Podocrates dulmensis

No picture of Podocrates dulmensis was found. Wikidata was searched and had none. iDigBio and GBIF were not searched: the Paleobiology Database does not place Podocrates dulmensis firmly enough to tell it from something else bearing the same name, and a search on the name alone returns whichever of them was photographed. Wikipedia and Smithsonian Open Access did not answer, so this is what the others held rather than everything there is.

On record

Recorded, not inferred
Sits inside
PodocratesPBDB

Time the record covers

At most 8.2 million years on record.

Every occurrence read is dated to somewhere between 93.9 Mya and 85.7 Mya, and nothing in the dating separates them, so that window is what the record shows rather than a span.

Late Cretaceous — about 2 of 2 occurrencesLate Cretaceous94–94 Mya — about 0.0 occurrences94–93 Mya — about 0.1 occurrences93–93 Mya — about 0.1 occurrences93–93 Mya — about 0.1 occurrences93–93 Mya — about 0.1 occurrences93–92 Mya — about 0.1 occurrences92–92 Mya — about 0.1 occurrences92–92 Mya — about 0.1 occurrences92–91 Mya — about 0.1 occurrences91–91 Mya — about 0.1 occurrences91–91 Mya — about 0.1 occurrences91–90 Mya — about 0.1 occurrences90–90 Mya — about 0.1 occurrences90–90 Mya — about 0.1 occurrences90–89 Mya — about 0.1 occurrences89–89 Mya — about 0.1 occurrences89–89 Mya — about 0.1 occurrences89–89 Mya — about 0.1 occurrences89–88 Mya — about 0.1 occurrences88–88 Mya — about 0.1 occurrences88–88 Mya — about 0.1 occurrences88–87 Mya — about 0.1 occurrences87–87 Mya — about 0.1 occurrences87–87 Mya — about 0.1 occurrences87–86 Mya — about 0.1 occurrences86–86 Mya — about 0.1 occurrences86–86 Mya — about 0.1 occurrences86–86 Mya — about 0.0 occurrences94.4 Mya85.2 Mya

2 occurrences of Podocrates dulmensis on record, most of them in the Late Cretaceous. 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

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

Teplice — 49.89°N, 14.42°EBřezno — 50.27°N, 16.75°E

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

Podocrates dulmensis and its relatives

Late Cretaceous

Where Podocrates dulmensis and its relatives were recorded in the Late Cretaceous.

Found in the same rock

4 taxa

The Paleobiology Database records 2 sites for Podocrates dulmensis, 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

1 reference

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. Each entry links to the Paleobiology Database's own record for the work.

Media and terms

Media content0

No picture of Podocrates dulmensis was found. Wikidata was searched and had none.

iDigBio and GBIF were not searched: the Paleobiology Database does not place Podocrates dulmensis firmly enough to tell it from something else bearing the same name, and a search on the name alone returns whichever of them was photographed.

Wikipedia and Smithsonian Open Access did not answer, so this is what the others held rather than everything there is.

No 3D scan of Podocrates dulmensis 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

Occurrence data from the Paleobiology Database, CC BY 4.0. Becks 1851