Cruralina
Collector(s): unknown · 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
- CricosiinaePBDB
- Diet
- suspension feederPBDB, for Cancellothyrididae
- Life habit
- low-level epifaunalPBDB, for Cancellothyrididae
- Motility
- stationary, attachedPBDB, for Cancellothyrididae
- Vision
- blindPBDB, for Rhynchonellata
- Environment
- marinePBDB, for Lophophorata
Time the record covers
At least 74 million years on record.
The record covers at least 157.9 Mya to 83.6 Mya. No occurrence read is dated outside 159 Mya to 66 Mya.
8 occurrences of Cruralina on record, most of them in the Early 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
8 occurrencesThese 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
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The named rock units Cruralina has been recovered from, largest first. Drawn where the rock is now, not where it formed. 5 occurrences have no formation on record, which is common for older literature.
Cruralina and its relatives
Early CretaceousWhere Cruralina and its relatives were recorded in the Early Cretaceous.
Found in the same rock
62 taxa- Argovithyris2 sites
- Dictyothyropsis2 sites
- Porifera2 sites
- Advenina oweni1 site
- Capillithyris1 site
- Cidaris1 site
- Cladocoropsis mirabilis1 site
- Cryptocoenia nivernensis1 site
- Dimorpharaea1 site
- Dimorphastrea concentrica1 site
- Dimorphastrea heteromorpha1 site
- Dimorphofungia aubouini1 site
- Duvalia lata1 site
- Echinoidea1 site
- Etallonasteria minima1 site
- Exogyra1 site
- Fortunella1 site
- Fortunella fortunae1 site
- Fungiastraea1 site
- Haplaraea elegans1 site
- Hemicrinus1 site
- Holaster1 site
- Ismenia pectunculoides1 site
- Lacunosella (Lacunosella) arolica1 site
The Paleobiology Database records 8 sites for Cruralina, 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
7 references- Les Terebratulidés de l'Oxfordien du Jura et de la bordure sud du Bassin de Paris2
- Lower Cretaceous brachiopods from Provence, France, and their biostratigraphical distribution1
- Braquiopodos del Hauteriviense de Fortuna (Prov. Murcia, Espana)1
- Tertiary and Cretaceous Brachiopods from Cuba and the Caribbean1
- Cancellothyridacea (Brachiopoda) from the Lower Cretaceous of Stramberk (Czechoslovakia)1
- L'unite de Miamou (Crete-Grece) et sa macrofaune d'age Jurassique superieur (Brachiopodes, Madreporaires) [The Miamou Unit (Crete, Greece) and its Upper Jurassic macrofauna (brachiopods, corals)]1
- Fossil and recent Cancellothyridacea (Brachiopoda)1
Each of the 8 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 Cruralina
- Source
- GBIF
- Credit
- Collector(s): unknown
- 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 itCricosiinae through timeFormations of the Early CretaceousThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. Smirnova 1966