| 词条 | Reynesocoeloceratinae |
| 释义 |
|fossil_range = {{fossil range|Pliensbachian}}[1] | image = Prodactylioceras davoei - Naturhistorisches Museum, Braunschweig, Germany - DSC05104.JPG | image_caption = Prodactylioceras cf. davoei | taxon = Reynesocoeloceratinae | authority = Dommergues, 1986 | subdivision_ranks = Genera | subdivision = | synonyms = }} The subfamily Reynesocoeloceratinae comprises early Jurassic ammonite genera that lived during Pliensbachian stage. These dactylioceratids existed from Ibex ammonite zone and died out in Spinatum zone. They have evolved from Metaderoceras and gave rise to subfamily Dactylioceratinae.[1] DescriptionAmmonites with depressed, cadicone, or even evolute, serpenticone shells. Tubercules might be present. Ribs can be both single, or bifurcating. Some members of this subfamily show size dimorphism. They differs from Dactylioceratinae by suture. While Reynesocoeloceratinae has on dorsal side of external lobe two major secondary lobes, this is not so in Dactylioceratinae, as there is external saddle not divided, while lateral lobe is strongly trifid.[1] Taxonomy[1]
References1. ^1 2 3 M. K. Howarth 2013. Treatise on Invertebrate Paleontology, Part L, Revised, Volume 3B, Chapter 4: Psiloceratoidea, Eoderoceratoidea, Hildoceratoidea. {{Taxonbar|from=Q23833121}}{{ammonitina-stub}} 4 : Dactylioceratidae|Pliensbachian life|Pliensbachian first appearances|Pliensbachian extinctions |
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