Leislingites quadratus

No picture of Leislingites quadratus was found. Wikipedia, Wikidata, iDigBio and Smithsonian Open Access were searched and had none. GBIF was asked, and what came back is not recorded: nothing, or a picture this site could not tie to Leislingites quadratus, or no answer at all. This entry cannot say which.

On record

Recorded, not inferred
Sits inside
LeislingitesPBDB
Diet
carnivorePBDB, for Ceratitida
Life habit
nektonicPBDB, for Ceratitida
Motility
actively mobilePBDB, for Ceratitida
Vision
well-developedPBDB, for Cephalopoda
Environment
marinePBDB, for Cephalopoda

Time the record covers

At most 4.2 million years on record.

Every occurrence read is dated to somewhere between 215.38 Mya and 211.18 Mya, and nothing in the dating separates them, so that window is what the record shows rather than a span.

Late Triassic — about 6 of 6 occurrencesLate Triassic216–215 Mya — about 0.0 occurrences215–215 Mya — about 0.2 occurrences215–215 Mya — about 0.2 occurrences215–215 Mya — about 0.2 occurrences215–215 Mya — about 0.2 occurrences215–214 Mya — about 0.2 occurrences214–214 Mya — about 0.2 occurrences214–214 Mya — about 0.2 occurrences214–214 Mya — about 0.2 occurrences214–214 Mya — about 0.2 occurrences214–214 Mya — about 0.2 occurrences214–213 Mya — about 0.2 occurrences213–213 Mya — about 0.2 occurrences213–213 Mya — about 0.2 occurrences213–213 Mya — about 0.2 occurrences213–213 Mya — about 0.2 occurrences213–213 Mya — about 0.2 occurrences213–212 Mya — about 0.2 occurrences212–212 Mya — about 0.2 occurrences212–212 Mya — about 0.2 occurrences212–212 Mya — about 0.2 occurrences212–212 Mya — about 0.2 occurrences212–212 Mya — about 0.2 occurrences212–211 Mya — about 0.2 occurrences211–211 Mya — about 0.2 occurrences211–211 Mya — about 0.0 occurrences215.9 Mya210.7 Mya

6 occurrences of Leislingites quadratus 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

6 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

Pardonet — 56.47°N, 123.68°WPardonet — 57.10°N, 123.28°WPardonet — 56.08°N, 123.04°W

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

Leislingites quadratus and its relatives

Late Triassic

Where Leislingites quadratus and its relatives were recorded in the Late Triassic.

Found in the same rock

10 taxa

The Paleobiology Database records 6 sites for Leislingites quadratus, 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 6 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 doi.org. Relayed as the Paleobiology Database holds them, not checked against what they resolve to.

Media and terms

Media content0

No picture of Leislingites quadratus was found. Wikipedia, Wikidata, iDigBio and Smithsonian Open Access were searched and had none.

GBIF was asked, and what came back is not recorded: nothing, or a picture this site could not tie to Leislingites quadratus, or no answer at all. This entry cannot say which.

No 3D scan was found. Smithsonian Open Access, MorphoSource and Sketchfab were all searched.

This is what the site found, which is not the same as what exists.

Keep going

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

Occurrence data from the Paleobiology Database, CC BY 4.0. Tozer 1994