Pseudomulceodens cancellatus

No picture of Pseudomulceodens cancellatus 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 Pseudomulceodens cancellatus, or no answer at all. This entry cannot say which.

On record

Recorded, not inferred
Sits inside
PseudomulceodensPBDB
Diet
suspension feederPBDB, for Rostroconchia
Life habit
semi-infaunalPBDB, for Rostroconchia
Motility
stationaryPBDB, for Rostroconchia
Vision
blindPBDB, for Rostroconchia

Time the record covers

At least 12 million years on record.

The record covers at least 342.9 Mya to 330.3 Mya. No occurrence read is dated outside 351.9 Mya to 323.4 Mya.

Carboniferous — about 10 of 10 occurrencesCarboniferous352–351 Mya — about 0.4 occurrences351–350 Mya — about 1.0 occurrences350–350 Mya — about 1.0 occurrences350–349 Mya — about 1.0 occurrences349–348 Mya — about 1.0 occurrences348–347 Mya — about 1.0 occurrences347–346 Mya — about 1.0 occurrences346–345 Mya — about 1.0 occurrences345–344 Mya — about 1.0 occurrences344–343 Mya — about 0.7 occurrences331–330 Mya — about 0.1 occurrences330–329 Mya — about 0.1 occurrences329–328 Mya — about 0.1 occurrences328–327 Mya — about 0.1 occurrences327–326 Mya — about 0.1 occurrences326–325 Mya — about 0.1 occurrences325–324 Mya — about 0.1 occurrences324–323 Mya — about 0.1 occurrences342.9 Mya330.3 Mya352.5 Mya322.8 Mya

10 occurrences of Pseudomulceodens cancellatus 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

10 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

5 formations

Logan — 38.78°N, 82.93°WLogan — 38.86°N, 82.86°WLogan — 40.04°N, 82.40°WNew Providence — 38.09°N, 85.72°WNew Providence — 38.16°N, 85.78°WRedoak Hollow — 34.37°N, 97.34°WSantiago — 17.58°N, 97.11°WCuyahoga — 40.04°N, 82.40°W

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

Pseudomulceodens cancellatus and its relatives

Carboniferous

Where Pseudomulceodens cancellatus and its relatives were recorded in the Carboniferous.

Found in the same rock

195 taxa

The Paleobiology Database records 10 sites for Pseudomulceodens cancellatus, 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

5 references

Each of the 10 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 Pseudomulceodens cancellatus 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 Pseudomulceodens cancellatus, or no answer at all. This entry cannot say which.

No 3D scan of Pseudomulceodens cancellatus 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 itPseudomulceodens through timeFormations of the CarboniferousThe world it lived on

Occurrence data from the Paleobiology Database, CC BY 4.0. (Hyde 1953)