Ehrhardina Martha and Taylor, 2016
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.4747841 |
persistent identifier |
https://treatment.plazi.org/id/03EB8789-FFF9-4465-A181-7100FD9AFA9A |
treatment provided by |
Carolina |
scientific name |
Ehrhardina Martha and Taylor, 2016 |
status |
|
Genus Ehrhardina Martha and Taylor, 2016 View in CoL
( Figure 8 View Figure 8 )
Type species
Ehrhardina voigti Martha and Taylor, 2016 View in CoL , by original designation. Cretaceous, early Cenomanian, Devon, England, United Kingdom .
Diagnosis
Colony encrusting, multilamellar; pore chambers present. Autozooids subhexagonal; zooidal boundaries raised with a medial groove ( Figure 8 View Figure 8 (a,b)). Cryptocyst extensive, granular. Gymnocyst lacking. Opesia terminal, occupying about one-third to half of the frontal surface; semicircular with moderate to deep opesiular indentations. Ovicells hyperstomial, ooecium gymnocystal with a median suture ( Figure 8 View Figure 8 (c)). Avicularia interzooidal, symmetrical, small ( Figure 8 View Figure 8 (b)), less than half the size of an autozooid; opesia longitudinally elliptical; rostrum spatulate, floor smooth.
Remarks
Martha and Taylor (2016) introduced this genus for two new early Cenomanian species, the type species, E. voigti , from Devon in the United Kingdom, and E. pikeae Martha and Taylor, 2016 , from North-Rhine Westphalia in Germany. Key features of the type species are the gymnocystal ooecium which contrasts with the cryptocyst-like ooecia seen in most other onychocellid genera that have non-immersed ovicells. Having an exteriorwalled ooecium can be interpreted as a primitive condition, possibly inherited from an ancestral form resembling Wilbertopora Cheetham, 1954 (see Ostrovsky 2013). Intact ovicells have not been seen in E. pikeae but autozooidal morphology is very similar to the type species. The avicularia in E. pikeae , however, are larger and have folds of gymnocyst over their opesiae.
Range
Cretaceous (early Cenomanian).
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