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Relevant bibliographies by topics / Kosmoceratidae

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Academic literature on the topic 'Kosmoceratidae'

Author: Grafiati

Published: 4 June 2021

Last updated: 4 February 2022

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Journal articles on the topic "Kosmoceratidae"

1

Mitta, Vasily V., and Aleksandr A. Mironenko. "Middle Jurassic (Upper Bathonian and Lower Callovian) jaws of Kosmoceratid ammonites of Central Russia." PalZ 95, no. 1 (2021): 61–69. http://dx.doi.org/10.1007/s12542-020-00533-8.

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2

Courville, Philippe, Alain Bonnot, Pierre-Yves Collin, Daniel Contini, and Didier Marchand. "Coupures morphologiques et biochronologie chez les Kosmoceratinae de l'Est de la France (Callovien inférieur pp. à Callovien supérieur pp.)." Comptes Rendus de l'Académie des Sciences - Series IIA - Earth and Planetary Science 327, no. 10 (1998): 685–91. http://dx.doi.org/10.1016/s1251-8050(99)80026-3.

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3

Kiselev, Dmitry N., and Mikhail A. Rogov. "Detailed biostratigraphy of the Middle Callovian – lowest Oxfordian in the Mikhaylov reference section (Ryazan region, European part of Russia) by ammonites." Volumina Jurassica XV, no. 1 (2018): 73–186. http://dx.doi.org/10.5604/01.3001.0012.7990.

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Study of the sections near the Mikhaylov (Ryazan region) has made it possible to improve the infrazonal subdivision of the Middle Callovian – Lower Oxfordian of the European Russia by ammonites. The Athleta Zone is the most complete in the studied sections. A sequence of kosmoceratid biohorizons (phaeinum, proniae, rowlstonense and kuklikum) is established here, as well as infrazonal units based on a phylogenetic sequence of species of the genus Funiferites. A study of the paleobiodiversity and frequency of occurrence of ammonites at different intervals of the section showed that the ammonite assemblages of the Athleta Zone are Sub-Boreal or Sub-Tethyan, while in the Lamberti Zone they are Boreal, and in the Lower Oxfordian they are Arctic. It is also shown that the change in ammonite composition in the sections coincides with the cycles of transgressions and regressions of Boreal basins. New species and subspecies of the ammonites Funiferites allae compressum, Cadoceras (Eichwaldiceras) intermedium, Brightia (B.) lominadzei, B. (B.) progzhellensis, B. (B.) eccentrtica, B. (Glyptia) canaliculata stankevitchae, Zieteniceras rarecostatum are described.

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4

Courville, Philippe. "Caractères ornementaux, disparité et diversité chez les Ammonitina : exemple des Kosmoceratinae (Stephanoceratoidea), Callovien moyen et supérieur (Jurassique moyen, Bassin parisien)." Comptes Rendus Palevol 10, no. 2-3 (2011): 155–70. http://dx.doi.org/10.1016/j.crpv.2010.11.005.

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5

Mitta, Vasily V., and Aleksandr A. Mironenko. "Middle Jurassic (Upper Bathonian and Lower Callovian) jaws of Kosmoceratid ammonites of Central Russia." PalZ, January 8, 2021. http://dx.doi.org/10.1007/s12542-020-00533-8.

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6

Alsen, Peter, Jussi Hovikoski, and Kristian Svennevig. "Middle Jurassic sandstone deposition in the Wandel Sea Basin: evidence from cardioceratid and kosmoceratid ammonites in the Mågensfjeld Formation in Kilen, North Greenland." GEUS Bulletin, December 21, 2020. http://dx.doi.org/10.34194/geusb.v44.5342.

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Age assessments from both palynostratigraphy and macrofossil biostratigraphy of the sandstone-dominated Mågensfjeld Formation, Wandel Sea Basin, North Greenland were hitherto hampered by post-burial thermal degradation of dinoflagellate cysts and a lack of well-preserved macrofossils. The formation was previously assigned to the Upper Cretaceous based on erroneous fossil identifications. Finds of cardioceratid and kosmoceratid ammonites during recent field work now provide the first age control of the unit, demonstrating it to be of late Bajocian – late Bathonian and perhaps Callovian (Middle Jurassic) age. This makes it among the oldest Jurassic units, perhaps even Mesozoic units, recorded in Kilen, North Greenland and eastern North Greenland. Previously, the complex structural and tectonic evolution of the area was poorly understood, and the structural relation of the Mågensfjeld Formation to the surrounding Mesozoic units was a puzzle. The new age assessment simplifies the structural situation in the area significantly. Further, the inference of a large reverse fault previously required to explain the proximity of the Mågensfjeld Formation to neighbouring Jurassic units is now unnecessary. The data show that the Wandel Sea Basin was influenced by the Middle Jurassic transgression and had sufficient accommodation space for marine deposition earlier than previously thought. The unit serves as a key datapoint and analogue for possible Middle Jurassic units in adjacent offshore basins.

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Books on the topic "Kosmoceratidae"

1

Lominadze, T. A. Kosmot͡s︡eratidy Kavkaza. "Met͡s︡niereba", 1985.

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