Nicholsonella Ulrich, 1890
publication ID |
https://doi.org/ 10.5252/geodiversitas2022v44a20 |
publication LSID |
urn:lsid:zoobank.org:pub:5EC74771-0B7B-494D-ADC8-79BECD097A3A |
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https://doi.org/10.5281/zenodo.6723126 |
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https://treatment.plazi.org/id/865C87FD-FFB7-FFF5-39B0-FE824A69FC20 |
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Nicholsonella Ulrich, 1890 |
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Genus Nicholsonella Ulrich, 1890 View in CoL
TYPE SPECIES. — Nicholsonella ponderosa Ulrich, 1890 View in CoL by original designation,Trentonian, Sandbian, Upper Ordovician, North America.
DIAGNOSIS. — Encrusting, frondose, ramose, less commonly massive colonies. Apertures rounded and irregularly petaloid. Walls structureless, very thin, irregularly thickened in different part of colonies. Diaphragms usually abundant in whole colony, more rarely – only in the exozone. Mesozooecia abundant, containing frequent diaphragms, sometimes beaded, irregularly closed by calcitic material on the colony surface. Acanthostyles usually small, abundant, short, restricted to the outermost exozone.
OCCURRENCE. — Lower Ordovician to Lower Silurian of North America and Siberia.
COMPARISON
Nicholsonella Ulrich, 1890 and some other genera (e.g. Dianulites ) are unique among trepostome bryozoans by their re-crystallized walls which suggest a diagenetically unstable aragonitic ( McKinney 1971) or high Mg calcite composition ( Taylor & Wilson 1999).
No known copyright restrictions apply. See Agosti, D., Egloff, W., 2009. Taxonomic information exchange and copyright: the Plazi approach. BMC Research Notes 2009, 2:53 for further explanation.
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