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Superregnum: Eukaryota
Regnum: Animalia
Phylum: Bryozoa
Classis: Stenolaemata
Ordines (1 + †5): †CryptostomidaCyclostomatida – †Cystoporida – †Esthonioporata – †Fenestrida – †Trepostomatida

Stenolaemata Borg, 1926: 490
Primary references

Borg, F. 1926. Studies on Recent Cyclostomatous Bryozoa. Zoologiska bidrag från Uppsala 10: 181–507.

Additional references

Rouse, S., Loxton, J., Jones, M.E.S. & Porter, J.S. 2018. A checklist of marine bryozoan taxa in Scottish sea regions. ZooKeys 787: 135-149. DOI: 10.3897/zookeys.787.24647 Reference page.


Stenolaemata in the World Register of Marine Species

Stenolaemata are a class of exclusively marine bryozoans. Stenolaemates originated and diversified in the Ordovician, and more than 600 species are still alive today.[1] All extant (living) species are in the order Cyclostomatida, the third-largest order of living bryozoans.[2]

These animals are stationary suspension feeders that live on the ocean floor. They formed colonies with robust, calcified exoskeletons, allowing for a high potential for fossil preservation. The individual zooids in the colony may be tubular, conical, or sac-shaped. Each individual, or zooid, may extend from the colony at an angle, extending its tentacles to feed.[1] The fossil genus Batostoma in the order Trepostomatida existed in monticular colonies.

Stenolaemates were the predominant bryozoan group during the Paleozoic, when many extinct orders proliferated within the class.[3] Some grew as lacy or fan-like colonies that became important reef builders, and in some regions form an abundant component of limestones. The extinct Palaeozoic stenolaemate orders are placed in the superorder Palaeostomata.[4] Their numbers were greatly reduced during the terminal Permian extinction event, and most stenolaemates were extinct by the start of the Jurassic.[5]

However, the basal and previously rare stenolaemate order Cyclostomatida diversified in the Jurassic and became the most abundant group of bryozoans in the late Mesozoic. Cyclostomatida is no longer the most speciose bryozoan group, as the order experienced high rates of extinction during the end-Cretaceous mass extinction, while ctenostome and cheilostome bryozoans in the class Gymnolaemata diversified around the same time. Nevertheless, cyclostomates are still major components of modern marine ecosystems.[5]

Extant and extinct orders in this class include:[1][6][5][4]

Cyclostomatida/Cyclostomata (Ordovician-present)
Cryptostomata/Cryptostomida † (Ordovician-Triassic)
Cystoporata/Cystoporida † (Ordovician-Triassic)
Esthonioporata † (Ordovician-Devonian)
Fenestrata/Fenestrida † (Ordovician-Permian)
Timanodictyina † (Devonian-Permian, may be a suborder of Cryptostomata)
Trepostomata/Trepostomatida † (Ordovician-Triassic)

Wikimedia Commons has media related to Stenolaemata.

Stenolaemata. The Digital Atlas of Ordovician Life.
Ramalho, L. V., G. Muricy, and P. D. Taylor. (2009). Cyclostomata (Bryozoa, Stenolaemata) from Rio de Janeiro State, Brazil. Zootaxa 2057 32-52.
Barnes, R. D. (1982). Invertebrate Zoology. Philadelphia, PA: Holt-Saunders International. p. 902. ISBN 0-03-056747-5.
Jun-ye, Ma; Buttler, Caroline J.; Taylor, Paul D. (2014). "Cladistic analysis of the 'trepostome' Suborder Esthonioporina and the systematics of Palaeozoic bryozoans". Studi Trent. Sci. Nat. 94: 153–161.
Taylor, Paul D.; Waeschenbach, Andrea (2015). "Phylogeny and diversification of bryozoans". Palaeontology. 58 (4): 585–599. doi:10.1111/pala.12170. ISSN 1475-4983.
Borg (1926). Bock P (ed.). "Stenolaemata". World list of Bryozoa. World Register of Marine Species. Retrieved 2020-02-10.

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