Austinocrinus

Austinocrinus

via GBIF · CC BY 4.0 · via GBIF. 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
IsselicrininaePBDB
Diet
suspension feederPBDB, for Isselicrinidae
Life habit
upper-level epifaunalPBDB, for Isselicrinidae
Motility
stationary, attachedPBDB, for Isselicrinidae
Vision
blindPBDB, for Crinoidea
Environment
marinePBDB, for Echinodermata

Time the record covers

At least 11 million years on record.

The record covers at least 83.6 Mya to 72.2 Mya. No occurrence read is dated outside 100.5 Mya to 66 Mya.

Early Cretaceous — about 0 of 7 occurrencesLate Cretaceous — about 7 of 7 occurrencesLate CretaceousPaleocene — about 0 of 7 occurrences101–100 Mya — about 0.0 occurrences100–99 Mya — about 0.0 occurrences99–98 Mya — about 0.0 occurrences98–96 Mya — about 0.0 occurrences96–95 Mya — about 0.0 occurrences95–94 Mya — about 0.0 occurrences94–93 Mya — about 0.0 occurrences93–92 Mya — about 0.0 occurrences92–90 Mya — about 0.0 occurrences90–89 Mya — about 0.0 occurrences89–88 Mya — about 0.0 occurrences88–87 Mya — about 0.0 occurrences87–86 Mya — about 0.1 occurrences86–84 Mya — about 0.6 occurrences84–83 Mya — about 0.6 occurrences83–82 Mya — about 0.5 occurrences82–81 Mya — about 0.5 occurrences81–80 Mya — about 0.5 occurrences80–78 Mya — about 0.5 occurrences78–77 Mya — about 0.5 occurrences77–76 Mya — about 0.5 occurrences76–75 Mya — about 0.5 occurrences75–74 Mya — about 0.5 occurrences74–72 Mya — about 0.5 occurrences72–71 Mya — about 0.3 occurrences71–70 Mya — about 0.2 occurrences70–69 Mya — about 0.2 occurrences69–68 Mya — about 0.2 occurrences68–67 Mya — about 0.2 occurrences67–65 Mya — about 0.1 occurrences83.6 Mya72.2 Mya101.2 Mya65.3 Mya

7 occurrences of Austinocrinus on record, most of them in the Late Cretaceous. 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

7 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

White Chalk — 54.52°N, 13.63°EMendez — 22.50°N, 98.46°WPattenau — 47.83°N, 12.69°E

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The named rock units Austinocrinus has been recovered from, largest first. Drawn where the rock is now, not where it formed. 4 occurrences have no formation on record, which is common for older literature.

Austinocrinus and its relatives

Late Cretaceous

Where Austinocrinus and its relatives were recorded in the Late Cretaceous.

Found in the same rock

251 taxa

The Paleobiology Database records 5 sites for Austinocrinus, 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

6 references

Each of the 7 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 Austinocrinus

Source
GBIF
Credit
via GBIF
Licence
CC BY 4.0
Commercial use
the licence allows it

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 itIsselicrininae through timeFormations of the Late CretaceousThe world it lived on

Occurrence data from the Paleobiology Database, CC BY 4.0. Loriol 1889