Turonian ammonite faunas from the southern Corbières, Aude, France

Kennedy, W. J.; Bilotte, M.; Melchior, P.

doi:10.1515/agp-2015-0020

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Tytuł artykułu

Turonian ammonite faunas from the southern Corbières, Aude, France

Autorzy

Kennedy W. J. , Bilotte M. , Melchior P.

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Identyfikatory

DOI

10.1515/agp-2015-0020

Warianty tytułu

Języki publikacji

Abstrakty

The Turonian successions of the southern Corbières comprise three transgressive-regressive cycles in which ammonites occur in three intervals. The lowest comes from the glauconitic basal transgressive unit of the first cycle, and comprises 21 species, including Kamerunoceras douvillei (Pervinquière, 1907), Kamerunoceras turoniense (d’Orbigny, 1850), Spathites (Jeanrogericeras) revelerianus (Courtiller, 1860), Spathites (Jeanrogericeras) combesi (d’Orbigny, 1856), Mammites nodosoides (Schlüter, 1871), Mammites powelli Kennedy, Wright and Hancock, 1987, Fagesia tevestensis (Péron, 1896), Neoptychites cephalotus (Coutiller, 1860), Thomasites rollandi (Thomas and Péron, 1889), Wrightoceras wallsi Reyment, 1954, and Choffaticeras (Choffaticeras) quaasi (Péron, 1904). This is a Lower Turonian assemblage referred to the Mammites nodosoides Zone, although the possibility that elements from the preceding Fagesia catinus Zone are also present cannot be excluded. The fauna from the transgressive glauconitic interval of the succeeding cycle comprises nine species, including Romaniceras (Romaniceras) mexicanum Jones, 1938, Romaniceras (Yubariceras) ornatissimum (Stoliczka, 1864), Pseudotissotia galliennei (d’Orbigny, 1850), Collignoniceras woollgari (Mantell, 1822) sensu lato, Coilopoceras springeri Hyatt, 1903, and Eubostrychoceras (Eubostrychoceras) saxonicum (Schlüter, 1872). They indicate the Middle Turonian Romaniceras (R.) mexicanum and R. (Y.) ornatissimum zones. The highest fauna, from the Marnes supérieurs de Saint-Louis of the Saint-Louis syncline, is: Subprionocyclus sp. juv., Prionocyclus sp. and Worthoceras cf. rochatianum (d’Orbigny, 1850). The Subprionocyclus are minute individuals that resemble S. bravaisianus (d’Orbigny, 1841), and suggest the presence of the lower Upper Turonian bravaisianus Zone.

Słowa kluczowe

ammonites biostratigraphy Turonian Cretaceous France

amonity biostratygrafia turon kreda Francja

Wydawca

Faculty of Geology of the University of Warsaw
Komitet Nauk Geologicznych PAN

Czasopismo

Acta Geologica Polonica

Rocznik

2015

Tom

Vol. 65, no. 4

Strony

437--494

Opis fizyczny

Bibliogr. 188 poz., rys., tab.

Twórcy

autor

Kennedy W. J.

Oxford University Museum of Natural History, Parks Road, Oxford OX1 3PW, and Department of Earth Sciences, South Parks Road, Oxford OX1 3AN, United Kingdom

autor

Bilotte M.

Géosciences Environnement Toulouse, Faculté des Sciences et Ingénierie de Toulouse, 14 avenue Edouard Belin, 31400 Toulouse and Service Commun d’Etudes et de Conservation des Collections Patrimoniales, 118 route de Narbonne, 31062 Toulouse cedex 4, France

autor

Melchior P.

9, Boulevard Challier de Néré, 13008 Marseille, France

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