Funiferites
Funiferites is genus of ammonite that lived during end of middle and in upper Callovian stage of middle Jurassic.[1]
| Funiferites Temporal range: [1] | |
|---|---|
Scientific classification  | |
| Domain: | Eukaryota |
| Kingdom: | Animalia |
| Phylum: | Mollusca |
| Class: | Cephalopoda |
| Subclass: | †Ammonoidea |
| Order: | †Ammonitida |
| Family: | †Cardioceratidae |
| Subfamily: | †Cadoceratinae |
| Genus: | †Funiferites Kiselev et al., 2003 |
| Type species | |
| Ammonites funiferus Phillips, 1829 | |
| Species | |
| |
Description
Ammonites of this genus had large shells. At the beginning of this evolutionary lineage, cross sectio. of shell was highly oval with rounded venter. Later, it has changed into subtriangular, or keeled. Ribs are curved sinusoidally and they are bending on the venter. During ontogeny, ribs are beginning to disappear from the sides. They are lasting the longest on the venter, mostly in the case of keeled specimens.[1]
Evolution
Genus Funiferites is a single evolutionary lineage. Its predecessor is Longaeviceras alpha. This gave rise to F. allae that evolved into F. patruus. Descendant of that one is F. funiferi.[2]
Validity
In 2002, few months before this genus has been erected, Ammonites funiferus, a type of Funiferites has been added into a new subgenus Chamousettia (Platychamousettia). Because of this, there is an opinion that Funiferites is only a junior synonym of subgenus Platychamousettia.[2] This opinion is opposed by another one (which one is debated even in a paper in which Funiferites has been described), that Platychamousettia is not a valid taxon and that there are identification and stratigraphic problems in its establishing and it is only a synonym of genus Chamousettia. This would mean, that Funiferites is a valid taxon.[1][3]
References
- Киселев Д.Н., Гуляев Д.Б., Рогов М.А. (2003) Происхождение и систематическое положение Funiferites – нового рода келловейских кардиоцератид (Ammonoidea)
- Mitta, V. V. "On the phylogeny of Early Cardioceratidae (Ammonoidea) and Cadoceratinae from Central Russia at the Bathonian–Callovian boundary." Paleontological Journal 50.4 (2016): 358-368.
- Gulyaev D.B. (2015) Stratigraphy of the Bathonian‐Callovian nearboundary deposits of European Russia // Jurassic System of Russia: Problems of stratigraphy and рaleogeography. Fifth All-Russian meeting. September 15–20, 2015, Makhachkala. Scientific materials. V.A. Zakharov (ch. ed.), M.A. Rogov, A.P. Ippolitov (eds.). Makhachkala: ALEF. P.94-101.
Literature
Kiselev D. N., Gulyaev D. B., Rogov M. A. (2003) Origin and systematic position of Funiferites, a new genus of the Callovian cardioceratid (Ammonoidea). In: N. A. Bogdanov, T. I. Vasil’eva, V. E. Verzbitsky et al. (Eds.). Modern questions of geology. Materials of the 3rd Lectures in Memory of Yanshine (March 26-28, 2003). Moscow: Nauchny mir. P. 220-225., 1 fig. [in Russian: Происхождение и систематическое положение Funiferites – нового рода келловейских кардиоцератид (Ammonoidea)].