Carabocrinus radiatus

Carabocrinus radiatus

via GBIF · CC0 · 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
CarabocrinusPBDB
Diet
suspension feederPBDB, for Cladida
Life habit
intermediate-level epifaunalPBDB, for Cladida
Motility
stationary, attachedPBDB, for Cladida
Vision
blindPBDB, for Crinoidea
Environment
marinePBDB, for Echinodermata

Time the record covers

At least 3.6 million years on record.

The record covers at least 453.8 Mya to 450.2 Mya. No occurrence read is dated outside 457.3 Mya to 445.2 Mya.

Ordovician — about 10 of 10 occurrencesOrdovician457–457 Mya — about 0.3 occurrences457–456 Mya — about 0.3 occurrences456–456 Mya — about 0.3 occurrences456–456 Mya — about 0.3 occurrences456–455 Mya — about 0.3 occurrences455–455 Mya — about 0.3 occurrences455–454 Mya — about 0.3 occurrences454–454 Mya — about 0.3 occurrences454–453 Mya — about 0.2 occurrences453–453 Mya — about 0.2 occurrences453–453 Mya — about 0.2 occurrences453–452 Mya — about 0.3 occurrences452–452 Mya — about 0.3 occurrences452–451 Mya — about 0.3 occurrences451–451 Mya — about 1.0 occurrences451–450 Mya — about 2 occurrences450–450 Mya — about 1 occurrence450–450 Mya — about 0.8 occurrences450–449 Mya — about 0.1 occurrences449–449 Mya — about 0.1 occurrences449–448 Mya — about 0.1 occurrences448–448 Mya — about 0.1 occurrences448–447 Mya — about 0.1 occurrences447–447 Mya — about 0.1 occurrences447–446 Mya — about 0.1 occurrences446–446 Mya — about 0.1 occurrences446–446 Mya — about 0.1 occurrences446–445 Mya — about 0.1 occurrences453.8 Mya450.2 Mya457.8 Mya444.7 Mya

10 occurrences of Carabocrinus radiatus on record, most of them in the Ordovician. 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

10 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

7 formations

Wise Lake — 43.28°N, 91.85°WWise Lake — 42.00°N, 90.50°WDunleith — 42.00°N, 90.50°WProsser Limestone — 44.00°N, 92.00°WStewartville — 44.00°N, 92.00°WOttawa — 45.46°N, 75.68°WHull — 45.41°N, 75.73°WBobcaygeon-Verulam — 44.53°N, 79.15°W

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

Carabocrinus radiatus and its relatives

Ordovician

Where Carabocrinus radiatus and its relatives were recorded in the Ordovician.

Found in the same rock

66 taxa

The Paleobiology Database records 9 sites for Carabocrinus radiatus, 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

5 references

Each of the 10 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 Carabocrinus radiatus

Source
GBIF
Credit
via GBIF
Licence
CC0
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 itCarabocrinus through timeFormations of the OrdovicianThe world it lived on

Occurrence data from the Paleobiology Database, CC BY 4.0. Billings 1857