Abstract
The integument of living lophophorates, which here includes all temporary and permanent covers secreted by a bounding “outer epithelium”, has not been studied in a comprehensively systematic way. Despite the cosmopolitan, if modest, distribution of all three lophophorate phyla, the secretory processes giving rise to their integuments are known for no more than a score or so species of Brachiopoda and Bryozoa (or Ectoprocta) and can only be inferred for the Phoronida. Indeed, the mineral parts of the exoskeletons of extinct brachio-pods and bryozoans have probably been more widely studied than those of living species. Yet all known fossilized integuments can be interpreted in terms of present-day secretory regimes which are, therefore, assumed to have operated in much the same way since the emergence of both phyla in early Phanerozoic times. This assumption underlies any observation made on the shell structure of fossil brachiopods and bryozoans. It does not hold for the phoronids which occur sporadically in post-Silurian rocks only as trace fossils.
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© 1984 Springer-Verlag Berlin Heidelberg
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Williams, A. (1984). Lophophorates. In: Bereiter-Hahn, J., Matoltsy, A.G., Richards, K.S. (eds) Biology of the Integument. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-51593-4_39
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DOI: https://doi.org/10.1007/978-3-642-51593-4_39
Publisher Name: Springer, Berlin, Heidelberg
Print ISBN: 978-3-642-51595-8
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