Agnosphitys cromhallensis

No picture of Agnosphitys cromhallensis 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 Agnosphitys cromhallensis, or no answer at all. This entry cannot say which.

On record

Recorded, not inferred
Sits inside
AgnosphitysPBDB
Motility
actively mobilePBDB, for Osteichthyes
Environment
terrestrialPBDB, for Diapsida

Time the record covers

At most 9.7 million years on record.

The one occurrence read is dated to somewhere between 237 Mya and 227.3 Mya, which is a dating window rather than a span.

Middle Triassic — about 0 of 1 occurrenceLate Triassic — about 1 of 1 occurrenceLate Triassic237–237 Mya — about 0.0 occurrences237–236 Mya — about 0.0 occurrences236–236 Mya — about 0.0 occurrences236–236 Mya — about 0.0 occurrences236–235 Mya — about 0.0 occurrences235–235 Mya — about 0.0 occurrences235–235 Mya — about 0.0 occurrences235–234 Mya — about 0.0 occurrences234–234 Mya — about 0.0 occurrences234–234 Mya — about 0.0 occurrences234–233 Mya — about 0.0 occurrences233–233 Mya — about 0.0 occurrences233–233 Mya — about 0.0 occurrences233–232 Mya — about 0.0 occurrences232–232 Mya — about 0.0 occurrences232–231 Mya — about 0.0 occurrences231–231 Mya — about 0.0 occurrences231–231 Mya — about 0.0 occurrences231–230 Mya — about 0.0 occurrences230–230 Mya — about 0.0 occurrences230–230 Mya — about 0.0 occurrences230–229 Mya — about 0.0 occurrences229–229 Mya — about 0.0 occurrences229–229 Mya — about 0.0 occurrences229–228 Mya — about 0.0 occurrences228–228 Mya — about 0.0 occurrences228–228 Mya — about 0.0 occurrences228–227 Mya — about 0.0 occurrences237.5 Mya226.8 Mya

1 occurrence of Agnosphitys cromhallensis on record, most of them in the Late Triassic. 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.

Agnosphitys cromhallensis and its relatives

Late Triassic

Where Agnosphitys cromhallensis and its relatives were recorded in the Late Triassic.

Found in the same rock

2 taxa

The Paleobiology Database records 1 site for Agnosphitys cromhallensis, 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 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 Agnosphitys cromhallensis 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 Agnosphitys cromhallensis, or no answer at all. This entry cannot say which.

No 3D scan of Agnosphitys cromhallensis 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

What may have been alongside itAgnosphitys through timeFormations of the Late TriassicThe world it lived on

Occurrence data from the Paleobiology Database, CC BY 4.0. Fraser et al. 2002