Karakaschiceras biassalense
No picture of Karakaschiceras biassalense was found. Wikipedia, Wikidata and iDigBio were searched and had none. Smithsonian Open Access did not answer, so this is what the others held rather than everything there is. GBIF was asked, and what came back is not recorded: nothing, or a picture this site could not tie to Karakaschiceras biassalense, or no answer at all. This entry cannot say which.
On record
Recorded, not inferred- Sits inside
- KarakaschicerasPBDB
- 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 most 4.5 million years on record.
Every occurrence read is dated to somewhere between 137.05 Mya and 132.6 Mya, and nothing in the dating separates them, so that window is what the record shows rather than a span.
23 occurrences of Karakaschiceras biassalense 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
23 occurrences- 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
5 formations
- Sidi Lhousseine Formation2
- Argiles Brunes Formation2
- Sabinal Formation2
- Brasov Formation1
- Grand Essert Formation1
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The named rock units Karakaschiceras biassalense has been recovered from, largest first. Drawn where the rock is now, not where it formed. 15 occurrences have no formation on record, which is common for older literature.
Karakaschiceras biassalense and its relatives
Early CretaceousWhere Karakaschiceras biassalense and its relatives were recorded in the Early Cretaceous.
Found in the same rock
80 taxa- Olcostephanus10 sites
- Olcostephanus atherstoni8 sites
- Bochianites neocomiensis7 sites
- Lytoceras7 sites
- Neocomites neocomiensis7 sites
- Neolissoceras salinarium7 sites
- Busnardoites6 sites
- Busnardoites campylotoxus5 sites
- Neohoploceras5 sites
- Neolissoceras grasianum5 sites
- Phylloceras5 sites
- Phylloceras semisulcatum5 sites
- Euphylloceras thetys4 sites
- Luppovella (Luppovella) superba4 sites
- Neocomites4 sites
- Neocomites (Eristavites) teschenensis4 sites
- Neocomites platycostatus4 sites
- Kilianella roubaudiana3 sites
- Neohoploceras arnoldi3 sites
- Neolissoceras cornutus3 sites
- Kilianella2 sites
- Lytoceras juilleti2 sites
- Olcostephanus (Olcostephanus) tenuituberculatus2 sites
- Parrasites victoriensis2 sites
The Paleobiology Database records 23 sites for Karakaschiceras biassalense, and this reads all 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
7 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 biostratigraphiques8
- Valanginian (Early Cretaceous ) ammonite faunas from the western High Atlas, Morocco, and the recognition of western Mediterranean 'standard' zones7
- The Berriasian-Valanginian (Early Cretaceous) boundary transition at Santa Catarina Ticuá, Oaxaca state, southern Mexico: ammonites, bivalves, calpionellids and their paleobiogeographic significance2
- Le Valanginien du bassin de Safi (Maroc atlantique) et sa faune d’ammonites. Implications paleobiogeographiques2
- Lithostratigraphy, biostratigraphy and sedimentary dynamics of the Lower Cretaceous deposits on the northern side of the western High Atlas (Morocco)2
- Itierella melognensis n.gen., n.sp., and Paradicostella hautevillelompnesensis n.gen., n.sp. (Ammonoidea, Neocomitidae, Neocomitinae), two new upper Valanginian trituberculated ammonoids from the Jura Mountains, eastern France1
- A peculiar Upper Valanginian cephalopod fauna from the Carpatic Bend (Codlea town area, Romania): biostratigraphic and paleobiogeographic implications1
Each of the 23 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. 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 content0
No picture of Karakaschiceras biassalense was found. Wikipedia, Wikidata and iDigBio were searched and had none.
Smithsonian Open Access did not answer, so this is what the others held rather than everything there is.
GBIF was asked, and what came back is not recorded: nothing, or a picture this site could not tie to Karakaschiceras biassalense, or no answer at all. This entry cannot say which.
No 3D scan of Karakaschiceras biassalense was found in Sketchfab.
Smithsonian Open Access and MorphoSource were not reached for this taxon, so this list is what the others held rather than everything there is.
This is what the site found, which is not the same as what exists.
Keep going
What may have been alongside itKarakaschiceras through timeFormations of the Early CretaceousThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. (Karakaschi 1889)