Tainoceras nebrascense
No picture of Tainoceras nebrascense 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 Tainoceras nebrascense, or no answer at all. This entry cannot say which.
On record
Recorded, not inferred- Sits inside
- TainocerasPBDB
- 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 8.8 million years on record.
The record covers at least 298.9 Mya to 290.1 Mya. No occurrence read is dated outside 303.7 Mya to 283.3 Mya.
2 occurrences of Tainoceras nebrascense on record. 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
2 occurrences- Carboniferous50%
- Permian50%
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
2 formations
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The named rock units Tainoceras nebrascense has been recovered from, largest first. Drawn where the rock is now, not where it formed.
Found in the same rock
70 taxa- Amphiscapha subrugosa1 site
- Araeonema novamexicanum1 site
- Astartella subquadrata1 site
- Aviculopecten arctisulcatus1 site
- Bakevellia1 site
- Bellerophon graphicus1 site
- Cancrinella boonensis1 site
- Carinanema kietzkei1 site
- Cerithioides1 site
- Coopericus semisulcatus1 site
- Crurithyris planoconvexa1 site
- Cyclites diminutus1 site
- Echinaria1 site
- Edmondia nebrascensis1 site
- Euphemites1 site
- Euphemites graffhami1 site
- Girtyspira minuta1 site
- Glabrocingulum (Ananias) tularosaensis1 site
- Globulobactrites sp.1 site
- Goniasma lasallense1 site
- Hemizyga (Hemizyga)1 site
- Hypergonia percostata1 site
- Leptodesma welleri1 site
- Leptoptygma carrizoensis1 site
The Paleobiology Database records 2 sites for Tainoceras nebrascense, 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
2 references- Stratigraphy and brachiopod and molluscan paleontology of the Red Tanks Formation (Madera Group) near the Pennsylvanian–Permian boundary, Lucero uplift, west-central New Mexico1
- American Permian nautiloids1
Each of the 2 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 Tainoceras nebrascense 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 Tainoceras nebrascense, or no answer at all. This entry cannot say which.
No 3D scan of Tainoceras nebrascense 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 itTainoceras through timeThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. Miller et al. 1933