http://dbpedia.org/ontology/abstract
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Dybowskites is an extinct genus of bryozoa … 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.les that protrude from the colony surface.
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http://dbpedia.org/ontology/wikiPageID
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70311848
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http://dbpedia.org/ontology/wikiPageLength
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1355
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http://dbpedia.org/ontology/wikiPageRevisionID
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1077448407
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http://dbpedia.org/ontology/wikiPageWikiLink
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http://dbpedia.org/resource/Category:Prehistoric_bryozoan_genera +
, http://dbpedia.org/resource/Silurian +
, http://dbpedia.org/resource/Ordovician +
, http://dbpedia.org/resource/Ralfimartitidae +
, http://dbpedia.org/resource/Bryozoan +
, http://dbpedia.org/resource/Category:Trepostomata +
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http://dbpedia.org/property/authority
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Pushkin 1987
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http://dbpedia.org/property/fossilRange
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Ordovician-Silurian
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http://dbpedia.org/property/taxon
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Dybowskites
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http://dbpedia.org/resource/Template:Automatic_taxobox +
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, http://dbpedia.org/resource/Template:Specieslist +
, http://dbpedia.org/resource/Template:Taxonbar +
, http://dbpedia.org/resource/Template:Fossilrange +
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http://purl.org/dc/terms/subject
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http://dbpedia.org/resource/Category:Trepostomata +
, http://dbpedia.org/resource/Category:Prehistoric_bryozoan_genera +
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http://www.w3.org/ns/prov#wasDerivedFrom
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http://en.wikipedia.org/wiki/Dybowskites?oldid=1077448407&ns=0 +
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http://xmlns.com/foaf/0.1/isPrimaryTopicOf
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http://en.wikipedia.org/wiki/Dybowskites +
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owl:sameAs |
http://dbpedia.org/resource/Dybowskites +
, https://global.dbpedia.org/id/nfeV +
, http://www.wikidata.org/entity/Q18520368 +
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rdfs:comment |
Dybowskites is an extinct genus of bryozoa … 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.les that protrude from the colony surface.
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rdfs:label |
Dybowskites
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