Normannites

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Normannites
Temporal range: Bajocian [1]
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Stephanoceratidae - Normannites braikenridgei.JPG
Fossil specimen of Normannites braikenridgei from Mid Jurassic - Germany
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Normannites

Munier-Chalmas 1892

Normannites is a strongly ribbed evolute Middle Jurassic [1] genus of ammonite included in the stephanoceratoid family Stephanoceratidae.

Contents

Normanites was previously included in the Otoitidae by Arkell et al. 1957. More recent classifications show it to belong to the family Stephanoceratidae, along with genera like Stephanoceras and Stemmatoceras .

Description

Normannites has shells reaching a diameter of 52–55 millimetres (2.0–2.2 in). These shells have large lappets, curved plate-like structures that project forward on either side of the aperture. Primary ribs on the inner side of each whorl are large and close spaced, bifurcate about mid flank before continuing over the venter. Secondary ribs, when present, appear about mid flank between primary pairs.

Stephanoceras differs in its tendency to develop tubercles at the point of furcation in the primary ribs. Primary ribs, low on the whorls, in Stemmatoceras tend to be narrower and sharper.

Selected genera

Distribution

Jurassic of Saudi Arabia [2]

Related Research Articles

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Stephanoceratidae Extinct family of ammonites

Stephanoceratidae is a family of planulate and coronate ammonites within the Stephanoceratoidea. Shells are evolute so that all whorls are exposed and have strong ribbing that bifurcates, that is splits in two, on the flanks. Many have tubercles at the point of bifurcation. Whorl sections are generally subequant; the outer rim, or venter, commonly rounded.

<i>Macrocephalites</i> Genus of mollusc

Macrocephalites is a genus of the stephanoceratoid ammonite family Macrocephalitidae, diagnostic of the Callovian stage of the Middle Jurassic. Three subgenera, Dolikephalites, Kamptokephalites, and Pleurocephalites are recognized in addition to Macrocephalites itself, with Indocephalites tentatively included as the fourth.

Coeloceratidae is a family of ammonites belonging to the Eoderoceratoidea that lived during the Early Jurassic. Shells are evolute, tending to be broadly discoidal with depressed whorls bearing primary and secondary ribs that branch from outer lateral tubercles. Most of the included species have coronate inner whorls and outer tubercles only. In general, Coeloceratids resemble the Middle Jurassic Stephanoceras. Once regarded as the subfamily Coeloceratinae in the Eoderoceratidae, these ammonites are now given familial rank.

Pachyceratidae is a family of Perisphinctoidean ammonites from the upper Middle - and lower Upper Jurassic. Genera within the Pachyceratidae have shells that are in general moderately involte but with most of the inner whorls exposed; whorl sections subquadrate to subtrapezoidal, with rounded venter. Ribbing is strong, in some sharp. Primary ribs typically branch above mid flanks into twos, threes, and even fours.

Hecticoceras is an ammonite genus belonging to the haploceratoid family Oppeliidae, that lived during the Middle and Late Jurassic, from the Callovian. Hecticoceras may be seen as a series of some nine subgenera, beginning with the lower Callovian H. (Hecticoceras) and H. (Hecticoceratoides) and ending with the lower Oxfordian H. (Pseudobrightia) and H. (Eochetoceras). Hecticocerassensu lato and Prohecticoceras from the underlying Bathonian form the oppeliid subfamily, Hecticoceratinae.

Saxoceras is a genus of very evolute schlotheimiid ammonoids from the Lower Jurassic.

Ochetoceras is a genus of ammonites, belonging to the Oppeliidae, that lived during the Late Jurassic from the early Oxfordian to the early Tithonian, and type for the subfamily Ochetoceratinae.

References

  1. 1 2 Sepkoski, Jack (2002). "Sepkoski's Online Genus Database" . Retrieved 2014-05-28.
  2. "Paleobiology Database - Normannites" . Retrieved 17 December 2021.

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