About: Dybowskites

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Dybowskites is an extinct genus of bryozoan of the family , found in the Ordovician and Silurian periods. It forms branching, frond-like, or sometimes segmented colonies. In cross-sections of the colonies, the tubular autozooecia are seen growing alongside the branch axis and then bending abruptly to reach the colony surface at a perpendicular angle. There are many mesozooecia and large acanthostyles that protrude from the colony surface.

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  • Dybowskites is an extinct genus of bryozoan of the family , found in the Ordovician and Silurian periods. It forms branching, frond-like, or sometimes segmented colonies. In cross-sections of the colonies, the tubular autozooecia are seen growing alongside the branch axis and then bending abruptly to reach the colony surface at a perpendicular angle. There are many mesozooecia and large acanthostyles that protrude from the colony surface. (en)
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  • 70311848 (xsd:integer)
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  • 1355 (xsd:nonNegativeInteger)
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  • 1077448407 (xsd:integer)
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  • Pushkin 1987 (en)
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  • Ordovician-Silurian (en)
dbp:taxon
  • Dybowskites (en)
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  • Dybowskites is an extinct genus of bryozoan of the family , found in the Ordovician and Silurian periods. It forms branching, frond-like, or sometimes segmented colonies. In cross-sections of the colonies, the tubular autozooecia are seen growing alongside the branch axis and then bending abruptly to reach the colony surface at a perpendicular angle. There are many mesozooecia and large acanthostyles that protrude from the colony surface. (en)
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  • Dybowskites (en)
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