Ogiva promonturiorum
No picture of Ogiva promonturiorum 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 Ogiva promonturiorum, or no answer at all. This entry cannot say which.
On record
Recorded, not inferred- Sits inside
- OgivaPBDB
- Diet
- suspension feederPBDB, for Cheilostomata
- Life habit
- epifaunalPBDB, for Cheilostomata
- Motility
- stationary, attachedPBDB, for Cheilostomata
- Vision
- blindPBDB, for Gymnolaemata
- Environment
- marinePBDB, for Lophophorata
Time the record covers
At most 14 million years on record.
Every occurrence read is dated to somewhere between 85.7 Mya and 72.2 Mya, and nothing in the dating separates them, so that window is what the record shows rather than a span.
5 occurrences of Ogiva promonturiorum on record, most of them in the Late 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
5 occurrences- Late 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
3 formations
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The named rock units Ogiva promonturiorum has been recovered from, largest first. Drawn where the rock is now, not where it formed. 2 occurrences have no formation on record, which is common for older literature.
Ogiva promonturiorum and its relatives
Late CretaceousWhere Ogiva promonturiorum and its relatives were recorded in the Late Cretaceous.
Found in the same rock
44 taxa- Acrochordonia bifurcata1 site
- Acrochordonia irregularis1 site
- Amphithelion1 site
- Amphithelion cupula1 site
- Astrocladia subramosa1 site
- Becksia soekelandi1 site
- Coelocorypha subglobosa1 site
- Craterella auricula1 site
- Craticularia1 site
- Craticularia auricularis1 site
- Craticularia roemeri1 site
- Cystispongia morchella1 site
- Cytoracia turbinata1 site
- Doryderma (Brochodora) roemeri1 site
- Ecblastesia intrinsecuscostata1 site
- Homalodoriana ficus1 site
- Homalodoriana tuberosa1 site
- Jerea1 site
- Jereica1 site
- Jereica polystoma1 site
- Jereica punctata1 site
- Laocoetis vulgata1 site
- Leiochonia cryptoporosa1 site
- Ozotrachelus conicus1 site
The Paleobiology Database records 1 site for Ogiva promonturiorum, 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 5 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 Ogiva promonturiorum 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 Ogiva promonturiorum, or no answer at all. This entry cannot say which.
No 3D scan of Ogiva promonturiorum 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 itOgiva through timeFormations of the Late CretaceousThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. Voigt 1924