Cimomia subrecta
No picture of Cimomia subrecta 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 Cimomia subrecta, or no answer at all. This entry cannot say which.
On record
Recorded, not inferred- Sits inside
- CimomiaPBDB
- Diet
- carnivorePBDB, for Nautilida
- Life habit
- nektobenthicPBDB, for Nautilida
- Motility
- actively mobilePBDB, for Nautilida
- Vision
- well-developedPBDB, for Cephalopoda
- Environment
- marinePBDB, for Cephalopoda
Time the record covers
At least 2.4 million years on record.
The record covers at least 61.66 Mya to 59.24 Mya. No occurrence read is dated outside 66 Mya to 56 Mya.
6 occurrences of Cimomia subrecta on record, most of them in the Paleocene. 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 occurrences- Paleocene100%
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
- Clayton Formation · Midway Group4
- Porters Creek Formation1
- Soldado Formation1
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The named rock units Cimomia subrecta has been recovered from, largest first. Drawn where the rock is now, not where it formed.
Cimomia subrecta and its relatives
PaleoceneWhere Cimomia subrecta and its relatives were recorded in the Paleocene.
Found in the same rock
25 taxa- Ostrea pulaskensis3 sites
- Rotularia2 sites
- Teredo2 sites
- Arcoscalpellum toulmini1 site
- Asteroidea1 site
- Bairdia1 site
- Cimomia kugleri1 site
- Cytherella1 site
- Dentalina1 site
- Dentalium1 site
- Echinoidea1 site
- Eutrephoceras1 site
- Gitolampas1 site
- Graphularia1 site
- Hercoglossa harrisi1 site
- Laevibuccinum1 site
- Lenticulina1 site
- Nodosaria1 site
- Ophiuroidea1 site
- Ostrea1 site
- Plagiochasma cruciferum1 site
- Pseudoliva1 site
- Rhopostoma1 site
- Terebratulina brundidgensis1 site
The Paleobiology Database records 6 sites for Cimomia subrecta, 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- Stratigraphic Distribution of Paleocene and Eocene Fossils in the Eastern Gulf Coast Region3
- Catalogue of the Paleocene and Eocene mollusca of the southern and eastern United States. Part 1. Pelecypoda, Amphineura, Pteropoda, Scaphopoda and Cephalopoda1
- Tertiary nautiloids of the Americas: supplement1
- The nautiloid cephalopods of the Midway Group1
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 Cimomia subrecta 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 Cimomia subrecta, or no answer at all. This entry cannot say which.
No 3D scan of Cimomia subrecta 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 itCimomia through timeFormations of the PaleoceneThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. Miller and Thompson 1933