Torvoneustes carpenteri

No picture of Torvoneustes carpenteri 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 Torvoneustes carpenteri, or no answer at all. This entry cannot say which.

On record

Recorded, not inferred
Sits inside
TorvoneustesPBDB
Diet
carnivorePBDB, for Thalattosuchia
Life habit
nektonicPBDB, for Thalattosuchia
Motility
actively mobilePBDB, for Thalattosuchia
Environment
marinePBDB, for Thalattosuchia

Time the record covers

At most 3.1 million years on record.

The one occurrence read is dated to somewhere between 152.21 Mya and 149.2 Mya, which is a dating window rather than a span.

Late Jurassic — about 1 of 1 occurrenceLate Jurassic152–152 Mya — about 0.0 occurrences152–152 Mya — about 0.0 occurrences152–152 Mya — about 0.0 occurrences152–152 Mya — about 0.0 occurrences152–152 Mya — about 0.0 occurrences152–152 Mya — about 0.0 occurrences152–151 Mya — about 0.0 occurrences151–151 Mya — about 0.0 occurrences151–151 Mya — about 0.0 occurrences151–151 Mya — about 0.0 occurrences151–151 Mya — about 0.0 occurrences151–151 Mya — about 0.0 occurrences151–151 Mya — about 0.0 occurrences151–150 Mya — about 0.0 occurrences150–150 Mya — about 0.0 occurrences150–150 Mya — about 0.0 occurrences150–150 Mya — about 0.0 occurrences150–150 Mya — about 0.0 occurrences150–150 Mya — about 0.0 occurrences150–150 Mya — about 0.0 occurrences150–150 Mya — about 0.0 occurrences150–149 Mya — about 0.0 occurrences149–149 Mya — about 0.0 occurrences149–149 Mya — about 0.0 occurrences152.71 Mya148.7 Mya

1 occurrence of Torvoneustes carpenteri on record, most of them in the Late Jurassic. 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

Kimmeridge Clay — 51.25°N, 2.16°W

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

Torvoneustes carpenteri and its relatives

Late Jurassic

Where Torvoneustes carpenteri and its relatives were recorded in the Late Jurassic.

Found in the same rock

1 taxon

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

No 3D scan of Torvoneustes carpenteri 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. (Wilkinson et al. 2008)