Crurithyris urei

Crurithyris urei

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
CrurithyrisPBDB
Diet
suspension feederPBDB, for Ambocoelioidea
Life habit
low-level epifaunalPBDB, for Ambocoelioidea
Motility
stationary, attachedPBDB, for Ambocoelioidea
Vision
blindPBDB, for Rhynchonellata
Environment
marinePBDB, for Lophophorata

Time the record covers

At least 31 million years on record.

The record covers at least 358.86 Mya to 326.9 Mya. No occurrence read is dated outside 372.15 Mya to 323.6 Mya.

Devonian — about 16 of 74 occurrencesDevonianCarboniferous — about 58 of 74 occurrencesCarboniferous373–371 Mya — about 0.7 occurrences371–370 Mya — about 2 occurrences370–368 Mya — about 2 occurrences368–366 Mya — about 2 occurrences366–365 Mya — about 2 occurrences365–363 Mya — about 2 occurrences363–361 Mya — about 2 occurrences361–360 Mya — about 2 occurrences360–358 Mya — about 1 occurrence355–353 Mya — about 0.1 occurrences353–351 Mya — about 0.1 occurrences351–350 Mya — about 0.1 occurrences350–348 Mya — about 0.1 occurrences348–346 Mya — about 0.2 occurrences346–345 Mya — about 0.4 occurrences345–343 Mya — about 0.4 occurrences343–341 Mya — about 0.4 occurrences341–339 Mya — about 0.4 occurrences339–338 Mya — about 0.4 occurrences338–336 Mya — about 0.4 occurrences336–334 Mya — about 14 occurrences334–333 Mya — about 16 occurrences333–331 Mya — about 16 occurrences331–329 Mya — about 7 occurrences328–326 Mya — about 0.3 occurrences326–324 Mya — about 0.5 occurrences324–323 Mya — about 0.2 occurrences358.86 Mya326.9 Mya373 Mya323 Mya

74 occurrences of Crurithyris urei on record, most of them in the Carboniferous. 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

74 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

9 formations

Second Abden Shale — 56.07°N, 3.17°WVelbert — 51.33°N, 7.05°EEtroeungt — 51.33°N, 7.05°EColsterdale Marine Beds — 54.07°N, 1.82°WMyslejovice — 49.27°N, 17.00°EMiddle Limestone Va — 54.30°N, 2.15°WFeltrim — 53.43°N, 6.20°WMonsal Dale Limestone — 53.19°N, 1.75°WBee Low Limestones — 53.35°N, 1.80°W

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The named rock units Crurithyris urei has been recovered from, largest first. Drawn where the rock is now, not where it formed. 11 occurrences have no formation on record, which is common for older literature.

Crurithyris urei and its relatives

Carboniferous

Where Crurithyris urei and its relatives were recorded in the Carboniferous.

Found in the same rock

385 taxa

The Paleobiology Database records 73 sites for Crurithyris urei, 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

8 references

Each of the 74 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 Crurithyris urei

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

No 3D scan of Crurithyris urei was found in Sketchfab.

Smithsonian Open Access and MorphoSource were 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.

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Occurrence data from the Paleobiology Database, CC BY 4.0. (Fleming 1828)