Jurassic Ammonite Aptychi: Functions and Evolutionary Implications
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The Middle Jurassic of Western and Northern Europe: Its Subdivisions, Geochronology and Correlations
The Middle Jurassic of western and northern Europe: its subdivisions, geochronology and correlations John H. Callomon The palaeogeographic settings of Denmark and East Greenland during the Middle Jurassic are outlined. They lay in the widespread epicontinental seas that covered much of Europe in the post-Triassic transgression. It was a period of continuing eustatic sea-level rise, with only distant connections to world oceans: to the Pacific, via the narrow Viking Straits between Greenland and Norway and hence the arctic Boreal Sea to the north; and to the subtropical Tethys, via some 1200 km of shelf-seas to the south. The sedimentary history of the region was strongly influenced by two factors: tectonism and climate. Two modes of tectonic movement governed basinal evolution: crustal extension lead- ing to subsidence through rifting, such as in the Viking and Central Grabens of the North Sea; and subcrustal thermal upwelling, leading to domal uplift and the partition of marine basins through emergent physical barriers, as exemplified by the Central North Sea Dome with its associated volcanics. The climatic gradient across the 30º of temperate latitude spanned by the European seas governed biotic diversity and biogeography, finding expression in rock-forming biogenic carbonates that dominate sediments in the south and give way to largely siliciclastic sediments in the north. Geochronology of unrivalled finesse is provided by standard chronostratigraphy based on the biostratigraphy of ammonites. The Middle Jurassic saw the onset of considerable bioprovincial endemisms in these guide-fossils, making it necessary to construct parallel standard zonations for Boreal, Subboreal or NW European and Submediterranean Provinces, of which the NW European zonation provides the primary international standard. -
New and Poorly Known Perisphinctoidea (Ammonitina) from the Upper Tithonian of Le Chouet (Drôme, SE France)
Volumina Jurassica, 2014, Xii (1): 113–128 New and poorly known Perisphinctoidea (Ammonitina) from the Upper Tithonian of Le Chouet (Drôme, SE France) Luc G. BULOT1, Camille FRAU2, William A.P. WIMBLEDON3 Key words: Ammonoidea, Ataxioceratidae, Himalayitidae, Neocomitidae, Upper Tithonian, Le Chouet, South-East France. Abstract. The aim of this paper is to document the ammonite fauna of the upper part of the Late Tithonian collected at the key section of Le Chouet (Drôme, SE France). Emphasis is laid on new and poorly known Ataxioceratidae, Himalayitidae and Neocomitidae from the upper part of the Tithonian. Among the Ataxioceratidae, a new account on the taxonomy and relationship between Paraulacosphinctes Schindewolf and Moravisphinctes Tavera is presented. Regarding the Himalayitidae, the range and content of Micracanthoceras Spath is discussed and two new genera are introduced: Ardesciella gen. nov., for a group of Mediterranean ammonites that is homoeomorphic with the Andean genus Corongoceras Spath, and Pratumidiscus gen. nov. for a specimen that shows morphological similarities with the Boreal genera Riasanites Spath and Riasanella Mitta. Finally, the occurrence of Neocomitidae in the uppermost Tithonian is documented by the presence of the reputedly Berriasian genera Busnardoiceras Tavera and Pseudargentiniceras Spath. INTRODUCTION known Perisphinctoidea from the Upper Tithonian of this reference section. Additional data on the Himalayitidae in- The unique character of the ammonite fauna of Le Chouet cluding the description and discussion of Boughdiriella (near Les Près, Drôme, France) (Fig. 1) has already been chouetensis gen. nov. sp. nov. are to be published elsewhere outlined by Le Hégarat (1973), but, so far, only a handful of (Frau et al., 2014). -
Back Matter (PDF)
GENERAL INDEX TO THE QUARTERLY JOURNAL AND PROCEEDINGS OF THE GEOLOGIC&L SOCIETY. AC~.AND,. H. D., on Vole. Series nr. Agglomerate, vole., of Lambay I., Herefordshire Beacon, 556-562 w. 141. maps & sect. Airolo (St: Gothard), Tremola Schists Aclisina, observats, on genus, 45"72 nr., 358, 359. & pls. iii-v. Aldeburgh (Suffolk), struct, of Cor. aciculata, sp. nov., 59 & pl. iv. Crag fr. Ramsholt to, 327, 329 fig. ; .... attenuata, sp. nov., 58 & pl. iv. Crag at, 338, 339. -- costatula, 56 & pl. iii ; car. dubia Alderbury Hill (Wilts), flint from, nov., 57 & pl. iii. exhib., cvi ; plateau-gravel at, 297. elegan~ula, sp. nov., 62 & pl. iv. Aldworth (Oxon), Quartzite-gravel nr., elongata, 54 & pl. iii ; vat. cingu- 591. lata nov., 55 & pl. iii; vat. varians Alexandra Land (Franz Josef Land), nov., 55 & pl. iii. geol. feats, of, 631. -- grantoneusis, sp. nov., 60 & pl. iv. hlgous (?) borings, infilled w. silicate ---parwda, sp. nov., 64 & pl. v. of iron, 322-323 fig. -- pulchra, vat. tenuis, 52 & pl. iii ; ALLrORV, S., obituary of, Ix. car. iutermedia nov., 53 & pl. iii. Almannagja (Iceland) basalt, chem. pusilla, sp. nov., 63 & pl. iv. anal. of, 647. quadrata, sp. nov., 61 & pl. iv; Amaltheidm, short period of domin- car. striatissima nov., 62. ance, 448 ; list of genera, 459. similis, sp. nov., 57 & pls. iii-iv. Amlweh (Anglesey), metamorph, grits -- (~.) sulcatula, 64 & pLv. & shales S.W. of, 374-381 figs. ~enuisgriata, sp. nov., 60 & pl. iv. Ammonite-families, & their conn. w. -- terebra, sp. nov., 63 & pl. iv, ' Jurassic' time-divs., 443-444 ; Aclisoides, section of Murchisonia, 66. -
A Revision of the Classification of the Plesiosauria with a Synopsis of the Stratigraphical and Geographical Distribution Of
LUNDS UNIVERSITETS ARSSKRIFT. N. F. Avd. 2. Bd 59. Nr l. KUNGL. FYSIOGRAFISKA SÅLLSKAPETS HANDLINGAR, N. F. Bd 74. Nr 1. A REVISION OF THE CLASSIFICATION OF THE PLESIOSAURIA WITH A SYNOPSIS OF THE STRATIGRAPHICAL AND GEOGRAPHICAL DISTRIBUTION OF THE GROUP BY PER OVE PERSSON LUND C. W. K. GLEER UP Read before the Royal Physiographic Society, February 13, 1963. LUND HÅKAN OHLSSONS BOKTRYCKERI l 9 6 3 l. Introduction The sub-order Plesiosauria is one of the best known of the Mesozoic Reptile groups, but, as emphasized by KuHN (1961, p. 75) and other authors, its classification is still not satisfactory, and needs a thorough revision. The present paper is an attempt at such a revision, and includes also a tabular synopsis of the stratigraphical and geo graphical distribution of the group. Some of the species are discussed in the text (pp. 17-22). The synopsis is completed with seven maps (figs. 2-8, pp. 10-16), a selective synonym list (pp. 41-42), and a list of rejected species (pp. 42-43). Some forms which have been erroneously referred to the Plesiosauria are also briefly mentioned ("Non-Plesiosaurians", p. 43). - The numerals in braekets after the generic and specific names in the text refer to the tabular synopsis, in which the different forms are numbered in successional order. The author has exaroined all material available from Sweden, Australia and Spitzbergen (PERSSON 1954, 1959, 1960, 1962, 1962a); the major part of the material from the British Isles, France, Belgium and Luxembourg; some of the German spec imens; certain specimens from New Zealand, now in the British Museum (see LYDEK KER 1889, pp. -
New Data on the Jaw Apparatus of Fossil Cephalopods
New dataon the jaw apparatus of fossil cephalopods YURI D. ZAKHAROV AND TAMAZ A. LOMINADZE \ Zakharov, Yuri D. & Lominadze, Tamaz A. 19830115: New data on the jaw apparatus of fossil LETHAIA cephalopods. Lethaia, Vol. 16, pp. 67-78. Oslo. ISSN 0024-1164. A newly discovered fossil cephalopod jaw apparatus that may belong to Permian representatives of the Endocochlia is described. Permorhynchus dentatus n. gen. n. sp. is established on the basis of this ~ apparatus. The asymmetry of jaws in the Ectocochlia may be connected with the double function of the ventral jaw apparatus, and the well-developed, relatively large frontal plate of the ventral jaw should be regarded as a feature common to all representatives of ectocochlian cephalopods evolved from early Palaeozoic stock. Distinct features seen in the jaw apparatus of Upper Pcrmian cndocochlians include the pronounced beak form of both jaws and the presence of oblong wings on the ventral mandible. o Cephalopoda. jaw. operculum. aptychus, anaptychus, Permorhynchus n.gen.• evolution. Permian. Yuri D. Zakharov llOpllll Ilscumpueeu« Gaxapoe], Institute of Biology and Pedology, Far-Eastern Scientific Centre. USSR Academy of Science, Vladivostok 690022, USSR (EUOJl020-n9~BnlHbliiuucmu my m Ilaot.neeocmo-cnoro Ha."~H020 uenmpav Axaoeuuu 'HayK CCCP, Bnaoueocmo« 690022, CCCP); Tamaz A. Lominadze ITa.'W3 Apl.j1L10BUl.j Jlouunaoee), Institute of Palaeobiology of Georgian SSR Academy of Science. Tbilisi 380004. USSR (Hncmumvm naJle06UOJl02UU Atcaoeuuu naytc TpY3UHUjKOii CCP. T6'LJUCU 380004. CCP; 19th August. 1980 (revised 1982 06 28). The jaw apparatus of Recent cephalopods is re Turek 1978, Fig. 7, but not the reconstruction in presented by two jaw elements (Fig. -
A Review of the Classification of Jurassic Aspidoceratid Ammonites – the Superfamily Aspidoceratoidea
VOLUMINA JURASSICA, 2020, XVIII (1): 47–52 DOI: 10.7306/VJ.18.4 A review of the classification of Jurassic aspidoceratid ammonites – the Superfamily Aspidoceratoidea Horacio PARENT1, Günter SCHWEIGERT2, Armin SCHERZINGER3 Key words: Superfamily Aspidoceratoidea, Aspidoceratidae, Epipeltoceratinae emended, Peltoceratidae, Gregoryceratinae nov. subfam. Abstract. The aspidoceratid ammonites have been traditionally included in the superfamily Perisphinctoidea. However, the basis of this is unclear for they bear unique combinations of characters unknown in typical perisphinctoids: (1) the distinct laevaptychus, (2) stout shells with high growth rate of the whorl section area, (3) prominent ornamentation with tubercles, spines and strong growth lines running in parallel over strong ribs, (4) lack of constrictions, (5) short to very short bodychamber, and (6) sexual dimorphism characterized by minia- turized microconchs and small-sized macroconchs besides the larger ones, including changes of sex during ontogeny in many cases. Considering the uniqueness of these characters we propose herein to raise the family Aspidoceratidae to the rank of a superfamily Aspi- doceratoidea, ranging from the earliest Late Callovian to the Early Berriasian Jacobi Zone. The new superfamily includes two families, Aspidoceratidae (Aspidoceratinae, Euaspidoceratinae, Epipeltoceratinae and Hybonoticeratinae), and Peltoceratidae (Peltoceratinae and Gregoryceratinae nov. subfam.). The highly differentiated features of the aspidoceratoids indicate that their life-histories -
First Record of Non-Mineralized Cephalopod Jaws and Arm Hooks
Klug et al. Swiss J Palaeontol (2020) 139:9 https://doi.org/10.1186/s13358-020-00210-y Swiss Journal of Palaeontology RESEARCH ARTICLE Open Access First record of non-mineralized cephalopod jaws and arm hooks from the latest Cretaceous of Eurytania, Greece Christian Klug1* , Donald Davesne2,3, Dirk Fuchs4 and Thodoris Argyriou5 Abstract Due to the lower fossilization potential of chitin, non-mineralized cephalopod jaws and arm hooks are much more rarely preserved as fossils than the calcitic lower jaws of ammonites or the calcitized jaw apparatuses of nautilids. Here, we report such non-mineralized fossil jaws and arm hooks from pelagic marly limestones of continental Greece. Two of the specimens lie on the same slab and are assigned to the Ammonitina; they represent upper jaws of the aptychus type, which is corroborated by fnds of aptychi. Additionally, one intermediate type and one anaptychus type are documented here. The morphology of all ammonite jaws suggest a desmoceratoid afnity. The other jaws are identifed as coleoid jaws. They share the overall U-shape and proportions of the outer and inner lamellae with Jurassic lower jaws of Trachyteuthis (Teudopseina). We also document the frst belemnoid arm hooks from the Tethyan Maastrichtian. The fossils described here document the presence of a typical Mesozoic cephalopod assemblage until the end of the Cretaceous in the eastern Tethys. Keywords: Cephalopoda, Ammonoidea, Desmoceratoidea, Coleoidea, Maastrichtian, Taphonomy Introduction as jaws, arm hooks, and radulae are occasionally found Fossil cephalopods are mainly known from preserved (Matern 1931; Mapes 1987; Fuchs 2006a; Landman et al. mineralized parts such as aragonitic phragmocones 2010; Kruta et al. -
'Cenoceras Islands' in the Blue Lias Formation (Lower Jurassic)
FOSSIL IMPRINT • vol. 75 • 2019 • no. 1 • pp. 108–119 (formerly ACTA MUSEI NATIONALIS PRAGAE, Series B – Historia Naturalis) ‘CENOCERAS ISLANDS’ IN THE BLUE LIAS FORMATION (LOWER JURASSIC) OF WEST SOMERSET, UK: NAUTILID DOMINANCE AND INFLUENCE ON BENTHIC FAUNAS DAVID H. EVANS1, *, ANDY H. KING2 1 Stratigrapher, Natural England, Rivers House, East Quay, Bridgwater, Somerset, TA6 4YS UK; e-mail: [email protected]. 2 Director & Principal Geologist, Geckoella Ltd, Suite 323, 7 Bridge Street, Taunton, Somerset, TA1 1TG UK; e-mail: [email protected]. * corresponding author Evans, D. H., King, A. H. (2019): ‘Cenoceras islands’ in the Blue Lias Formation (Lower Jurassic) of West Somerset, UK: nautilid dominance and influence on benthic faunas. – Fossil Imprint, 75(1): 108–119, Praha. ISSN 2533-4050 (print), ISSN 2533-4069 (on-line). Abstract: Substantial numbers of the nautilid Cenoceras occur in a stratigraphically limited horizon within the upper part of the Lower Jurassic (Sinemurian Stage) Blue Lias Formation at Watchet on the West Somerset Coast (United Kingdom). Individual nautilid conchs are associated with clusters of encrusting organisms (sclerobionts) forming ‘islands’ that may have been raised slightly above the surrounding substrate. Despite the relatively large numbers of nautilid conchs involved, detailed investigation of their preservation suggests that their accumulation reflects a reduction in sedimentation rates rather than an influx of empty conches or moribund animals. Throughout those horizons in which nautilids are present in relative abundance, the remains of ammonites are subordinate or rare. The reason for this unclear, and preferential dissolution of ammonite conchs during their burial does seem to provide a satisfactory solution to the problem. -
Revisión De Los Ammonoideos Del Lías Español Depositados En El Museo Geominero (ITGE, Madrid)
Boletín Geológico y Minero. Vol. 107-2 Año 1996 (103-124) El Instituto Tecnológico Geominero de España hace presente que las opiniones y hechos con signados en sus publicaciones son de la exclusi GEOLOGIA va responsabilidad de los autores de los trabajos. Revisión de los Ammonoideos del Lías español depositados en el Museo Geominero (ITGE, Madrid). Por J. BERNAD (*) y G. MARTINEZ. (**) RESUMEN Se revisan desde el punto de vista taxonómico, los fósiles de ammonoideos correspondientes al Lías español que se encuentran depositados en el Museo Geominero. La colección está compuesta por ejemplares procedentes de 67 localida des españolas, pertenecientes a colecciones de diferentes autores. Se identifican los ordenes Phylloceratina, Lytoceratina y Ammonitina, las familias Phylloceratidae, Echioceratidae, eoderoceratidae, Liparoceratidae, Amaltheidae, Dactyliocerati Los derechos de propiedad de los trabajos dae, Hildoceratidae y Hammatoceratidae y las subfamilias Xipheroceratinae, Arieticeratinae, Harpoceratinae, Hildocerati publicados en esta obra fueron cedidos por nae, Grammoceratinae, Phymatoceratinae y Hammatoceratinae correspondientes a los pisos Sinemuriense, Pliensbachien los autores al Instituto Tecnológico Geomi se y Toarciense. nero de España Oueda hecho el depósito que marca la ley. Palabras clave: Ammonoidea, Taxonomía, Lías, España, Museo Geominero. ABSTRACT The Spanish Liassic ammonoidea fossil collections of the Geominero Museum is revised under a taxonomic point of view. The collection includes specimens from 67 Spanish -
Abhandlungen Der Geologischen Bundesanstalt in Wien
ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Abhandlungen der Geologischen Bundesanstalt in Wien Jahr/Year: 2002 Band/Volume: 57 Autor(en)/Author(s): Sprey Anton Martin Artikel/Article: Early Ontogeny of three Callovian Ammonite Genera (Binatisphinctes, Kosmoceras (Spinikosmoceras) and Hecticoceras) from Ryazan (Russia) 225-255 ©Geol. Bundesanstalt, Wien; download unter www.geologie.ac.at ABHANDLUNGEN DER GEOLOGISCHEN BUNDESANSTALT Abh. Geol. B.-A. ISSN 0016–7800 ISBN 3-85316-14-X Band 57 S. 225–255 Wien, Februar 2002 Cephalopods – Present and Past Editors: H. Summesberger, K. Histon & A. Daurer Early Ontogeny of three Callovian Ammonite Genera (Binatisphinctes, Kosmoceras (Spinikosmoceras) and Hecticoceras) from Ryazan (Russia) ANTON MARTIN SPREY*) 15 Text-Figures, 3 Tables and 8 Plates Callovian Ammonoidea Shell Structure Early Ontogeny Micro-ornament Contents Zusammenfassung ...................................................................................................... 225 Abstract ................................................................................................................. 226 1. Introduction ............................................................................................................. 226 2. Material and Methods .................................................................................................... 226 2.1. Examined Taxa and Their Source ................................................................................... -
GEOS 33000/EVOL 33000: Winter 2006 Course Outline Page 1
GEOS 33000/EVOL 33000: Winter 2006 Course Outline Page 1 Meetings: Tuesdays and Thursdays, 10:30-12:00, HGS 180 Nature of the course: This course is an introduction to mathematical modeling as applied to problems in paleobiology and evolutionary biology. Topics include: basic probability theory; general approaches to modeling; model comparison using likelihood and other criteria; forward modeling of branching processes; sampling models; and inverse methods. A series of programming exercises and a term project are required. Programming in R or C is recommended, but any language may be used. Requirements: 1. Short exercises 2. Readings to be assigned 3. Term paper: Original research, relevant to topics covered in course. Publication length and quality. Brief presentation of research. Prerequisites: Mathematics through first-year calculus; basic computer programming skills (or willingness to learn) URL for course materials: http://geosci.uchicago.edu/∼foote/MODEL Reading General Reference Works Burnham, K.P., and D. R. Anderson. 1998. Model selection and inference: a practical information-theoretic approach. Springer, New York. Edwards, A.W.F. 1992. Likelihood. Johns Hopkins U. Press. Efron, B. and R.J. Tibshirani. 1993. An introduction to the bootstrap. Chapman and Hall, N.Y. Feller, W. 1968 (and other editions). An introduction to probability theory and its applications (two volumes). John Wiley and Sons, N.Y. Gilinsky, N.L., and P.W. Signor, eds. 1991. Analytical paleobiology. Short Courses in Paleontology Number 4. Paleontological Society, Knoxville, Tenn. Gumbel, E.J. 1958. Statistics of extremes. Columbia University Press, N.Y. Press, W.H., S.A. Teukolsky, W.T. Vetterling, B.P. -
Paléontologie Au Luxembourg (2) A
Paléontologie au Luxembourg (2) A. Di Cencio, D. Sadki, R. Weis (eds.) R. Weis D. Sadki, A. Di Cencio, Les ammonites de la Minette Andrea Di Cencio, Driss Sadki, Paléontologie au Luxembourg (2) Luxembourg au Paléontologie Robert Weis (eds.) Ferrantia Travaux scientifiques du Musée national d'histoire naturelle Luxembourg www.mnhn.lu 83 2020 Ferrantia 83 2020 2020 83 Ferrantia est une revue publiée à intervalles non réguliers par le Musée national d’histoire naturelle à Luxembourg. Elle fait suite, avec la même tomaison, aux T M ’ L parus entre 1981 et 1999. Comité de rédaction: Eric Buttini Guy Colling Alain Frantz Thierry Helminger Ben Thuy Mise en page: Romain Bei Design: Thierry Helminger Prix du volume: 20 € Rédaction: Échange: Musée national d’histoire naturelle Exchange MnhnL Rédaction Ferrantia c/o Musée national d’histoire naturelle 25, rue Münster 25, rue Münster L-2160 Luxembourg L-2160 Luxembourg Tél +352 46 22 33 - 1 Tél +352 46 22 33 - 1 Fax +352 46 38 48 Fax +352 46 38 48 Internet: http://www.mnhn.lu/ferrantia/ Internet: http://www.mnhnl.lu/biblio/exchange email: [email protected] email: [email protected] Page de couverture: Bredyia subinsignis (Oppel, 1856), DOU833. Natural History Museum of Luxembourg. Citation: Di Cencio A., Sadki D., Weis R. (eds.) 2020. - Paléontologie au Luxembourg (2) - Les ammonites de la Minette. Ferrantia 83, Musée national d’histoire naturelle, Luxembourg, 129 p. Date de publication: 15 décembre 2020 (réception du manuscrit: 19 mai 2020) Impression: Imprimerie Centrale climatiquement neutre Impression | LU-319-JR8FDJV | www.natureOffice.com Ferrantia est publiée sous la licence Creative Commons BY-NC-ND 3.0 LU.