Cusacrinus
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
- CactocrininaePBDB
- Diet
- suspension feederPBDB, for Monobathrida
- Life habit
- upper-level epifaunalPBDB, for Monobathrida
- Motility
- stationary, attachedPBDB, for Monobathrida
- Vision
- blindPBDB, for Crinoidea
- Environment
- marinePBDB, for Echinodermata
Time the record covers
At most 16 million years on record.
Every occurrence read is dated to somewhere between 358.86 Mya and 342.9 Mya, and nothing in the dating separates them, so that window is what the record shows rather than a span.
10 occurrences of Cusacrinus 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
10 occurrences- Carboniferous100%
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
4 formations
Loading coastlines…
The named rock units Cusacrinus has been recovered from, largest first. Drawn where the rock is now, not where it formed.
Cusacrinus and its relatives
CarboniferousWhere Cusacrinus and its relatives were recorded in the Carboniferous.
Found in the same rock
136 taxa- Platycrinites4 sites
- Agaricocrinus planoconvexus3 sites
- Ancalocrinus spinobrachiatus3 sites
- Aorocrinus3 sites
- Blairocrinus macurdai3 sites
- Cribanocrinus3 sites
- Cribanocrinus urceolatus3 sites
- Displodocrinus divergens3 sites
- Hypselocrinus3 sites
- Nunnacrinus dalyanus3 sites
- Physetocrinus copei3 sites
- Physetocrinus lobatus3 sites
- Plemnocrinus bullatus3 sites
- Plemnocrinus homalus3 sites
- Steganocrinus pentagonus3 sites
- Actinocrinus tenuidiscus2 sites
- Amphoracrinus rupinus2 sites
- Amphoracrinus viminalis2 sites
- Aorocrinus helice2 sites
- Aorocrinus meyeri2 sites
- Aryballocrinus whitei2 sites
- Blothrocrinus2 sites
- Cyathocrinites lamellosus2 sites
- Cyathocrinites simplex2 sites
The Paleobiology Database records 9 sites for Cusacrinus, 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
4 references- Camerate crinoids from the Nunn Member (Tournaisian, Osagean) of the Lower Mississippian Lake Valley Formation, New Mexico4
- A bootstrap analysis for comparative taphonomy applied to Early Mississippian (Kinderhookian) crinoids from the Wassonville Cycle of Iowa3
- Camerate and disparid crinoids from the late Kinderhookian Meadville Shale, Cuyahoga Formation of Ohio2
- The Stratigraphy of the Kinderhook Series of Iowa1
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. Each entry links to doi.org. Relayed as the Paleobiology Database holds them, not checked against what they resolve to.
Media and terms
Media content2
Picture of Cusacrinus
- Source
- iDigBio
- Credit
- via iDigBio
- Licence
- CC0
- Commercial use
- the licence allows it
3D model
- Source
- Sketchfab
- Credit
- UIPaleoRepository
- Licence
- CC Attribution
- Commercial use
- cannot be read from the licence given — check the record
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 itCactocrininae through timeFormations of the CarboniferousThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. Bowsher 1955