Eopsephaea torulosa
No picture of Eopsephaea torulosa was found. Wikidata and iDigBio were searched and had none. Wikipedia and 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 Eopsephaea torulosa, or no answer at all. This entry cannot say which.
On record
Recorded, not inferred- Sits inside
- EopsephaeaPBDB
- Diet
- carnivorePBDB, for Volutidae
- Life habit
- epifaunalPBDB, for Volutidae
- Motility
- actively mobilePBDB, for Volutidae
- Vision
- limitedPBDB, for Gastropoda
Time the record covers
At least 18 million years on record.
The record covers at least 56 Mya to 37.71 Mya. No occurrence read is dated outside 59.24 Mya to 33.9 Mya.
6 occurrences of Eopsephaea torulosa on record, most of them in the Eocene. 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
6 occurrencesThese 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
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The named rock units Eopsephaea torulosa has been recovered from, largest first. Drawn where the rock is now, not where it formed. 5 occurrences have no formation on record, which is common for older literature.
Eopsephaea torulosa and its relatives
EoceneWhere Eopsephaea torulosa and its relatives were recorded in the Eocene.
Found in the same rock
311 taxa- Ampullina4 sites
- Cepatia cepacea3 sites
- Chama calcarata3 sites
- Conus diversiformis3 sites
- Galeodea (Mambrinia) nodosa3 sites
- Rimella fissurella3 sites
- Seraphs3 sites
- Trachycardium3 sites
- Turricula3 sites
- Angaria2 sites
- Arca biangula2 sites
- Athleta2 sites
- Batillaria2 sites
- Benoistia2 sites
- Borsonia2 sites
- Calyptraea2 sites
- Calyptraea (Trochita) aperta2 sites
- Cerithiopsis2 sites
- Cerithium (Ptychocerithium)2 sites
- Chama fimbriata2 sites
- Clavilithes2 sites
- Conus2 sites
- Ficus greenwoodi2 sites
- Haustator2 sites
The Paleobiology Database records 6 sites for Eopsephaea torulosa, 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
4 references- Fauna de moluste a depozitelor Paleogene din nord-vestul Transilvaniei [Molluscan fauna from Paleogene deposits from NW Transilvania]3
- Five shallow benthic mollusc faunas from the Upper Eocene (Baron, Priabona, Garoowe, Nanggulan, Takashima)1
- Karagyuleva, 19641
- Mollusca of the Babica Clays (Paleocene) of the Middle Carpathians. Pt. I. Gastropoda1
Each of the 6 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 the Paleobiology Database's own record for the work.
Media and terms
Media content0
No picture of Eopsephaea torulosa was found. Wikidata and iDigBio were searched and had none.
Wikipedia and 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 Eopsephaea torulosa, or no answer at all. This entry cannot say which.
No 3D scan of Eopsephaea torulosa 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.
This is what the site found, which is not the same as what exists.
Keep going
What may have been alongside itEopsephaea through timeFormations of the EoceneThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. (Deshayes 1835)