Kataria anisodonta

No picture of Kataria anisodonta 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 Kataria anisodonta, or no answer at all. This entry cannot say which.

On record

Recorded, not inferred
Sits inside
KatariaPBDB
Motility
actively mobilePBDB, for Osteichthyes
Environment
terrestrialPBDB, for Amniota

Time the record covers

At most 4.4 million years on record.

The one occurrence read is dated to somewhere between 66 Mya and 61.66 Mya, which is a dating window rather than a span.

Late Cretaceous — about 0 of 1 occurrencePaleocene — about 1 of 1 occurrencePaleocene66–66 Mya — about 0.0 occurrences66–66 Mya — about 0.0 occurrences66–66 Mya — about 0.0 occurrences66–65 Mya — about 0.0 occurrences65–65 Mya — about 0.0 occurrences65–65 Mya — about 0.0 occurrences65–65 Mya — about 0.0 occurrences65–65 Mya — about 0.0 occurrences65–65 Mya — about 0.0 occurrences65–64 Mya — about 0.0 occurrences64–64 Mya — about 0.0 occurrences64–64 Mya — about 0.0 occurrences64–64 Mya — about 0.0 occurrences64–64 Mya — about 0.0 occurrences64–63 Mya — about 0.0 occurrences63–63 Mya — about 0.0 occurrences63–63 Mya — about 0.0 occurrences63–63 Mya — about 0.0 occurrences63–63 Mya — about 0.0 occurrences63–63 Mya — about 0.0 occurrences63–62 Mya — about 0.0 occurrences62–62 Mya — about 0.0 occurrences62–62 Mya — about 0.0 occurrences62–62 Mya — about 0.0 occurrences62–62 Mya — about 0.0 occurrences62–62 Mya — about 0.0 occurrences66.5 Mya61.2 Mya

1 occurrence of Kataria anisodonta 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

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

Santa Lucía — 18.03°S, 65.58°W

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

Kataria anisodonta and its relatives

Paleocene

Where Kataria anisodonta and its relatives were recorded in the Paleocene.

Found in the same rock

46 taxa

The Paleobiology Database records 1 site for Kataria anisodonta, 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

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 doi.org. Relayed as the Paleobiology Database holds them, not checked against what they resolve to.

Media and terms

Media content0

No picture of Kataria anisodonta 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 Kataria anisodonta, or no answer at all. This entry cannot say which.

No 3D scan of Kataria anisodonta 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 itKataria through timeFormations of the PaleoceneThe world it lived on

Occurrence data from the Paleobiology Database, CC BY 4.0. Scanferla et al. 2013