Lupaceradotus useviaensis

No picture of Lupaceradotus useviaensis was found. Wikidata and iDigBio were searched and had none. Wikipedia and 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 Lupaceradotus useviaensis, or no answer at all. This entry cannot say which.

On record

Recorded, not inferred
Sits inside
LupaceradotusPBDB
Motility
actively mobilePBDB, for Osteichthyes
Environment
lagoonal,marine,brackish,freshwaterPBDB, for Dipnoi

Time the record covers

At most 28 million years on record.

The one occurrence read is dated to somewhere between 121.4 Mya and 93.9 Mya, which is a dating window rather than a span.

Early Cretaceous — about 1 of 1 occurrenceEarly CretaceousLate Cretaceous — about 0 of 1 occurrenceLate Cretaceous122–121 Mya — about 0.0 occurrences121–120 Mya — about 0.0 occurrences120–119 Mya — about 0.0 occurrences119–118 Mya — about 0.0 occurrences118–117 Mya — about 0.0 occurrences117–116 Mya — about 0.0 occurrences116–115 Mya — about 0.0 occurrences115–114 Mya — about 0.0 occurrences114–113 Mya — about 0.0 occurrences113–112 Mya — about 0.0 occurrences112–111 Mya — about 0.0 occurrences111–111 Mya — about 0.0 occurrences111–110 Mya — about 0.0 occurrences110–109 Mya — about 0.0 occurrences109–108 Mya — about 0.0 occurrences108–107 Mya — about 0.0 occurrences107–106 Mya — about 0.0 occurrences106–105 Mya — about 0.0 occurrences105–104 Mya — about 0.0 occurrences104–103 Mya — about 0.0 occurrences103–102 Mya — about 0.0 occurrences102–101 Mya — about 0.0 occurrences101–100 Mya — about 0.0 occurrences100–99 Mya — about 0.0 occurrences99–98 Mya — about 0.0 occurrences98–97 Mya — about 0.0 occurrences97–96 Mya — about 0.0 occurrences96–95 Mya — about 0.0 occurrences95–94 Mya — about 0.0 occurrences94–93 Mya — about 0.0 occurrences122 Mya93.3 Mya

1 occurrence of Lupaceradotus useviaensis on record, most of them in the Early 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

1 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

1 formation

Galula — 7.10°S, 31.17°E

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

Lupaceradotus useviaensis and its relatives

Early Cretaceous

Where Lupaceradotus useviaensis and its relatives were recorded in the Early Cretaceous.

Found in the same rock

No other named taxon is catalogued from that site.

The Paleobiology Database records 1 site for Lupaceradotus useviaensis, and this reads all of them.

Entered from

1 reference

Each of the 1 occurrence 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 Lupaceradotus useviaensis was found. Wikidata and iDigBio were searched and had none.

Wikipedia and 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 Lupaceradotus useviaensis, or no answer at all. This entry cannot say which.

No 3D scan of Lupaceradotus useviaensis 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. Gottfried et al. 2009