Caseodus eatoni

No picture of Caseodus eatoni was found. Wikidata, iDigBio and Smithsonian Open Access were searched and had none. Wikipedia has a picture filed under this name, but nothing tied it to Caseodus eatoni itself, so it was not used. GBIF was asked, and what came back is not recorded: nothing, or a picture this site could not tie to Caseodus eatoni, or no answer at all. This entry cannot say which.

On record

Recorded, not inferred
Sits inside
CaseodusPBDB
Diet
carnivorePBDB, for Eugeneodontiformes
Life habit
nektonicPBDB, for Eugeneodontiformes
Motility
actively mobilePBDB, for Eugeneodontiformes

Time the record covers

At most 12 million years on record.

Every occurrence read is dated to somewhere between 315.2 Mya and 303.7 Mya, and nothing in the dating separates them, so that window is what the record shows rather than a span.

Carboniferous — about 3 of 3 occurrencesCarboniferous315–315 Mya — about 0.1 occurrences315–314 Mya — about 0.1 occurrences314–314 Mya — about 0.1 occurrences314–314 Mya — about 0.1 occurrences314–313 Mya — about 0.1 occurrences313–313 Mya — about 0.1 occurrences313–312 Mya — about 0.1 occurrences312–312 Mya — about 0.1 occurrences312–312 Mya — about 0.1 occurrences312–311 Mya — about 0.1 occurrences311–311 Mya — about 0.1 occurrences311–310 Mya — about 0.1 occurrences310–310 Mya — about 0.1 occurrences310–309 Mya — about 0.1 occurrences309–309 Mya — about 0.1 occurrences309–309 Mya — about 0.1 occurrences309–308 Mya — about 0.1 occurrences308–308 Mya — about 0.1 occurrences308–307 Mya — about 0.1 occurrences307–307 Mya — about 0.1 occurrences307–307 Mya — about 0.1 occurrences307–306 Mya — about 0.1 occurrences306–306 Mya — about 0.1 occurrences306–305 Mya — about 0.1 occurrences305–305 Mya — about 0.1 occurrences305–304 Mya — about 0.1 occurrences304–304 Mya — about 0.1 occurrences304–304 Mya — about 0.1 occurrences315.7 Mya303.2 Mya

3 occurrences of Caseodus eatoni 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

3 occurrences

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

Staunton — 39.85°N, 87.30°WAltamont Limestone — 37.04°N, 95.53°WMinnelusa — 44.22°N, 103.41°W

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The named rock units Caseodus eatoni has been recovered from, largest first. Drawn where the rock is now, not where it formed.

Caseodus eatoni and its relatives

Carboniferous

Where Caseodus eatoni and its relatives were recorded in the Carboniferous.

Found in the same rock

20 taxa

The Paleobiology Database records 3 sites for Caseodus eatoni, and this reads all of them. The number is how many of those sites it was catalogued from too.

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

3 references

Each of the 3 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 Caseodus eatoni was found. Wikidata, iDigBio and Smithsonian Open Access were searched and had none.

Wikipedia has a picture filed under this name, but nothing tied it to Caseodus eatoni itself, so it was not used.

GBIF was asked, and what came back is not recorded: nothing, or a picture this site could not tie to Caseodus eatoni, or no answer at all. This entry cannot say which.

No 3D scan was found. Smithsonian Open Access, MorphoSource and Sketchfab were all searched.

This is what the site found, which is not the same as what exists.

Keep going

Occurrence data from the Paleobiology Database, CC BY 4.0. Zangerl 1981