Arcticoceras

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Arcticoceras
Temporal range: Bathonian [1]
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Arcticoceras.jpg
Arcticoceras cranocephaloides fossils at the Geological Museum in Copenhagen
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Arcticoceras [2]

Spath,(1924)

Arcticoceras is an extinct ammonoid cephalopod genus from the late Middle Jurassic belonging to the ammonite family Cardioceratidae, more commonly found to high northern latitudes.

The Arcticoceras shell is involute, inner whorls sharply ribbed, outer ones becoming smooth. [3] The suture, following the description of the Stephanoceratoidea, is complex, ammonitic, with a dominant 1st lateral lobe and well-developed umbilical lobe. May be derived from Arctocephalites .

Arcticoceras is found in northern Alaska, arctic Canada, Greenland, northern and central Russia, as well as in Wyoming, North Dakota, and Utah. [3] Part of the fauna that lived in high latitude (arctic and subarctic) marine waters during the second half of the Middle Jurassic.

Arcticoceras kochi and A ishmanae have been found in the boreal Bathonian stage of central East Greenland. Arcticoceras and Arctocephalites are found the Volga River Basin, Sartov Region, and Arctocephalites in the Pechora River Basin indicating an earlier and deeper penetration of arctic water into European Russia than previously thought. [4]

Related Research Articles

In the geologic timescale, the Bajocian is an age and stage in the Middle Jurassic. It lasted from approximately 170.9 ±0.8 Ma to around 168.2 ±1.2 Ma. The Bajocian Age succeeds the Aalenian Age and precedes the Bathonian Age.

In the geologic timescale the Bathonian is an age and stage of the Middle Jurassic. It lasted from approximately 168.2 ±1.2 Ma to around 165.3 ±1.1 Ma. The Bathonian Age succeeds the Bajocian Age and precedes the Callovian Age.

In the geologic timescale, the Callovian is an age and stage in the Middle Jurassic, lasting between 165.3 ± 1.1 Ma and 161.5 ± 1.0 Ma. It is the last stage of the Middle Jurassic, following the Bathonian and preceding the Oxfordian.

<i>Acanthohoplites</i> Extinct genus of Cretaceous ammonites

Acanthohoplites is an extinct genus of ammonites in the family Parahoplitidae that lived in the Aptian and Early Albian stages of the Early Cretaceous.

Alcidellus is an oxyconic haploceratacean ammonite from the Middle Jurassic.

<i>Audaxlytoceras</i> Genus of molluscs (fossil)

Audaxlytoceras is an extinct genus of lytoceratid ammonites.

Arctocephalites is an extinct ammonitic cephalopod genus from the Middle Jurassic with a wide northern distribution belonging to the stephanoceratacean family, Cardioceratidae.

Arctomercaticeras is an extinct genus of cephalopod belonging to the Ammonite subclass and the family Hildoceratidae that lived during the Early Jurassic in the Arctic zone of Russia.

<i>Oppelia</i> Genus of molluscs (fossil)

Oppelia is a haploceratoid ammonite and type genus for the Oppeliidae that lived during the Middle Jurassic. Shells of Oppelia are involute with a small to moderate size umbilicus, bluntly rounded to sharp venter, and deeply impressed dorsum. Sides are generally smooth but may be variously ribbed on the outer flanks. Similar and related genera include Oxycerites and Oecotraustes.

<i>Nannolytoceras</i> Genus of molluscs (fossil)

Nannolytoceras is an extinct genus of lytoceratid ammonite, family Lytoceratidae, with a stratigraphic range extending from the Bajocian age to Bathonian age.

<i>Psiloceras</i> Genus of molluscs (fossil)

Psiloceras is an extinct genus of ammonite. Psiloceras is among the earliest known Jurassic ammonites, and the appearance of the earliest Psiloceras species form the definition for the base of the Jurassic. Unlike most earlier ammonites, which had complex shell shapes and ornamentation, Psiloceras had a smooth shell.

<i>Craspedites</i> Genus of molluscs (fossil)

Craspedites is an ammonoid cephalopod included in the Perisphinctoidea that lived during the Late Jurassic and Early Cretaceous, found in Canada, Greenland, Poland, and the Russian Federation.

<i>Calycoceras</i> Genus of molluscs (fossil)

Calycoceras is an extinct genus of cephalopods belonging to the subclass Ammonoidea and family Acanthoceratidae that lived during the Cenomanian stage of the Late Cretaceous, 100-94 Mya. Their shells had ornate ribs.

<i>Harpoceras</i> Genus of molluscs (fossil)

Harpoceras is an extinct genus of ammonite belonging to the family Hildoceratidae. These cephalopods existed in the Jurassic period, during the Toarcian age from the Falciferum zone to the Commune subzone of the Bifrons zone. They were fast-moving nektonic carnivores.

<i>Reineckeia</i> Genus of molluscs (fossil)

Reineckeia is an extinct genus of ammonoid cephalopods belonging to the family Reineckeiidae.

<i>Pseudopeltoceras</i> Genus of molluscs (fossil)

Pseudopeltoceras is a genus of perisphinctoid ammonites belonging to the family Perisphinctidae.

<span class="mw-page-title-main">Parkinsoniidae</span> Extinct family of ammonites

Parkinsoniidae is a family of ammonites belonging to the order Ammonitida. The cephalopod family lived from the Bajocian stage to the Bathonian age of the Middle Jurassic.

<i>Parkinsonia</i> (ammonite) Genus of molluscs (fossil)

Parkinsonia is a genus of ammonites belonging to the family Parkinsoniidae.

Reynesoceras is genus of ammonites that lived during the upper Pliensbachian stage of early Jurassic. It has evolved from Prodactylioceras, or Cetonoceras. Dactylioceras (Eodactylites) has probably evolved from this genus. Aveyroniceras is a name for macroconchs of this genus. Their fossils were found in Europe, northern Africa, Asia, North America and South America.

References

  1. Sepkoski, Jack (2002). "Sepkoski's Online Genus Database" . Retrieved 2014-05-28.
  2. "Paleobiology Database - Arcticoceras" . Retrieved 2017-10-19.
  3. 1 2 Arkell et al,1957, Mesozoic Ammonoidea, Treatise on Invertebrate Paleontology, Part L, Mollusca 4, R.C. Moore, ed. p.L301 -L303
  4. Meledina, S. V.; Nal'Nyaeva, T. I.; Shurygin, B. N. (2009). "Correlation of upper Bajocian-Bathonian zones in Siberia with the stage standard". Stratigraphy and Geological Correlation. 17 (3): 291–297. Bibcode:2009SGC....17..291M. doi:10.1134/S0869593809030058.