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Literaturverzeichnis Mit Asterisk bezeichnete Arbeiten sind besonders von Revisionen in systematischer und/oder bio stratigraphischer Hinsicht betroffen, oder dienten als Grundlage für die Korrelation auf Tabelle 4. ACCORSI BENINI, C. & BROGLIO LORIGA, C. (1977): Lithiotis Güm• BOULE, M. & THEVENIN, A. (1906,1907): Types du Prodrome de Pale­ bel, 1871 e Cochlearites Reis, 1903. 1°. Revisione morfologica e ontologie universelle de d'Orbigny. - Ann. Paleont., 1, p. 97-100, tassonomica. - Boll. Soc. paleont ital., 16, 1, p. 15-60. 165-172, 193-196, Taf. 8, 9, 12, 13, 21, 22; 2, p. 89-96, 161-172, AGER, D. V. & CALLOMON, J. H. (1971): On the Liassie age of the Taf. 13,14,23,24. "Bathonian" of Villäny (Baranya). - Ann. Univ. Sei. Budapest BOURDENET, A. M. (1964): Les Pleuroceras du Domerien superieur Eötvös, Sect geo!., 14, p. 5-16. de Charrnoille (Haute-Saöne). - Ann. sei. Univ. Besan~on, (2) 18, ARKELL, W. J. (1956): Jurassie geology of the world. - London and p.3-24. Edinburgh (Oliver & Boyd). *BREMER, H. (1965): Zur Ammonitenfauna und Stratigraphie des ARKELL, W. J., BRAMKAMP, R. A. & STEINEKE, M. (1952): Jurassie unteren Lias (Sinemurium bis Carixium) in der Umgebung von Ammonites from Jebel Tuwaiq, central Arabia. - Phi!. Trans. r. Ankara (Türkei). - N. Jb. Geol. Paläont., Abh., 122, S. 127-221. Soc. London, (B) 236, p. 241-313. BUCKMAN, S. S. (1918): Jurassie chronology: I. Lias. - Quart 1. geol. *ARKELL, W. J., KUMMEL, B. & WRIGHT, C. W. (1957): Mesozoic Soc. London, 73 (1917), p. 257-327. Ammonoidea. In: MOORE, R. C. (Ed.): Treatise on invertebrate - (1909-30): Yorkshire Type Ammonites (ab vol. 3: Type Ammo­ paleontology, (L) Mollusca 4 (p. L80-L490). - Geo!. Soc. Amer. nites). - London (Wheldon & Wesley), vol. 1-7. (Daten der ein­ & Univ. Kansas Press. zelnen Teile: s. DEAN et al. 1961: 498f.; HOWARTH 1962a: 135f.). ATROPS, F., DUBEL, C., ELMI, S. & REVERT, J. (1970): La limite Do­ CALLOMON, J. H. & DONOVAN, D. T. (1974): A code of Mesozoie merien-Toareien et l'apparition de la sedimentation marneuse stratigraphical nomenclature. - Mem. Bur. Rech. geo!. min., 75 dans Je Lias des Monts de Rhar-Roubane (Ouestalgerien). - Bull. (Colloque du Jurassique, Luxembourg, 1967), p. 75-81. Soc. Hist. nat. Afrique Nord, 61,3-4, p. 9-18. CANTALUPPI, G. (1966): Fossili sinemuriani e domeriani nel «Corso ATROPS, F. & ELMI, S. (1971): Les divisions chronostratigraphiques bianco» ad Est di Breseia. - Atti Ist. Geol. Univ. Pavia, 17, p. 103 de I'Oranie oceidentale (Algerie) etIeur correlations. - C. R. Acad. bis 120. Sei. Paris, (D) 273, p. 2422. - (1967 a): Le ammoniti domeriane della Val Ceppelline (Suello - AUBOUIN, 1., BLANCHET, R., STEPHAN, 1.-F. & TARDY, M. (1977): Prealpi Lombarde). - Atti Ist. Geol. Univ. Pavia, 18, p. 1-50. Tethys (Mesogee) et Atlantique: donnees de la geologie. - - (1967 b): AIcune ammoniti domeriane della bassa Valganna (Vare­ c. R. Acad. Sei. Paris, (D) 285, p. 1025-1028. sotto). - Atti Soc. ita!. Sei. nat Mus. eiv. Storia nat Milano, 106, BARBERA, C. (1968): Ammoniti giurassiei dei Gran Sasso edelI'Aqui­ 3, p. 216-231. lano. - Atti Accad. Sei. fis. mat. Napoli, (3) 6, 3, p. 227-313. - (1968): Illimite paleontologico Domeriano-Toardano a Molvina *BEHMEL, H. & GEYER, O. F. (1966): Beiträge zur Stratigraphie und (Est di Breseia). - Atti Soc. ital. Sei. nat. Mus. eiv. Storia nat. Paläontologie des Juras von Ostspanien. III. Stratigraphie und Milano, 107,2, p. 153-158. Fossilftihrnng im Unterjura von Albarracin (Provinz Terne!). - - *(1970): Le Hildoceratidae dei Lias medio delle regioni mediter­ N. Jb. Geo!. Paläont, Abh., 124,1, S. 1-62. ranee. Loro successione e modificazioni nel tempo. Riflessi bio­ BERNOULLI, D. (1964): Zur Geologie des Monte Generoso (Lombar­ stratigrafici e sistematici. - Mem. Soc. ital. Sei. nat. Mus. civ. dische Alpen). Ein Beitrag zur Kenntnis der südalpinen Sedi­ Storia nat Milano, 19, 1, p. 7-46. mente. - Beitr. geo!. Karte Schweiz, (N. F.) 118. - *(1972): Revisione di «Grammoceras» bassanii, controversa speeie­ - (1967): Lombardischer Kieselkalk. In: PRUVOST, P. & RUTSCH, tipo dei generi d'ammoniti Protogrammoceras e Bassaniceras. - R. F. (Ed.): Lexique stratigraphique international, vol. 1/7 c, Atti Soc. ital. Sei. nat Mus. eiv. Storia nat. Milano, Jl3, 4, p. 335- Europe/Suisse/Alpes Suisses et Tessin meridional (p. 701-703). - 356. Centre National de la Recherche Seientifique, Paris. *CANTALUPPI, G. & BRAMBILLA, G. (1968): Le ammoniti dei Ripian­ BERNOULLI, D. & JENKYNS, H. C. (1974): Alpine, Mediterranean and tino (SaItrio) edella Breggia (Canton Tieino). Riflessi bio strati­ central Atlantic Mesozoie faeies in relation 10 the early evolution grafiei sul Domeriano ed il suo limite inferiore. - Atti Soc. ita!. ofthe Tethys. In: DOTT, R. H., J R. & SHA VER, R. H. (Eds.): Modern Sei. nat Mus. civ. Storia nat Milano, 107, 3-4, p. 277-315. and aneient geosynclynal sedimentation. - Spec. Pub!. Soc. econ. CANTALUPPI, G. & MONTANARI, L. (1969a): Carixiano superiore e Paelont Mineral., 19, p. 129-160. suo passaggio al Domeriano a NW di Arzo (Canton Tieino). - BERNOULLI, D. & WIEDENMAYER, F. (1967): Exkursion Nr. 26. Luga­ Boll. Soc. paleont ital., 7, p. 57-77. no-Mendrisio, Mendrisio-Arzo-Serpiano, Mendrisio-Breggia­ CANTALUPPI, G. & MONTANARI, L. (1969b): La serie domeriana della schlucht-Chiasso. In: SCHWEIZ. GEOL. GES. (Ed.): Geologischer Val Ceppelline (Alta Brianza). - Atti Soc. ital. Sei. nat. Mus. civ. Führer der Schweiz (S. 441-460). - Basel (Wept). Storia nat. Milano, 109, 3, p. 223-258. BETTONI, A. (1900): Fossili domeriani della Provineia di Breseia. - *CANTALUPPI, G. & MONTANARI, L. (1973): Quadro biostratigrafico Schweiz. paläont. Abh., 26. conclusivo dei Carixiano e suo passaggio al Domeriano nelle *BLAISON, J. (1967): Etudes biometriques et revision de l'espece Pro­ Prealpi lombarde occidentali. - Boll. Soc. paleont ital.,10, 2 (1971), togrammoceras madagascariense (THEVENIN 1908). Definition du p.43-74. nouveau genre Parahildaites. - Ann. sei. Univ. Besan~on, (3) 3, *CANTALUPPI, G. & SAVI, A. (1968): Le ammoniti di Molino Grasso p.59-ll5. d'Olona (Varesotto). Riflessi biostratigrafiei sul Domeriano ed il BONARELLI, G. (1899a): Cefalopodi Sinemuriani dell'Appennino suo limite superiore. - Atti Soc. ital. Sei. nat Mus. eiv. Storia centrale. - Palaeon1ogr. ital., 5, 1899 (1900), p. 55-83. nat. Milano, 107, 3, p. 205-261. - (1899b): Le Ammoniti dei «Rosso ammonitico» descritte e figu­ CASSINIS, G. (1968): Stratigrafia e tettonica dei terreni mesozoiei rate da Giuseppe Meneghini. - Bull. Soc. malac. ital., 20 (1895), compresi tra Brescia e Serie. - Atti Ist. geol. Univ. Pavia, 19, p.198-219. S.50-152. *BORDALO DARoCHA,R. (1970): UnMetaderoceras(Carixien) du Cap CITA, M., CASSINIS, G. & POZZI, R. (1961): Introduction a l'etude du S. Vicente (Algarve). - Bol. Soc. geol. Port., 17, p. 169-176. Domerien-Type. - Mem. Bur. Rech. geol. min., 4 (Colloque sur BÖSE, E. (1894): Über liasische und mitteljurassische Fleckenmergel le Lias fran~ais, Chambery, 1960), p. 323-344. in den bayerischen Alpen. - Z. dtsch. geol. Ges., 1894, S. 703-768. COLLIGNON, M. (1958): Atlas des fossiles caracteristiques de Mada- 181 gascar. Fasc. I (Lias, Bajocien). - Tananarive (Service Geolo­ Bur. Rech. geol. min., 4, (Colloque sur le Lias fran~ais, Chambery, gique). 196O),p.236-244,263-269. COLO, G. (1961): Contribution a l'etude du Jurassique du Moyen *Du DRESNAY, R. (1963): Quelques ammonites de la partie inferieure Atlas septentrional. - Notes Mem. Servo geol. Maroc, 139. du Pliensbachien (Carixien et Domerien pro parte) dujbel Bou­ DAGIS, A. A. (1968): Toarskiye ammonity (Dactylioceratidae) severa Rharraf (Haut Atlas oriental). - Notes Mem. Servo geol. Maroc, Sibiri. - Trudy Inst geol. geoftz. Sib. Otd. Akad. Nauk SSSR, 40. 23,172, p. 141-164. DEAN, W. T., DONOVAN, D. T. & HOWARTH, M. K. (1961): The *DUMORTIER, E. (1867,1869): Etudes paleontologiques sur les depots Liassic ammonite zones and subzones of the North-West Euro­ jurassiques du bassin du Rhone. 11. Lias-inferieur (1867). III. Lias­ pean Province. - Bull. brit. Mus. nat Hist. (Geol.), 4, 10, p. 435- moyen (1869). - Paris (Savy). 505. ERBEN, H. K. (1954): Dos amonitas nuevos y su importancia para la DEL CAMPANA, D. (1900): I cefalopodi deI Medolo di Valtrompia. - estratigrafia deI Juräsico inferior de Mexico. - Paleontologia Boll. Soc. geol. ital., 19, p. 555-644. mex., 1. DENCKMANN, A. (1887): Über geognostische Verhältnisse der Um­ - (1956): EI Juräsico inferior de Mexico y sus amonitas. - 20° Congr. gegend von Dörnten nördlich Goslar, mit besonderer Berück• geol. int Mexico. sichtigung der Fauna des oberen Lias. - Abh. geol. Spez.-Karte FANTINI SESTINI, N. (1962): Contributo aHo studio delle ammoniti Preussen thüring. Staaten, 8, 2 (Text + Atlas). deI Domeriano di M. Domaro (Brescia). - Riv. ital. Paleont Strat., *DEUTSCHE SUBKOMMISSION FÜR JURA-STRATIGRAPHIE (1973): F. 68, 4, p. 485-550. A. Quenstedt: die Ammoniten des Schwäbischen Jura. Revision - *(1975): Dactylioceratidae (Ammonoidea) deI Domeriano. - Riv. der Gattungsnamen und Untergattungsnamen. - Stuttgart ital. Paleont., 81, 4, p. 437-476. (Schweizerbart). FANTINI, N. & PAGANONI, C. (1953): Studi paleontologici sul Lias deI DONOVAN, D. T. (1954): Synoptic supplement to T. Wrighfs ''Mono­ Monte Albenza. Ammoniti deI Lothringiano edel Domeriano. - graph of the Lias Ammonites of the British Islands" (1878-86). - Riv. ital. Paleont. Strat., 59, 2, p. 65-90. Palaeontogr. Soc. (London). FEDERICI, P. R. (1968): Fossili sinemuriani della Liguria orientale. - - (1955): Revision des espe
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    Jurassic (170 - 199 Ma Time-Slice) Time

    Early Jurassic (170 - 199 Ma time-slice) Time ScaLe R Creator CHRONOS Cen Mesozoic Updated by James G. Ogg (Purdue University) and Gabi Ogg to: GEOLOGIC TIME SCALE 2004 (Gradstein, F.M., Ogg, J.G., Smith, A.G., et al., 2004) and The CONCISE GEOLOGIC TIME SCALE (Ogg, J.G., Ogg, G., and Gradstein, F.M., 2008) Paleozoic Sponsored, in part, by: Precambrian ICS Based, in part, on: CENOZOIC-MESOZOIC BIOCHRONOSTRATIGRAPHY: JAN HARDENBOL, JACQUES THIERRY, MARTIN B. FARLEY, THIERRY JACQUIN, PIERRE-CHARLES DE GRACIANSKY, AND PETER R. VAIL,1998. Mesozoic and Cenozoic Sequence Chronostratigraphic Framework of European Basins in: De Graciansky, P.- C., Hardenbol, J., Jacquin, Th., Vail, P. R., and Farley, M. B., eds.; Mesozoic and Cenozoic Sequence Stratigraphy of European Basins, SEPM Special Publication 60. Standard Geo- Ammonites Sequences Ammonites Sequences Smaller Benthic Foraminifers Larger Benthic Foraminifers Calcareous Nannofossils Dinoflagellate Cysts Radiolarians Belemnites Brachiopods Ostracodes Charophytes Stage Age Chronostratigraphy magnetic North Atlantic Tethys Age Polarity Sequences Boreal Sequences T-R Major T-R Period Epoch Stage Substage Boreal Boreal T-R Cycles Tethyan Global, Tethyan Cycles Cycles Zones Tethyan markers Zones Zonal Markers Zonal Markers Zones Boreal Zonal Markers Other Boreal Nannofossils Zones Zonal Markers Other Dinocysts Tethyan Dinocysts Zones Zonal Markers NW Europe Boreal Tethyan Boreal Ostracodes Tethyan Ostracodes Markers Lt. Bajoc. Strenoceras niortense Teloceras banksi Strenoceras niortense Teloceras banksi DSJ14 Lithodinia valensii Belemnopsis Lissajouthyris Lissajouthyris [un-named] 169.8 Stephanolithion speciosum Mancodinium semitabulatum, 169.8 L. galeata mg P., speciosum Durotrigia daveyi, Phallocysta apiciconus matisconensis matisconensis Glyptocythere scitula Teloc. blagdeni Bj3 Telo. blagdeni Bj3 NJ10 Andromeda depressa, G.
  • The Taxonomy and Systematics of Parapsicephalus Purdoni (Reptilia

    The Taxonomy and Systematics of Parapsicephalus Purdoni (Reptilia

    The taxonomy and systematics of Parapsicephalus purdoni (Reptilia: Pterosauria) from the Lower Jurassic Whitby Mudstone Formation, Whitby, U.K. Michael O’Sullivan1 and David M. Martill2 1,2School of Earth and Environmental Sciences, University of Portsmouth, Burnaby Building, Burnaby Road, United Kingdom, PO1 3QL *Corresponding author: [email protected] Keywords: Pterosauria, Parapsicephalus, United Kingdom, taxonomy, Lower Jurassic, Toarcian. Abstract The Lower Jurassic (Toarcian) pterosaur Parapsicephalus purdoni (Newton, 1888) from the Whitby Mudstone Formation of North Yorkshire is known from a three-dimensionally preserved skull with brain cast. Since Newton’s original description, its taxonomic status has been contentious. Several cladistic studies have placed it within either Dimorphodontidae or Rhamphorhynchidae. Some investigators have suggested that it is a junior synonym of the Toarcian pterosaur Dorygnathus from the Posidonia Shale of south-western Germany. The holotype skull (GSM 3166) is redescribed and its taxonomic status re-evaluated. Several apomorphies place it suggest it belongs in the Rhamphorhynchidae while autapomorphies of the palate and jugal distinguish Parapsicephalus from Dorygnathus, supporting the continued separation of the two genera. 1. Introduction The Lower Jurassic marine strata of the United Kingdom yield a diverse assemblage of reptilian taxa (Owen, 1881), including ichthyosaurs, plesiosaurs, marine crocodiles and, more rarely, pterosaurs. While Lower Jurassic pterosaurs are best known from the Liassic strata of Dorset (Buckland, 1829; Benton and Spencer, 1995), one of the best preserved examples is a three-dimensional near-complete skull (GSM 3166, figs. 1, 2) from the Toarcian (~182 ma) Whitby Mudstone Formation of Loftus, Yorkshire. Identified as the holotype of Parapsicephalus purdoni by Newton, 1888, it is deposited in the British Geological Survey (BGS) at Keyworth, Nottinghamshire.
  • Biostor-118662.Pdf

    Biostor-118662.Pdf

    /v^ GL''i£. The stratigraphy and ammonite fauna of the Upper Lias of Northamptonshire ,^^ UBRAR'' M. K. Howarth Department of Palaeontology, British Museum (Natural History), Cromwell Road, London SW7 5BD Contents Abstract 235 Introduction . 236 Acknowledgements 237 Stratigraphical succession 237 The Yorkshire coast 243 Zonal subdivisions and correlation with Yorkshire 244 Correlations with other areas .... 246 England ....... 246 Southern France, the Alps and Italy . 247 North-eastern Siberia, northern Alaska, arctic Canada, Greenland, Spitzbergen 249 Palaeontology ..... 249 Family Dactylioceratidae Hyatt 249 Genus Dactylioceras Hyatt 252 Subgenus Orthodactylites Buckman 253 Dactylioceras {Orthodactylites) semiannulatum sp. nov. 253 Genus Nodicoeloceras Buckman . 256 Nodicoeloceras crassoides (Young & Bird) 256 Genus Peronoceras Hyatt .... 259 Peronoceras fibulatiim (J. de C. Sowerby) 260 Peronoceras turriculatum (Simpson) 262 Peronoceras subarmatum (Young & Bird) 262 Peronoceras perarmatum (Young & Bird) 263 Genus Zugodactylites Buckman . 264 Zugodactylites braUnianus (d'Orbigny) 268 Zugodactylites rotundiventer Buckman . 273 Zugodactylites thompsoni sp. nov. 274 Zugodactylites pseudobraunianus (Monestier) 276 Genus Porpoceras Buckman 278 Porpoceras vortex (Simpson) 280 References ....... 281 Index ........ 284 Abstract The Upper Lias of Northamptonshire is redescribed from a now obscured exposure of the 3 m of lime- stones and clays, up to the Upper Cephalopod Bed, that could formerly be seen above the Marlstone Rock Bed in a quarry near Byfield, and from Beeby Thompson's descriptions and collections from the overlying 50 m of clays that were exposed in numerous 19th-century brickpits around Northampton. The three lowest subzones of the Upper Lias occur in the top 1 m of the Marlstone Rock Bed. This is overlain by the Transition Bed of Semicelatum Subzone age and the Abnormal Fish Bed of Exaratum Subzone age.
  • Biogeography Exercise Name ______

    Biogeography Exercise Name ______

    EART101: Biogeography exercise Name ______________________________ The Cordilleran belt of western North America is composed of a collage of exotic terranes, microcontinental blocks that originated as island arcs in the Pacific and later were accreted to the continental margin. You would like to know the location of these terranes in the past. The table below contains presence/absence data for Early Jurassic ammonite species from three accreted terranes (Wrangellia W, Stikinia S, and Quesnellia Q) and from the North American continent (Boreal Craton BC and Sonomia So). The Boreal Craton represents higher-latitude, cooler-water faunas and Sonomia contained lower-latitude, warmer-water faunas. W S Q BC So Amaltheus X X X X Pleuroceras X Pseudoamaltheus X Becheiceras X X Arieticeras X X X X Fontanelliceras X Fuciniceras X X X Leptaleoceras X X Lioceratoides X X X Protogrammoceras X X X X X Aveyroniceras X X X Prodactylioceras X X X Reynesoceras X X Cymbites X Fanninoceras X X X X Phylloceras X 1. Calculate Jaccard similarity coefficients between each of the accreted terranes (W, S, and Q), and between the terranes and the two stable continent regions BC and So. The Jaccard coefficient is M/(N1+N2-M), where M is the number of taxa shared between the two regions, N1 is the number of taxa in region 1, and N2 is the number of taxa in region 2. Fill in your answers in the table below. W S Q BC So W S Q BC So 2. For each terrane, determine its approximate paleolatitude in the Early Jurassic.