Search results for "Ammoniti"

showing 10 items of 14 documents

A North American ammonite fauna from the late Middle Turonian of Vaucluse and Gard, southern France: the Romaniceras mexicanum, Prionocyclus hyatti a…

2016

Abstract An unusual, exotic, ammonite fauna including Romaniceras mexicanum Jones, 1938, Prionocyclus hyatti (Stanton, 1894) and Coilopoceras cf. springeri Hyatt, 1903 is recorded from the late Middle Turonian of Vaucluse and Gard, southern France. It is the first record of this ammonite association outside the Gulf Coast region and the Western Interior of the United States of North America. Up to present, these species were considered as endemic to the Western Interior sea-way. The migration of numerous ammonites from North America to western Europe during the late Middle Turonian suggests it is linked to a transgressive event or to a short sea-level high.

010506 paleontologyCoilopocerasFauna010502 geochemistry & geophysics01 natural sciencesCretaceousAmmonitidaPaleontologyAmmonitesMigration[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/Paleontology0105 earth and related environmental sciencesAmmonitebiologyTransgressive eventGeologyTuronianbiology.organism_classificationlanguage.human_languageCretaceousSouthern FranceWestern europeNorth AmericalanguageTransgressiveGeologyActa Geologica Polonica
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Problems in the identity of "Crioceras" barremense Kilian, 1895 (Ancyloceratida, Late Barremian), and their proposed resolution

2010

17 pages; The study of "Crioceras" barremense KILIAN was undertaken as a part of the revision of the Hemihoplitidae. This species was considered "classic" and has been used as the index of an Upper Barremian subzone; this usage raises a number of problems. The type specimen from Tyrol was a fragment described and illustrated by UHLIG as Crioceras sp. ind. aff. roemeri. This specimen could not be retrieved, and a topotype could not be collected. Our study revealed that there is both a biostratigraphic hiatus and important differences between conceptions of this species: (1) that ascribed UHLIG's type specimen (Upper Barremian, Tyrol), (2) KILIAN's concept of the specimen he found and named "…

010506 paleontologyStratigraphyHiatusAmmonitinae[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy010502 geochemistry & geophysics01 natural sciencesLower limitPaleontologylcsh:StratigraphyGenusmedicinelcsh:QE701-760Gassendiceras[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/Paleontology0105 earth and related environmental sciencesConfusionTaxonomylcsh:QE640-699Upper Barremianbiologylcsh:QE1-996.5PaleontologybiozonationGeologyAlpinum Subzonebiology.organism_classificationlcsh:GeologyBiohorizonlcsh:Paleontology[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyAlpinum Subzone / BiohorizonGassendiceratinae[SDU.STU.ST] Sciences of the Universe [physics]/Earth Sciences/StratigraphyType specimen[SDU.STU.PG] Sciences of the Universe [physics]/Earth Sciences/PaleontologyVandenheckei Biozonemedicine.symptomsoutheastern France[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyCarnets de Géologie
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Pseudoshasticrioceras bersaci nov. sp. (Ammonoidea, Gassendiceratinae), and new ammonite biohorizon for the Upper Barremian of southeastern France

2009

International audience; Research in the Feraudianus Subzone of the Sartousiana Zone of the Barremian stage led to the discovery of a new species of Pseudoshasticrioceras: P. bersaci nov. sp. Its study provides evidence concerning the developments of the latest Gassendiceratinae BERT et alii, 2006, and the relationship between the genus Pseudoshasticrioceras DELANOY, 1998, and Gassendiceras BERT et alii, 2006. In particular, this new species is derived from Pseudoshasticrioceras magnini (DELANOY, 1992) by a minor revision in the processes of ontogenesis (retardation of ornamentation - neoteny). However, the evolution towards Pseudoshasticrioceras autrani DELANOY, 1998, implies a "failure" in…

010506 paleontologyStratigraphyLineage (evolution)Ammonitinae[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy010502 geochemistry & geophysics01 natural sciencesPaleontologylcsh:StratigraphyGenusStage (stratigraphy)lcsh:QE701-760NeotenyGassendiceraslcsh:QE640-699[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/Paleontology0105 earth and related environmental sciencesAmmoniteUpper BarremianbiologyEcologylcsh:QE1-996.5PaleontologybiozonationGeologyAmmonoideabiology.organism_classificationlanguage.human_languagelcsh:GeologyPseudoshasticriocerasFeraudianus Subzonelcsh:Paleontology[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyGassendiceratinae[SDU.STU.ST] Sciences of the Universe [physics]/Earth Sciences/StratigraphylanguageSartousiana Zone[SDU.STU.PG] Sciences of the Universe [physics]/Earth Sciences/Paleontologysoutheastern France[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/Paleontology
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Les Gregoryceras (Ammonitina) de l'Oxfordien moyen terminal et supérieur téthysien : révision systématique, biostratigraphie et évolution.

2009

43 pages; Les Gregoryceras Spath, 1924 (Ammonitina, Peltoceratina) de la fin de l'Oxfordien moyen (sous-zone à Rotoides) et de la base de l'Oxfordien supérieur (zone à Bifurcatus) sont révisés. Les coupes ayant fourni la plupart des spécimens de ce travail (Espagne et Maghreb) sont décrites et datées sur la base de comparaisons fauniques entre les domaines téthysien et subtéthysien. Le meilleur outil pour ces corrélations est la présence du genre Gregoryceras. La succession des espèces de Gregoryceras est identique pour les deux domaines suscités, ce qui permet de compléter l'échelle biostratigraphique proposée antérieurement et parallèle à la zonation standard. Les espèces reconnues et red…

010506 paleontologybiologyAmmonitinaPaleontologyÉvolutionEcological succession[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy010502 geochemistry & geophysicsbiology.organism_classification01 natural sciencesSpecies successionPaleontologyGeographyCorrélations biostratigraphiquesSpace and Planetary ScienceGregoryceras (Ammonitina)Taxinomie[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyDimorphismeOxfordien[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/Paleontology[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/Paleontology0105 earth and related environmental sciences
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The Use of Landmarks to Describe Ammonite Shap

1999

The use of landmarks and geometrical morphometric techniques is illustrated with examples from the Harpoceratinae (Ammonitina). This approach is useful in analysing morphological variations of characters such as rib pattern or ventral shape on the scale of the genus or species. It can be used to map forms so that similarities and dissimilarities between organisms can be read and quantified directly.

AmmonitePaleontologybiologyScale (ratio)GenusAmmonitinalanguagebiology.organism_classificationlanguage.human_languageGeology
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Existe-t-il une crise au passage Lias-Dogger chez les ammonites? Approche morphometrique par quantification de la disparite morphologique

2001

Abstract Morphological changes observed in ammonites at the Lias-Dogger (Toarcian-Aalenian) boundary are analyzed here. The study covers all known ammonites worldwide over some 2 m.y. (the last two biozones of the Toarcian: Pseudoradiosa and Aalensis and the first biozone of the Aalenian: Opalinum). Ammonite taxonomy at this boundary is still open to question, the main disagreements being over groupings at family or super-family level. The evolutionary schema developed by Tintant and Mouterde [1981] shows two main sets of Ammonitina for the time: (1) the dominant Hammatocerataceae (Graphoceratidae+Hammatoceratidae) and (2) the final representatives of the Hildocerataceae. Two conservative a…

AmmonitebiologyAmmonitinaPhylloceratinaGeologyAmmonoideaBiozonebiology.organism_classificationlanguage.human_languagePaleontologylanguagePhragmoconeLytoceratinaHeterochronyGeologyBulletin de la Société Géologique de France
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World distribution of middle Jurassic ammonites (Upper Aalenian to Middle Bathonian): relationships between biodiversity and palaeogeography

2004

Abstract The break up of the Pangea takes place in the Jurassic; the palaeoceanographic consequences are the opening of seaways, particularly at the place of the future Atlantic and Indian oceanic areas. During the Toarcian, and from the late Aalenian to the middle Bathonian, the so-called “Hispanic corridor” (or “Atlantic seaway”) exists between the “western Tethys” and the “American Pacific border”, through the “Caribbean Tethys”. Two additional seaways which play as by-passes of the Pangea are proposed, one along the northern border of Laurasia (Boreal sea), and a second along the southern border of Gondwana (South Pacific Sea); however, if these two last could be effectively used for fa…

AmmonitebiologyRange (biology)AmmonitinaGeologyBiozoneDiachronousbiology.organism_classificationlanguage.human_languagePaleontologyGondwanaLaurasialanguageEndemismGeologyBulletin de la Société Géologique de France
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Studio delle associazioni ad ammoniti dell'Oxfordiano della Sicilia occidentale

2004

Ammoniti Oxfordiano Giurassico Stratigrafia SiciliaSettore GEO/02 - Geologia Stratigrafica E Sedimentologica
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Sistematica, tafonomia e paleobiogeografia delle associazioni ad ammoniti del Giurassico Medio e Superiore della Sicilia Occidentale con particolare …

2012

AmmonitiSettore GEO/02 - Geologia Stratigrafica E SedimentologicaPaleobiogeografiaGiurassicoSiciliaSettore GEO/01 - Paleontologia E Paleoecologia
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Leptechioceras (Neomicroceras) Donovan, 1966 (Ammonitina, Echioceratidae, Sinémurien, Europe du Nord-Ouest): Taxon progénétique ou microconque?

1992

Resume Des faunes d'ammonites inedites collectees banc par banc dans des series epaisses a dominante argileuse duSinemurien terminal du Bassin parisien (Cher, France) sont decrites. Certains des peuplements etudies sont esentiellement constitues d'ammonites de petite taille attribuees au sous-genre Leptechioceras (Neomicroceras) ; le rattachement de ces formes aux Echioceratidae, alors qu'elles etaient initialement interpretees comme des Eoderoceratidae, est base sur des arguments cladistiques et est confirme par les observations stratigraphiques. Une nouvelle espece, la plus tardive du sous-genre, Leptechioceras (Neomicroceras) sparsicosta est decrite. L'originalite en termes d'heterochron…

GeographybiologySpace and Planetary ScienceWestern europeAmmonitinaPaleontologyMesozoicbiology.organism_classificationHumanitiesGeobios
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