Olcostephanus
Olcostephanus is an extinct ammonoid cephalopod genus belonging to the family Olcostephanidae. These fast-moving nektonic carnivores lived during the Cretaceous, from the upper Valanginian to the lower Hauterivian age.
Uncredited · via Wikipedia/Commons. May be a photograph of a specimen, or an artist’s reconstruction — an interpretation of a skeleton, since colour and soft tissue are almost never preserved.
On record
Recorded, not inferred- Sits inside
- OlcostephaninaePBDB
- Diet
- carnivorePBDB, for Ammonoidea
- Life habit
- nektonicPBDB, for Ammonoidea
- Motility
- fast-movingPBDB, for Ammonoidea
- Vision
- well-developedPBDB, for Cephalopoda
- Environment
- marinePBDB, for Cephalopoda
Time the record covers
At least 10 million years on record.
The record covers at least 143.1 Mya to 132.6 Mya. No occurrence read is dated outside 161.5 Mya to 121.4 Mya.
656 occurrences of Olcostephanus on record, most of them in the Early Cretaceous. Bar height is expected occurrences, not a count: each fossil is spread across the span it is dated to, so a tall narrow bar means tight dating and a low wide one means loose.
When
656 occurrences- Late Jurassicunder 1%
- Early Cretaceous100%
These are dates about fossils, not the animal: the record can only begin after it arose and end before it died out, so either end may reach further. Shares are expected occurrences: a fossil dated to a span is counted partly in each period it straddles. More on what this infers.
Found in
35 formations
- Agrio Formation · Mendoza Group68
- Miravetes Formation37
- Taraises Formation25
- El Mergueb Formation · M' Chergua Group23
- Maiolica Formation12
- Bersek Marl Formation12
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The named rock units Olcostephanus has been recovered from, largest first. Drawn where the rock is now, not where it formed. 11 further formations hold fewer occurrences each and are not listed. 390 occurrences have no formation on record, which is common for older literature.
Olcostephanus and its relatives
Early CretaceousWhere Olcostephanus and its relatives were recorded in the Early Cretaceous.
Found in the same rock
400 taxa- Neolissoceras grasianum55 sites
- Bochianites neocomiensis30 sites
- Thurmanniceras24 sites
- Tintinnopsella24 sites
- Lytoceras22 sites
- Remaniella22 sites
- Thurmanniceras pertransiens21 sites
- Calpionellopsis20 sites
- Lorenziella19 sites
- Neocomites neocomiensis19 sites
- Kilianella roubaudiana18 sites
- Phylloceras16 sites
- Calpionellites14 sites
- Protancyloceras14 sites
- Bochianites13 sites
- Calcicalathina13 sites
- Kilianella13 sites
- Praecalpionellites13 sites
- Neocomites12 sites
- Phyllopachyceras winkleri12 sites
- Rucinolithus wisei12 sites
- Crioceratites11 sites
- Lytoceras subfimbriatum11 sites
- Neocomites premolicus11 sites
The Paleobiology Database records 484 sites for Olcostephanus, and this reads 240 of them. The number is how many of those sites it was catalogued from too. The 24 sharing the most are listed.
This is not a list of everything alive at the time. It is only what has come out of the same ground as this animal and been written down.
Entered from
68 references- L'évolution des ammonites du Valanginien-Hauterivien inférieur du bassin Vocontien et de la plate-form Provençale (sud-est de la France): relations avec la stratigraphie séquentielle et implications biostratigraphiques271
- Lower Cretaceous ammonites from the Neuquén Basin, Argentina: a Hauterivian Olcostephanus fauna29
- Lower Cretaceous ammonites from the Neuquen Basin, Argentina: Viluceras, a new Valanginian subgenus of Olcostephanus29
- Valanginian (Early Cretaceous ) ammonite faunas from the western High Atlas, Morocco, and the recognition of western Mediterranean 'standard' zones28
- The Berriasian/Valanginian boundary in the Mediterranean region: new data from the Caravaca and Cehegin sections, SE Spain27
- Ammonoid and foraminiferal biostratigraphy from uppermost Valanginian to lowermost Barremian of the Jebel Boulahouajeb section (northern Tunisia)23
- Early Crioceratites (heteromorphic ammonites) from the lower Hauterivian of south-eastern France: systematics, intraspecific variation and biostratigraphic implications15
- Valanginian ammonite biostratigraphy of the La Peña del Águila section, Zacatecas State, northern Mexico14
- Valanginian and early Hauterivian ammonite successions in the Mt Catria group (Central Apennines) and the Lessini Mts (Southern Alps), Italy13
- Le Crétacé inférieur de l'arc subalpin de Castellane entre l'Asse et le Var: Stratigraphy et Sédimentologie13
- Integrated Lower Cretaceous biostratigraphy of the Bersek Quarry, Gerecse Mountains, Transdanubian Range. Hungary12
- Integrated isotope and biostratigraphy of a Lower Cretaceous section from the Bakony Mountains (Transdanubian Range, Hungary): A new Tethyan record of the Weissert event10
Each of the 656 occurrences read was entered from one of these publications, ordered by how many each accounts for. This is not a search for papers mentioning the name. 56 further references are not listed. Entries link to doi.org where the Paleobiology Database holds an identifier, and to its own record where it does not. Relayed as the Paleobiology Database holds them, not checked against what they resolve to.
Media and terms
Media content1
Picture of Olcostephanus
- Source
- Wikipedia/Commons
- Credit
- nobody named on the record
- Licence
- not stated by the source
- Commercial use
- cannot be read from the licence given — check the record
No 3D scan of Olcostephanus was found in MorphoSource and Sketchfab.
Smithsonian Open Access was not reached for this taxon, so this list is what the others held rather than everything there is.
The description on this site
- Licence
- CC BY-SA 4.0
This is what the site found, which is not the same as what exists.
Keep going
What may have been alongside itOlcostephaninae through timeFormations of the Early CretaceousThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. (Neumayr 1875)