Camerata (crinoid)

For other uses, see Camerata (disambiguation).

The Camerata or camerate crinoids are an extinct subclass of Paleozoic stalked crinoids. They were some of the earliest crinoids to originate during the Early Ordovician, reached their maximum diversity during the Mississippian, and became extinct during the Permian–Triassic extinction event.^[2] Camerates are the sister group of Pentacrinoidea, which contains all other crinoids (including living species). The two largest camerate subgroups are the orders Diplobathrida and Monobathrida.^[3][4]

The platycrinitid Platycrinites hemisphaericus. Early Carboniferous, Muldraugh Formation, Indiana. At the Royal Tyrrell Museum of Palaeontology.

Camerata Temporal range: Middle Ordovician–Late Permian PreꞒ Ꞓ O S D C P T J K Pg N
Rhodocrinus serpens, a sea lily of the family Rhodocrinidae, 16mm measured along the stem fragment and including cup and arms, collected at the Gilmore City Formation, near Gilmore City Iowa, USA, from the Lower Mississippian Carboniferous (Tournaisian)
Scientific classification
Kingdom:	Animalia
Phylum:	Echinodermata
Class:	Crinoidea
Subclass:	†Camerata Wachsmuth and Springer, 1885[1]
Subgroups
See text

Anatomically, they are distinguished by:^[5]

• fused junctions between the plates of the cup
• brachial plates incorporated into the cup
• tegmen forming a rigid roof over the mouth
• no less than ten and sometimes a very large number of free arms, often pinnulate

Subdivisions

• Order Cladida?
• Adelphicrinus
• Eknomocrinus
• Cnemecrinus
• Quechuacrinus
• Reteocrinus
• Eucamerata
  • Rosfacrinus
  • Order Diplobathrida
  • Order Monobathrida