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. Stephanoceratidae is derived from the Otoitidae. Their fossils are found in upper Middle- and lower Upper Jurassic sediments.
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| - Stephanoceratidae (es)
- Stephanoceratidae (en)
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| - Stephanoceratidae es una familia de amonitas planuladas y coronadas dentro de Stephanoceratoidea. Las conchas son evolutas de modo que todos los verticilos están expuestos y tienen fuertes nervaduras que se bifurcan, es decir, se parten en dos, en los flancos. Muchos tienen tubérculos en el punto de bifurcación. Las secciones de verticilo son generalmente subequant; el borde exterior, o venter, comúnmente redondeado.Stephanoceratidae se deriva de Otoitidae. Sus fósiles se encuentran en sedimentos del Jurásico Superior Medio e Inferior. (es)
- 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. Stephanoceratidae is derived from the Otoitidae. Their fossils are found in upper Middle- and lower Upper Jurassic sediments. (en)
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| - Stephanoceras blagdeni from Mid Jurassic - Germany (en)
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| - Stephanoceratidae es una familia de amonitas planuladas y coronadas dentro de Stephanoceratoidea. Las conchas son evolutas de modo que todos los verticilos están expuestos y tienen fuertes nervaduras que se bifurcan, es decir, se parten en dos, en los flancos. Muchos tienen tubérculos en el punto de bifurcación. Las secciones de verticilo son generalmente subequant; el borde exterior, o venter, comúnmente redondeado.Stephanoceratidae se deriva de Otoitidae. Sus fósiles se encuentran en sedimentos del Jurásico Superior Medio e Inferior. (es)
- 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. Stephanoceratidae is derived from the Otoitidae. Their fossils are found in upper Middle- and lower Upper Jurassic sediments. (en)
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