Calceocrinidae

Calceocrinus Hall, 1852, a relative of Calceocrinidae — not Calceocrinidae itself

Not Calceocrinidae. This is Calceocrinus Hall, 1852, a relative — both are Calceocrinidae.

Graffham, Allen · 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
CalceocrinidaPBDB
Diet
suspension feederPBDB, for Disparida
Life habit
intermediate-level epifaunalPBDB, for Disparida
Motility
stationary, attachedPBDB, for Disparida
Vision
blindPBDB, for Crinoidea
Environment
marinePBDB, for Echinodermata

Time the record covers

At least 168 million years on record.

The record covers at least 458.2 Mya to 290.1 Mya. No occurrence read is dated outside 471.3 Mya to 283.3 Mya.

Ordovician — about 84 of 248 occurrencesOrdovicianSilurian — about 73 of 248 occurrencesSilurianDevonian — about 29 of 248 occurrencesDevonianCarboniferous — about 60 of 248 occurrencesCarboniferousPermian — about 2 of 248 occurrencesPermian475–469 Mya — about 0.4 occurrences469–462 Mya — about 1.0 occurrences462–456 Mya — about 13 occurrences456–449 Mya — about 59 occurrences449–442 Mya — about 14 occurrences442–436 Mya — about 18 occurrences436–429 Mya — about 24 occurrences429–423 Mya — about 22 occurrences423–416 Mya — about 8 occurrences416–410 Mya — about 7 occurrences410–403 Mya — about 3 occurrences403–397 Mya — about 3 occurrences397–390 Mya — about 2 occurrences390–384 Mya — about 7 occurrences384–377 Mya — about 2 occurrences377–371 Mya — about 0.1 occurrences371–364 Mya — about 0.5 occurrences364–358 Mya — about 0.8 occurrences358–351 Mya — about 5 occurrences351–345 Mya — about 30 occurrences345–338 Mya — about 21 occurrences338–332 Mya — about 0.7 occurrences332–325 Mya — about 0.7 occurrences325–319 Mya — about 2 occurrences293–286 Mya — about 1 occurrence286–280 Mya — about 0.8 occurrences458.2 Mya290.1 Mya475 Mya280 Mya

248 occurrences of Calceocrinidae 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

248 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

67 formations

Fort Payne — 36.93°N, 84.97°WFort Payne — 36.71°N, 85.48°WFort Payne — 36.95°N, 85.01°WFort Payne — 36.75°N, 85.15°WFort Payne — 36.78°N, 85.10°WFort Payne — 36.72°N, 85.36°WFort Payne — 36.54°N, 85.13°WFort Payne — 36.96°N, 85.07°WDunleith — 37.07°N, 89.57°WDunleith — 42.00°N, 90.50°WDunleith — 43.49°N, 91.87°WEdwardsville — 39.75°N, 86.67°WEdwardsville — 39.25°N, 86.33°WEdwardsville — 39.00°N, 86.33°WEdwardsville — 39.04°N, 86.50°WRochester Shale — 43.15°N, 77.62°WRochester Shale — 43.10°N, 79.06°WRochester Shale — 43.20°N, 78.45°WRochester Shale — 43.18°N, 78.69°WRochester Shale — 43.15°N, 79.04°WFort Payne Chert — 36.92°N, 84.96°WFort Payne Chert — 36.95°N, 84.98°WFort Payne Chert — 36.86°N, 85.13°WFort Payne Chert — 36.71°N, 85.37°WBromide — 34.00°N, 97.00°WBromide — 34.03°N, 97.17°WBromide — 34.10°N, 97.18°WHenryhouse — 35.08°N, 98.24°WHenryhouse — 34.73°N, 96.63°WHenryhouse — 34.37°N, 97.00°WBobcaygeon — 44.56°N, 78.98°WBobcaygeon — 44.53°N, 78.55°WBobcaygeon — 44.58°N, 79.09°WProsser Limestone — 44.00°N, 92.00°WBrassfield — 39.34°N, 85.48°WBrassfield — 39.80°N, 82.98°WBrassfield — 39.73°N, 84.26°WBrassfield — 39.81°N, 83.98°WPlatteville — 44.98°N, 93.27°WPlatteville — 44.00°N, 92.00°WWayne — 36.08°N, 87.00°WWayne — 35.38°N, 88.00°WWayne — 38.08°N, 87.02°WBorden — 38.08°N, 85.71°WBorden — 36.44°N, 88.06°WBorden — 37.70°N, 85.87°WBorden — 37.96°N, 83.69°WBecscie — 49.82°N, 64.35°WBecscie — 49.42°N, 62.25°WWaldron Shale — 39.45°N, 85.67°WSilica — 41.72°N, 83.72°WSilica — 41.12°N, 84.85°WWise Lake — 43.28°N, 91.85°WWise Lake — 42.00°N, 90.50°WDecorah Shale — 44.98°N, 93.27°WDecorah Shale — 44.00°N, 92.00°WGrand Detour — 42.00°N, 90.50°WGrand Detour — 41.87°N, 89.45°WQuimbys Mill — 42.00°N, 90.50°WIon — 42.00°N, 90.50°WRochester — 43.17°N, 79.03°WBainbridge Limestone — 38.22°N, 90.67°WBainbridge Limestone — 37.80°N, 90.05°WLochkov — 50.03°N, 14.33°ELochkov — 49.98°N, 14.18°E

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The named rock units Calceocrinidae has been recovered from, largest first. Drawn where the rock is now, not where it formed. 43 further formations hold fewer occurrences each and are not listed. 23 occurrences have no formation on record, which is common for older literature.

Calceocrinidae and its relatives

Ordovician

Where Calceocrinidae and its relatives were recorded in the Ordovician.

Found in the same rock

1,703 taxa

The Paleobiology Database records 171 sites for Calceocrinidae, 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

57 references

Each of the 248 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. 45 further references are not listed. 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 Calceocrinus Hall, 1852

Source
GBIF
Credit
Graffham, Allen
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

Occurrence data from the Paleobiology Database, CC BY 4.0. Meek and Worthen 1869