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Phylactolaemata
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Phylactolaemata

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Phylactolaemata is a class of the phylum Bryozoa whose members live only in freshwater environments. Like all bryozoans, they filter feed by means of an extensible "crown" of ciliated tentacles called a lophophore, and like nearly all bryozoans (the only known exception being Monobryozoon), they live in colonies, each of which consists of clones of the founding member. Unlike those of some marine bryozoans, phylactolaemate colonies consist of only one type of zooid, the feeding forms known as autozooids. These are supported by an unmineralized "exoskeleton" made of gelatinous material or prote

Wikidata facts

Instance of
monotypic taxon
Parent taxon
Bryozoa
Image
Freshwater Bryozoan234.JPG
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Commons category
Phylactolaemata
taxon name
Phylactolaemata
taxon rank
class
topic's main category
Category:Phylactolaemata
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Phylactolaemata
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Encyclopedic overview

3 sections
Contents
  • Fossil record
  • Biology
  • References

Phylactolaemata is a class of the phylum Bryozoa whose members live only in freshwater environments. Like all bryozoans, they filter feed by means of an extensible "crown" of ciliated tentacles called a lophophore, and like nearly all bryozoans (the only known exception being Monobryozoon), they live in colonies, each of which consists of clones of the founding member. Unlike those of some marine bryozoans, phylactolaemate colonies consist of only one type of zooid, the feeding forms known as autozooids. These are supported by an unmineralized "exoskeleton" made of gelatinous material or protein, secreted by the zooids. The class contains only one extant order, Plumatellida.

==Fossil record== Phylactolaemata is regarded to have been the earliest group of bryozoans to evolve. However, because they did not have calcified skeletons, these early bryozoans would have had very low potential to fossilize. Fossils of phylactolaemate statoblasts, which consist of protective chitinous shells that serve as protection for dormant masses of cells holding the potential to grow new colonies, have been found rarely, dating back to the Permian. It is possible that the absence of statoblasts in earlier rocks is because statoblasts evolved as an adaptation for surviving in freshwater, and earlier phylactolaemates were marine.

Excerpted from Wikipedia’s “Phylactolaemata” article, available under the CC BY-SA 4.0 licence.