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Trepostomatida ( anglais )

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Trepostome bryozoan with bioerosion; Bellevue Formation, Upper Ordovician (Katian), northern Kentucky.

Trepostomatida (the trepostomates) is an extinct order of bryozoans in the class Stenolaemata. Trepostome bryozoans possessed mineralized calcitic skeletons and are frequently fossilized; some of the largest known fossilized bryozoan colonies are branching trepostomes and massive dome-shaped trepostomes. [3] Trepostomes did not have many specialized zooecia beyond ordinary feeding autozooecia. The two main known heteromorphs are exilazooecia and mesozooecia, which had the purpose of maintaining regular spacing between autozooecia. [4]

See also

References

  1. ^ Redescription of type specimens of bryozoan Stigmatella from the Upper Ordovician of the Toronto region, Ontario (1973). By Fritz, Madeleine A., 1896, Royal Ontario Museum
  2. ^ New Monticuliporidae (Bryozoa, Trepostomata) from the Cystoid Limestone Formation (Upper Ordovician) of the Iberian Chains (NE Spain). Jimenez-Sanchez Andrea, Geodiversitas, 2010, vol. 32, no2, pages 177-199, INIST:22896890
  3. ^ Ernst, Andrej (2020). "2- Fossil record and evolution of Bryozoa". Phylum Bryozoa. pp. 11–56.
  4. ^ Ernst, Andrej (2020). "2- Fossil record and evolution of Bryozoa". Phylum Bryozoa. p. 19.

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Trepostomatida: Brief Summary ( anglais )

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Trepostome bryozoan with bioerosion; Bellevue Formation, Upper Ordovician (Katian), northern Kentucky.

Trepostomatida (the trepostomates) is an extinct order of bryozoans in the class Stenolaemata. Trepostome bryozoans possessed mineralized calcitic skeletons and are frequently fossilized; some of the largest known fossilized bryozoan colonies are branching trepostomes and massive dome-shaped trepostomes. Trepostomes did not have many specialized zooecia beyond ordinary feeding autozooecia. The two main known heteromorphs are exilazooecia and mesozooecia, which had the purpose of maintaining regular spacing between autozooecia.

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Trepostomata ( portugais )

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 src=
Ordoviciano Trepostomata.

Trepostomata é uma ordem de briozoários extintos no Permiano, que compreende cerca de 100 gêneros.

Classificação

  • Ordem Trepostomata Ulrich, 1882
    • Família Aisenvergiidae Dunaeva, 1964
    • Família Amplexoporidae Miller 1889
    • Família Anisotrypidae Dunaeva e Morozova, 1967
    • Família Araxoporidae Morozova, 1970
    • Família Astralochomidae Ross, 1988
    • Família Atactotoechidae Duncan, 1939
    • Família Batostomellidae Miller, 1889
    • Família Bimuroporidae Key, 1990
    • Família Crustoporidae Dunaeva e Morozova, 1967
    • Família Cycloporidae Ulrich, 1890
    • Família Dianulitidae Vinassa de Regny, 1921
    • Família Diplotrypidae Vinassa de Regny, 1921
    • Família Dittoporidae Vinassa de Regny, 1921
    • Família Dyscritellidae Dunaeva e Morozova, 1967
    • Família Eridotrypellidae Morozova, 1960
    • Família Esthonioporidae Vinassa de Regny, 1921
    • Família Girtyporidae Morozova, 1966
    • Família Halloporidae Bassler, 1911
    • Família Helenoporidae Ross, 1988
    • Família Hemieridotrypidae Pushkin, 1973
    • Família Heterotrypidae Ulrich, 1890
    • Família Leioclemidae
    • Família Maychellinidae Goryunova, 1985
    • Família Mesotrypidae Astrova, 1965
    • Família Mishulgellidae Gorjunova, 2001
    • Família Monticuliporidae Nicholson, 1881
    • Família Nipponostenoporidae Xia, 1987
    • Família Orbiporidae Astrova, 1978
    • Família Pseudocampylidae Xia, 1997
    • Família Ralfimartitidae Gorjunova, 2005
    • Família Revalotrypidae Goryunova, 1986
    • Família Stenoporellidae Kiseleva, 1982
    • Família Stenoporidae Waagen & Wenzel, 1886
    • Família Stereotoechidae Yang, Hu e Xia, 1988
    • Família Trematoporidae Miller, 1889
    • Família Ulrichotrypellidae Romantchuk, 1967
    • Família Zozariellidae Zágoršek, 1993

Referências

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Trepostomata: Brief Summary ( portugais )

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 src= Ordoviciano Trepostomata.

Trepostomata é uma ordem de briozoários extintos no Permiano, que compreende cerca de 100 gêneros.

licence
cc-by-sa-3.0
droit d’auteur
Autores e editores de Wikipedia
original
visiter la source
site partenaire
wikipedia PT