Cladida
Cladida is a major subgroup of crinoids with a complicated taxonomic history. Cladida was originally applied to a wide assortment of extinct crinoids with a dicyclic calyx. Under this original definition, cladids would represent a paraphyletic order ancestral to several other major crinoid groups, particularly the living Articulata. More recently, Cladida has been redefined as a monophyletic parvclass of pentacrinoids which encompasses articulates and the extinct Flexibilia (flexibles). Cladids also include various minor taxa such as the hybocrinids and "cyathocrines". As flexibles were not originally considered cladids, the new subgroup Eucladida has been erected for cladids which are more derived than flexibles. Cladida is the sister group to Disparida, another large group of extinct crinoids.

Dwergenpaartje · CC BY-SA 3.0 · via Wikipedia/Commons. 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
- InadunataPBDB
- Diet
- suspension feederPBDB
- Life habit
- intermediate-level epifaunalPBDB
- Motility
- stationary, attachedPBDB
- Vision
- blindPBDB, for Crinoidea
- Environment
- marinePBDB, for Echinodermata
Time the record covers
At least 476 million years on record.
The record covers at least 477.1 Mya to 129 ka. No occurrence read is dated outside 488.9 Mya to 11.7 ka.
5,659 occurrences of Cladida on record, most of them in the Carboniferous. The Paleobiology Database records this as a living group. 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
5,659 occurrences- Cambrianunder 1%
- Ordovician9%
- Silurian6%
- Devonian7%
- Carboniferous30%
- Permian14%
- Early Triassic1%
- Middle Triassic5%
- Late Triassic5%
- Early Jurassic4%
- Middle Jurassic3%
- Late Jurassic4%
- Early Cretaceous4%
- Late Cretaceous5%
- Paleoceneunder 1%
- Eocene1%
- Oligoceneunder 1%
- Mioceneunder 1%
- Pleistoceneunder 1%
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
661 formations
- Bangor Limestone Formation170
- Stanton Formation · Lansing Group167
- Edwardsville Formation154
- Barnsdall Formation · Lansing Group125
- Fort Payne Formation118
- Bloyd Formation · Morrow Group117
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The named rock units Cladida has been recovered from, largest first. Drawn where the rock is now, not where it formed. 637 further formations hold fewer occurrences each and are not listed. 1,061 occurrences have no formation on record, which is common for older literature.
Cladida and its relatives
CarboniferousWhere Cladida and its relatives were recorded in the Carboniferous.
Found in the same rock
2,337 taxa- Fenestella87 sites
- Platycrinites76 sites
- Fistulipora74 sites
- Echinoidea69 sites
- Cleiothyridina65 sites
- Dichocrinus63 sites
- Eumetria57 sites
- Pentremites53 sites
- Archimedes52 sites
- Tabulipora50 sites
- Barycrinus48 sites
- Cyathocrinites48 sites
- Orthotetes47 sites
- Anthracospirifer leidyi45 sites
- Composita45 sites
- Rhombopora45 sites
- Rhabdomeson44 sites
- Camptocrinus43 sites
- Cornulites42 sites
- Polypora42 sites
- Torynifer42 sites
- Bryozoa41 sites
- Cladochonus41 sites
- Punctospirifer41 sites
The Paleobiology Database records at least 761 sites for Cladida, and this reads 240 of them. Of that, one read hit the database's own return limit, so every count below is a floor rather than a total. 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
760 references- Filtration models, guilds, and biofacies: crinoid paleoecology of the Stanton Formation (Upper Pennsylvanian), Midcontinent, North America286
- Die permischen Krinoiden von Timor195
- Caradocian-Gedinnian echinoderm associations of Central and Eastern North America192
- Upper Mississippi Valley Champlainian and Cincinnatian echinoderms182
- The Paleontology and Paleoecology of the Lower Bangor Limestone (Chesterian, Mississippian)in northwestern Alabama170
- Lower Pennsylvanian (Morrowan) crinoids from Arkansas, Oklahoma, and Texas142
- Crinoid assemblages from the Fort Payne Formation (late Osagean, early Viséan, Mississippian) from Kentucky, Tennessee, and Alabama140
- Community Organization, Paleontology, and Sedimentology of the Lower Mississippian Borden Delta Platform (Edwardsville Formation, Southern Indiana)117
- Stratigraphical and geographical distribution of Mississippian (Lower Carboniferous) Crinoidea from Scotland105
- Paleontology and paleoecology of the Crawfordsville fossil site (Upper Osagian: Indiana)103
- Late Cretaceous-Early Paleocene echinoderms and the K/T boundary in the southeast Netherlands and the northeast Belgium. - part 2: Crinoids91
- The Prati di Stuores/Stuores Wiesen Section (Dolomites, Italy): a candidate Global Stratotype Section and Point for the base of the Carnian stage.84
Each of the 5,659 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. 748 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 Cladida
- Source
- Wikipedia/Commons
- Credit
- Dwergenpaartje
- Licence
- CC BY-SA 3.0
- Commercial use
- the licence allows it
No 3D scan was found. Smithsonian Open Access, MorphoSource and Sketchfab were all searched.
The description on this site
- Source
- Wikipedia, “Cladida”
- Licence
- CC BY-SA 4.0
This is what the site found, which is not the same as what exists.
Keep going
What may have been alongside itInadunata through timeFormations of the CarboniferousThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. (Moore and Laudon 1943)