Ouaoufilalites creber
No picture of Ouaoufilalites creber 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 Ouaoufilalites creber, or no answer at all. This entry cannot say which.
On record
Recorded, not inferred- Sits inside
- OuaoufilalitesPBDB
- Diet
- carnivorePBDB, for Ammonoidea
- Life habit
- nektonicPBDB, for Goniatitida
- Motility
- fast-movingPBDB, for Ammonoidea
- Vision
- well-developedPBDB, for Cephalopoda
- Environment
- marinePBDB, for Cephalopoda
Time the record covers
At most 13 million years on record.
Every occurrence read is dated to somewhere between 358.86 Mya and 346.7 Mya, and nothing in the dating separates them, so that window is what the record shows rather than a span.
11 occurrences of Ouaoufilalites creber on record, most of them in the Carboniferous. 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
11 occurrences- Carboniferous100%
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
1 formation
Loading coastlines…
The named rock units Ouaoufilalites creber has been recovered from, largest first. Drawn where the rock is now, not where it formed.
Ouaoufilalites creber and its relatives
CarboniferousWhere Ouaoufilalites creber and its relatives were recorded in the Carboniferous.
Found in the same rock
43 taxa- Muensteroceras multitudum7 sites
- Dzhaprakoceras biconvexum6 sites
- Eurites permutus6 sites
- Kusinia falcifera6 sites
- Eurites doliaris5 sites
- Imitoceras dimidium4 sites
- Serpenticyclus inornatus4 sites
- Dzhaprakoceras vergum3 sites
- Follotites folloti3 sites
- Imitoceras strictum3 sites
- Jerania subvexa3 sites
- Mouydiria mouydirensis3 sites
- Muensteroceras subparallelum3 sites
- Nodopericyclus circumnodosus3 sites
- Nodopericyclus deficerus3 sites
- Pericyclus intercisus3 sites
- Progoniatites uncus3 sites
- Serpenticyclus laxaris3 sites
- Temertassetia coarta3 sites
- Acrocanites disparilis2 sites
- Follotites flexus2 sites
- Jerania persimilis2 sites
- Jerania pusillens2 sites
- Pericyclus circulus2 sites
The Paleobiology Database records 11 sites for Ouaoufilalites creber, 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
1 referenceEach of the 11 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. Each entry links to doi.org. Relayed as the Paleobiology Database holds them, not checked against what they resolve to.
Media and terms
Media content0
No picture of Ouaoufilalites creber 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 Ouaoufilalites creber, or no answer at all. This entry cannot say which.
No 3D scan of Ouaoufilalites creber 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 itOuaoufilalites through timeFormations of the CarboniferousThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. Korn et al. 2010