Timorites schucherti

Timorites schucherti

via iDigBio · CC0 · via iDigBio. May be a photograph of a specimen, or an artist’s reconstruction — an interpretation of a skeleton, since colour and soft tissue are almost never preserved.

On record

Recorded, not inferred
Sits inside
TimoritesPBDB
Diet
carnivorePBDB, for Ammonoidea
Life habit
nektonicPBDB, for Goniatitida
Motility
fast-movingPBDB, for Ammonoidea
Vision
well-developedPBDB, for Cephalopoda
Environment
marinePBDB, for Cephalopoda

Time the record covers

At most 7.1 million years on record.

Every occurrence read is dated to somewhere between 266.9 Mya and 259.857 Mya, and nothing in the dating separates them, so that window is what the record shows rather than a span.

Permian — about 3 of 3 occurrencesPermian267–267 Mya — about 0.0 occurrences267–267 Mya — about 0.1 occurrences267–266 Mya — about 0.1 occurrences266–266 Mya — about 0.1 occurrences266–266 Mya — about 0.1 occurrences266–266 Mya — about 0.1 occurrences266–265 Mya — about 0.1 occurrences265–265 Mya — about 0.1 occurrences265–265 Mya — about 0.1 occurrences265–264 Mya — about 0.1 occurrences264–264 Mya — about 0.1 occurrences264–264 Mya — about 0.1 occurrences264–264 Mya — about 0.1 occurrences264–263 Mya — about 0.1 occurrences263–263 Mya — about 0.1 occurrences263–263 Mya — about 0.1 occurrences263–263 Mya — about 0.1 occurrences263–262 Mya — about 0.1 occurrences262–262 Mya — about 0.1 occurrences262–262 Mya — about 0.1 occurrences262–262 Mya — about 0.1 occurrences262–261 Mya — about 0.1 occurrences261–261 Mya — about 0.1 occurrences261–261 Mya — about 0.1 occurrences261–260 Mya — about 0.1 occurrences260–260 Mya — about 0.1 occurrences260–260 Mya — about 0.1 occurrences260–260 Mya — about 0.0 occurrences267.4 Mya259.4 Mya

3 occurrences of Timorites schucherti on record, most of them in the Permian. 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

3 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

3 formations

La Difunta — 26.38°N, 102.93°WBell Canyon — 31.94°N, 104.76°WLas Delicias — 26.42°N, 102.87°W

Loading coastlines…

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

Timorites schucherti and its relatives

Permian

Where Timorites schucherti and its relatives were recorded in the Permian.

Found in the same rock

29 taxa

The Paleobiology Database records 3 sites for Timorites schucherti, 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

3 references

Each of the 3 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. Entries link to doi.org where the Paleobiology Database holds an identifier, and to its own record where it does not. Relayed as the Paleobiology Database holds them, not checked against what they resolve to.

Media and terms

Media content1

Picture of Timorites schucherti

Source
iDigBio
Credit
via iDigBio
Licence
CC0
Commercial use
the licence allows it

No 3D scan of Timorites schucherti 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 itTimorites through timeFormations of the PermianThe world it lived on

Occurrence data from the Paleobiology Database, CC BY 4.0. Miller and Furnish 1940