrie). Revue de Paléobiologie 26:137-305. Gil, M. S. U. 1985. Bioestratigrafia y paleontologia (Ammonitina) del Aaleniense en el sector noroccidental de la Cordillera Iberica. Unpublished Ph.D. dissertation, Universidad Complutense de Madrid, 452 p., 34 pls. Guérin-Franiatte, S. 1990. Ammonites du Lias inférieur de France (II): Psiloceratidae, Schlotheimiidae et premiers Arietitidae. Centre d’Etude et de Recherches Geologique et Hydrologiques Mémoire 29, 207 p., 30 pls. Guex, J. 1972. Répartition biostratigraphique des ammonites du Toarcien moyen de la bordure sud des Causses (France) et révisions des ammonites décrites et figurées par Monestier (1931). Eclogae geologicae Helvetiae 65:611-645, 13 pls. ____. 1975. Description biostratigraphique du Toarcien supérieur de la bordure sud des Causses (France). Eclogae geologicae Helvetiae 68:97-129, 12 pls. ____. 1995. Ammonites Hettangiennes de la Gabbs Valley Range (Nevada, USA). Géologie Lausanne Mémoires 27, 131 p. ____. 2000. Paronychoceras gen. n., un nouveau genre d’ammonites (Cephalopoda) du Lias supérieur. Société Vaudoise des Sciences Naturelles Bulletin 87.2:115-124. Hall, R. L. and G. E. G. Westermann. 1980. Lower Bajocian (Jurassic) cephalopod faunas from western Canada and proposed assemblage zones for the Lower Bajocian of North America. Palaeontographica Americana 9(52), 93 p. Henriques, M. H. 2000. Aalenian of the Zambujal de Alcaria Section (Central Lusitanian Basin; Portugal). Pp. 85-94 in R. L. Hall and P. L. Smith, eds. Advances in Jurassic Research 2000. Proceedings of the Fifth International Symposium on the Jurassic System. GeoResearch Forum 6. Trans Tech, Switzerland. Hillebrandt, A. Von. 2000. Die ammoniten-fauna des südamerikanischen Hettangium (basaler Jura). Palaeontographica, Abteilung A, Teil 257:85-189, 14 pls; Teil 258:65-116, 12 pls; Teil 258:1-64, 16 pls. ____. 2002. Ammoniten aus dem oberen Sinemurium von Südamerika. Revue de Paléobiologie 21:35-147. ____. 2006. Pliensbachian ammonites of South America. Revue de Paléobiologie 25:1-403. ____ and Westermann, G. E. G. 1985. Aalenian (Jurassic) ammonite faunas and zones of the Southern Andes. Zitteliana 12:3-55. Howarth, M. K. 1992. The ammonite family Hildoceratidae in the Lower Jurassic of Britain. Part 2. Monograph of the Palaeontographical Society London 146:107-200, 38 pls. Imlay, R. W. 1953. Callovian (Jurassic) ammonites from the United States and Alaska-Part 2. Alaska Peninsula and Cook Inlet regions. U.S. Geological Survey Professional Paper 249B: 25-55, plates 25-55. ____. New genera and subgenera of Jurassic (Bajocian) ammonites from Alaska. Journal of Paleontology 35:467-474, pls 63-64. ____. 1962. Late Bajocian ammonites from the Cook Inlet Region, Alaska. U.S. Geological Survey Professional Paper 418-A:A1-A14, 5 pls. ____. 1964. Middle Bajocian ammonites from the Cook Inlet Region, Alaska. U.S. Geological Survey Professional Paper 418-B:B1-B61, 29 pls. ____. 1980. Middle Jurassic (Bathonian) ammonites from southern Alaska. U.S. Geological Survey Professional Paper 1091: 42 p., 12 pls. ____. 1981. Jurassic (Bathonian and Callovian) ammonites in eastern Oregon and western Idaho. U.S. Geological Survey Professional Paper 1142: 24 p., 5 pls. ____. 1982. Late Bajocian ammonites from Southern Alaska. U.S. Geological Survey Professional Paper 1189, 19 p., 7 pls. Irnstorfer, O. 2005. Trias-ammoniten aus den Hallstätter Kalken. Fossilien 6:361-368. Jakobs, G. K. 1997. Toarcian (Early Jurassic) ammonoids from Western North America. Geological Survey of Canada Bulletin 428, 137 p. ____ and P. L. Smith. 1996. Latest Toarcian ammonoids from the North American Cordillera. Palaeontology 39:97-147. Johnston, F. N. 1941. Trias at New Pass, Nevada (new Lower Karnic Ammonids). Journal of Paleontology 15:447-491. Konstantinov, A. G. 1995. Arctophyllites, a new genus of
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  • Austroalpine Liassic Ammonites from the Adnet Formation (Northern Calcareous Alps) 163-211 ©Geol

    Austroalpine Liassic Ammonites from the Adnet Formation (Northern Calcareous Alps) 163-211 ©Geol

    ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Jahrbuch der Geologischen Bundesanstalt Jahr/Year: 1993 Band/Volume: 136 Autor(en)/Author(s): Meister Christian, Böhm Florian Artikel/Article: Austroalpine Liassic Ammonites from the Adnet Formation (Northern Calcareous Alps) 163-211 ©Geol. Bundesanstalt, Wien; download unter www.geologie.ac.at Jb. Geol. B.-A. ISSN 0016-7800 Band 136 S.163-211 Wien, Juli 1993 Austroalpine Liassic Ammonites from the Adnet Formation (Northern Calcareous Alps) By CHRISTIAN MEISTER & FLORIAN BÖHM *) With 14 Text-Figures and 9 Plates Oslerreich Salzburg Oberöslerreich Nördliche Kalkalpen Lias Ammoniten Oslerreichische Karle 1. 50.000 Biostratigraphie BI/1l1er94, 95, 96,126 Palaeogeographie Contents Zusammenfassung 163 Abstract. .. 164 Resume 164 1. Introduction 164 2. Geographical and Geological Framework 164 3. Lithological Description and Qualitative/Quantitative Ammonite Distributions 165 3.1. Schmiedwirt Quarry 165 3.2. Breitenberg Quarry 166 3.3. Rotkogel Outcrop 166 3.4. Rötelstein Outcrop 168 4. Systematic Palaeontology 169 PhylioceratinaARKELL 1950 171 LytoceratinaHYATT1889 174 Ammonitina HYATT 1889 175 5. Biostratigraphical Framework 184 5.1. Sinemurian 184 5.1.1. Early Sinemurian 184 5.1.2. Late Sinemurian 184 5.2. Pliensbachian 184 5.2.1. Early Pliensbachian (Carixian) 184 5.2.2. Late Pliensbachian (Domerian) 186 5.3. Toarcian 186 6. Faunal Composition and Palaeogeographical Remarks 189 7. Conclusion 190 Acknowledgements 190 References 208 Oberostalpine Liasammoniten aus der Adnetformation (Nördlichen Kalkalpen) Zusammenfassung Das Oberostalpin spielt eine Schlüsselrolle für das Verständnis der Verteilungsmuster der jurassischen Ammonitenfaunen und für die Fixierung genauer biostratigraphischer Korrelationen zwischen Tethyaler und Euroborealer Faunenprovinz.
  • Paleontological Research of the Mesozoic in Uie Central Zone And

    Paleontological Research of the Mesozoic in Uie Central Zone And

    Západně Karpaty • séria paleontológia (1) • P. 7—23 • GÚDŠ • Bratislava • 1975 Miloš Rakús Hettangian ammonites from the Strážovská hornatina Mts. (West Carpathians) 1 plate (CIV), 10 text-figs, Slovak summary The thorough geological — paleontological research of the Mesozoic in uie central zone and particularly in the Strážovská hornatina mountains resulted in detailed knowledge of the Hettangian Ammonites. Conse­ quently, a summarizing report may be presented on the ammonites. The first, and for considerable time the only published report on the Hettangian Ammonites was that by D. Stúr (1868, p. 378) from the loca­ lity Rakytov (the Velká Fatra mountains), viz A. psilonotus laevis (Q u .) = Psiloceras psilonotum (Quenstedt). Unfortunately, the find has not been repeated so far. Still I suppose that in this case its presence might be regarded as probable, since: a) the species Psiloceras psilonotum is a typical, easily identifiable form, and it is almost impossible to mistake it for another species; b) on the locality Rakytov are well-developed se­ quences of the Upper Triassic (the Rhaetic) to Lower Liassic. Both they yielded rich fauna of lamellibranchiates, so the presence of the Hettan­ gian may be taken for sure there. In the sixties (M. Rakús in M. Mahel 1962; V. Andrusovová —D. Andrusov 1968) published were some reports on the finds of the Hettangian Ammonites from the central zone. In the central zone of the West Carpathians, most Hettangian Ammonites come from the Strá­ žovská hornatina mountains (Central Slovakia). Other finds are from these localities: — the vicinity of Cierna Lehota (text — fig. 1); — Kozinec (text — fig. 2); — Trencianska Teplá.
  • Paleontological Contributions

    Paleontological Contributions

    THE UNIVERSITY OF KANSAS PALEONTOLOGICAL CONTRIBUTIONS May 15, 1970 Paper 47 SIGNIFICANCE OF SUTURES IN PHYLOGENY OF AMMONOIDEA JURGEN KULLMANN AND JOST WIEDMANN Universinit Tubingen, Germany ABSTRACT Because of their complex structure ammonoid sutures offer best possibilities for the recognition of homologies. Sutures comprise a set of individual elements, which may be changed during the course of ontogeny and phylogeny as a result of heterotopy, hetero- morphy, and heterochrony. By means of a morphogenetic symbol terminology, sutural formulas may be established which show the composition of adult sutures as well as their ontogenetic development. WEDEKIND ' S terminology system is preferred because it is the oldest and morphogenetically the most consequent, whereas RUZHENTSEV ' S system seems to be inadequate because of its usage of different symbols for homologous elements. WEDEKIND ' S system includes only five symbols: E (for external lobe), L (for lateral lobe), I (for internal lobe), A (for adventitious lobe), U (for umbilical lobe). Investigations on ontogenetic development show that all taxonomic groups of the entire superorder Ammonoidea can be compared one with another by means of their sutural development, expressed by their sutural formulas. Most of the higher and many of the lower taxa can be solely characterized and arranged in phylogenetic relationship by use of their sutural formulas. INTRODUCTION Today very few ammonoid workers doubt the (e.g., conch shape, sculpture, growth lines) rep- importance of sutures as indication of ammonoid resent less complicated structures; therefore, phylogeny. The considerable advances in our numerous homeomorphs restrict the usefulness of knowledge of ammonoid evolution during recent these features for phylogenetic investigations.
  • Paleontological Journal

    Paleontological Journal

    ISSN 0031-0301 PALEONTOLOGICAL JOURNAL A TRANSLATION OF UDC 564.53 Paleontological Journal, 25(4), 1991 HIGHER TAXA OF JURASSIC AND CRETACEOUS AMMONITIDA N. V. Besnosov and I. A. Michailova All-Union Petroleum Geological Exploration Institute; Moscow University Abstract: The division of the order Ammonitida into the four suborders Ammonitina Hyatt, 1889, Haploceratina Besnosov et Michailova, 1983, Perisphinctina Besnosov et Michailova, 1983 and Ancyloceratina Wiedmann, 1966 is substantiated, and the phylogenetic relationships among the suborders and superfamilies are considered. • • • This article completes the systematics of taxa of ordinal, subordinal and superfamilial ranks of the Jurassic and Cretaceous ammonoids that we began in previous publications [3-5). These set forth the history of the problem and the current ideas on the system of the Jurassic and Cretaceous ammonoids, and consider the orders Phylloceratida and Lytoceratida, within the latter of which the independence of the suborder Turrilitina is documented. We believe that the Jurassic and Cretaceous ammonoids should be regarded as belonging to three orders: the Phylloceratida, Lytoceratida and Ammonitida. The first of these orders is small in volume and includes only one superfamily; the second is divided into two suborders and four superfamilies; and the third and largest order, the Ammonitida, combines four suborders and 15 superfamilies (fig. 1 ). The present system of the higher taxa of the Jurassic and Cretaceous ammonoids was described in the Treatiseon InvertebratePaleontology [25] and the SovietPrinciples of Paleontology [12, 13]. Substantial changes were later subsequently introduced into it by Schindewolf [23] and Wiedmann [26, 27], and also by Donovan, Callomon and Howarth [15]. The revision of the taxa of ordinal and familial rank proposed here is based primarily on phylogenetic research both in and outside the Soviet Union during the last three decades [4].