Nudonychocella Voigt and Ernst, 1985
publication ID |
https://doi.org/ 10.1080/00222933.2018.1481235 |
publication LSID |
lsid:zoobank.org:pub:63A31AD2-F049-42CB-A45B-557014DC286E |
DOI |
https://doi.org/10.5281/zenodo.4747862 |
persistent identifier |
https://treatment.plazi.org/id/03EB8789-FFC9-4455-A18D-7739FDE8FA09 |
treatment provided by |
Carolina |
scientific name |
Nudonychocella Voigt and Ernst, 1985 |
status |
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Genus Nudonychocella Voigt and Ernst, 1985 View in CoL
( Figure 19 View Figure 19 )
Type species
Nudonychocella nuda Voigt and Ernst, 1985 View in CoL , by original designation. Cretaceous, late Maastrichtian ( Tuffeau de Maastricht ), Maastricht, Netherlands .
Diagnosis
Colony encrusting ( Figure 19 View Figure 19 (a)). Autozooids subhexagonal, rounded distally. Opesia occupying entire frontal surface in post-ancestrular zooids with no preserved cryptocyst or gymnocyst ( Figure 19 View Figure 19 (a,d); in ancestrula, proximal cryptocyst occupying more than half of frontal area ( Figure 19 View Figure 19 (b,c)), opesia terminal, semi-elliptical, proximal edge concave, lacking opesiular indentations and constrictions. Ovicells?immersed, preserved only as small caplike structures ( Figure 19 View Figure 19 (e)). Avicularia vicarious, symmetrical ( Figure 19 View Figure 19 (f)), pointed, without preserved cryptocyst, about half or more of the width of an autozooid.
Remarks
The ancestrula is critical to the placement of this genus in Onychocellidae as it preserves the typically onychocellid, shelf-like cryptocyst ( Figure 19 View Figure 19 (b,c)) that is missing in zooids from later astogeny. A bioimmured example of N. nuda shown by Voigt and Ernst (1985, fig. 2.1) was interpreted by these authors as moulding the unmineralised frontal membrane but is equally likely to have moulded a cryptocystal frontal wall that was lost through leaching, probably because it had a more soluble mineralogy of aragonite or high-Mg calcite ( Taylor and McKinney 2006, p. 104).
Two additional Cretaceous species are suggested as belonging to Nudonychocella . Membranipora subsimplex d’ Orbigny, 1852a , which can be found in the Campanian of SW France ( Figure 19 View Figure 19 (c–f)), resembles the type species in lacking preserved frontal calcification in zooids from late astogeny but retains a cryptocyst in the first budded autozooid ( Figure 19 View Figure 19 (c)) as well as the ancestrula. Aplousina incompta Taylor and McKinney, 2006 , from the Maastrichtian of the south-eastern USA, may perhaps be better placed in Nudonychocella even though avicularia have not been observed and occasional autozooids from the zone of astogenetic repetition preserve remnants of a cryptocyst.
Range
Cretaceous (Campanian to Maastrichtian).
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