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Schloenbachiidae
Shloenbachiidae is a family of hoplitoid ammonoid cephalopds mostly from the lower Upper Cretaceous, (U Albian - Cenomanian). Shloenbachiidae can be recognized by their usually keel bearing, irregularly ribbed and tuberculate shells that vary from evolute to rather involute and compressed to inflated. Tubercles are concentrated on the umbilical and ventrolateral shoulders. The suture, similar in all members, is ammonitic; raggedy with spikey subdivided lobes and irregularly subdivided saddles. The Schloenbachiidae first appeared near the end of the Albian, beginning with '' Schloenbachia'', derived from the hoplitid genus '' Pleurohoplites'' or perhaps '' Lepthoplites'', just before the beginning of the Late Cretaceous. References * Arkell ''et al.'', 1957. Mesozoic Ammonoidea; Treatise on Invertebrate Paleontology, Part L (Ammonoidea). Geol. Soc. of America and Univ. Kansas Press. Hoplitoidea Ammonitida families Albian first appearances Cenomanian extinctions { ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Schloenbachia
''Schloenbachia'' is a genus of ammonoid cephalopods from the Cenomanian stage of the Upper Cretaceous, and type for the Schloenbachiidae, a family within the ammonitid Hoplitoidea Hoplitoidea, formerly Hoplitaceae, is a superfamily of mostly Upper Cretaceous ammonites comprising families united by a similar suture pattern with multiple similar elements that tend to decrease in size going toward the umbi ....Arkell ''et al.'', Mesozoic Ammonoidea; Treatise on Invertebrate Paleontology, Part L, 1957. ''Schloenbachia'' was named by Newmayer, 1875, the type species is Schloenbachia varians (Sowerby 1817). The genus has been found in Europe (France, Germany, England), the Middle East (Iran), and North America (California, Oregon). Species ''Schloenbachia varians'' ''Schloenbachia varians'', known from Europe and Iran, is a highly varied species with a number of possible synonyms. Variations include ''S. varians'' (var) ''subvarinas'', ''S.v''. (var) ''subt ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hoplitoidea
Hoplitoidea, formerly Hoplitaceae, is a superfamily of mostly Upper Cretaceous ammonites comprising families united by a similar suture pattern with multiple similar elements that tend to decrease in size going toward the umbilicus, at the inner edge of any whorl, and which are typically in a straight line. Sutural elements are commonly ammonitic, but in some saddles and in others both saddles and lobes are smooth and undivided. Shells are variable in form, both ribbed, evolute forms and smooth, involute forms are included.Arkell et al 1957. Mesozoic Ammonoidea; Treatise on Invertebrate Paleontology, Part L. Families regarded as part now include the Engonoceratidae, Hoplitidae, Placenticeratidae, and Schloenbachiidae. Some classifications however include the Forbesiceridae in place of the Engonoceratidae The older version of the Treatise includes in addition to the five families already mentioned, the Pulchelliidae, Trochleiceratidae, Douvilleiceratidae, D ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hoplitidae
The Hoplitidae is a family of Cretaceous ammonites that lived during the middle of the period from the late Aptian to the Cenomanian. They are part of the superfamily Hoplitoidea. Members of the Hoplitidae are typically evolute, with inner whorls exposed, although some are more involute, and are commonly stout and strongly ribbed, with pronounced tubercles. The Hoplitidae are thought to be derived from the U Aptian -M Albian '' Uligella'' of the Desmoceratidae, or some related form and have been divided into three subfamilies. Subtaxa Classification of Hoplitidae was revised multiple times during last decades. Currently, is contains 3 subfamilies:Amédro, F., Matrion, B., Magniez-Jannin, F., & Touch, R. (2014). La limite Albien inférieur-Albien moyen dans l’Albien type de l’Aube (France): ammonites, foraminifères, séquences. Revue de Paléobiologie, 33(1), 159-279. * Gastroplitinae ** '' Freboldiceras'' ** ''Arcthoplites'' ** ?'' Sokolovites'' ** '' Pseudopulchellia'' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pleurohoplites
''Pleurohoplites'' is a genus in the ammonitid family Hoplitidae, found in middle Cretaceous (Upper Albian - Cenomanian The Cenomanian is, in the ICS' geological timescale, the oldest or earliest age of the Late Cretaceous Epoch or the lowest stage of the Upper Cretaceous Series. An age is a unit of geochronology; it is a unit of time; the stage is a unit in the s ...) of Europe, and included in the subfamily Hoplitinae. ''Pleurohoplites'' has a somewhat involute, compressed to rather inflated shell, with a rounded to subcoronate venter, that bears umbilical tubercles from which branch strong, un-looped, ribs that end in ventrolateral nodes, or are continuous to the siphonal line. References * R.C. Moore (ed), ''Treatise on Invertebrate Paleontology'', Part L: Ammonoidea. ''Geological Soc of America'' and Univ. Kansas Press, 1957, p. L397-nb, 398 Ammonitida genera Hoplitidae Fossil taxa described in 1921 {{ammonite-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ammonitida Families
Ammonitida is an order of Ammonoidea, ammonoid cephalopods that lived from the Jurassic through Paleocene time periods, commonly with intricate ammonitic sutures. Ammonitida is divided into four suborders, the Phylloceratina, Lytoceratina, Ancyloceratina, and Ammonitina. The Phylloceratina is the ancestral stock, derived from the Ceratitida near the end of the Triassic. The Phylloceratina gave rise to the Lytoceratina near the beginning of the Jurassic which in turn gave rise to the highly specialized Ancyloceratina near the end of the Jurassic. Both the Phylloceratina and Lytoceratina gave rise to various stocks combined in the Ammonitina. These four suborders are further divided into different stocks, comprising various families combined into superfamilies. Some like the Hildoceratoidea and Stephanoceratoidea are restricted to the Jurassic. Others like the Hoplitoidea and Acanthoceratoidea are known only from the Cretaceous. Still others like the Perisphinctoidea are found ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Albian First Appearances
The Albian is both an age of the geologic timescale and a stage in the stratigraphic column. It is the youngest or uppermost subdivision of the Early/Lower Cretaceous Epoch/Series. Its approximate time range is 113.0 ± 1.0 Ma to 100.5 ± 0.9 Ma (million years ago). The Albian is preceded by the Aptian and followed by the Cenomanian. Stratigraphic definitions The Albian Stage was first proposed in 1842 by Alcide d'Orbigny. It was named after Alba, the Latin name for River Aube in France. A Global Boundary Stratotype Section and Point (GSSP), ratified by the IUGS in 2016, defines the base of the Albian as the first occurrence of the planktonic foraminiferan '' Microhedbergella renilaevis'' at the Col de Pré-Guittard section, Arnayon, Drôme, France. The top of the Albian Stage (the base of the Cenomanian Stage and Upper Cretaceous Series) is defined as the place where the foram species '' Rotalipora globotruncanoides'' first appears in the stratigraphic column. The Albian i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |