Pseudoamphiroa propria

No picture of Pseudoamphiroa propria 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 Pseudoamphiroa propria, or no answer at all. This entry cannot say which.

On record

Recorded, not inferred
Sits inside
PseudoamphiroaPBDB
Diet
"photoautotroph"PBDB, for Rhodophyta

Time the record covers

At least 41 million years on record.

The record covers at least 100.5 Mya to 59.24 Mya. No occurrence read is dated outside 113.2 Mya to 56 Mya.

Early Cretaceous — about 1 of 15 occurrencesEarly CretaceousLate Cretaceous — about 0 of 15 occurrencesPaleocene — about 14 of 15 occurrencesPaleoceneEocene — about 0 of 15 occurrences114–112 Mya — about 0.1 occurrences112–110 Mya — about 0.2 occurrences110–108 Mya — about 0.2 occurrences108–106 Mya — about 0.2 occurrences106–104 Mya — about 0.2 occurrences104–102 Mya — about 0.2 occurrences102–100 Mya — about 0.2 occurrences67–65 Mya — about 0.2 occurrences65–63 Mya — about 0.4 occurrences63–61 Mya — about 1 occurrence61–59 Mya — about 3 occurrences59–57 Mya — about 7 occurrences57–55 Mya — about 3 occurrences100.5 Mya59.24 Mya114 Mya55 Mya

15 occurrences of Pseudoamphiroa propria 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

15 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

8 formations

Ulukışla — 37.62°N, 35.00°EKambuhel — 49.38°N, 20.67°EKambuhel — 49.37°N, 18.54°EKambuhel Limestone — 48.57°N, 17.39°ERasov — 48.80°N, 17.73°EHradisko — 49.22°N, 18.62°EHricocske Podhradie — 49.22°N, 18.70°EKambuhel Limestone — 47.54°N, 13.50°EKallakudi limestone — 11.52°N, 78.82°E

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The named rock units Pseudoamphiroa propria has been recovered from, largest first. Drawn where the rock is now, not where it formed. 4 occurrences have no formation on record, which is common for older literature.

Pseudoamphiroa propria and its relatives

Paleocene

Where Pseudoamphiroa propria and its relatives were recorded in the Paleocene.

Found in the same rock

43 taxa

The Paleobiology Database records 8 sites for Pseudoamphiroa propria, 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

6 references

Each of the 15 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 Pseudoamphiroa propria 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 Pseudoamphiroa propria, or no answer at all. This entry cannot say which.

No 3D scan of Pseudoamphiroa propria 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.

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Occurrence data from the Paleobiology Database, CC BY 4.0. (Lemoine 1934)