Palocyathus seymourensis Filkorn, 1994
publication ID |
11755334 |
DOI |
https://doi.org/10.5281/zenodo.5241470 |
persistent identifier |
https://treatment.plazi.org/id/D24287AB-FF87-8E74-7DFF-77306F1AFBAE |
treatment provided by |
Felipe |
scientific name |
Palocyathus seymourensis Filkorn, 1994 |
status |
|
Palocyathus seymourensis Filkorn, 1994 View in CoL
Pl. 8, fig. 4
v*1994 Palocyathus seymourensis n. sp.: Filkorn, p. 57, figs 19 (1–4).
v1997 Palocyathus seymourensis Filkorn, 1994 : Cairns, p. 18, figs 1k, 4k.
2000 Palocyathus seymourensis, Filkorn 1995 : Löser, p. 58.
v2002 Palocyathus seymourensis Filkorn, 1994 : Baron-Szabo, p. 176, text-fig. 75.
Dimensions. d (min)=4.4–8.2 mm; d (max)=4.4–9.1 mm; d (min)/d (max)=0.85–1; s=48; h=3.2–8.5 mm.
Description. Solitary, turbinate-cuneiform; intercostal regions greater than width of costae and exteriorly pitted; costosepta arranged in 4 complete cycles in 6 systems; pali in front of S3 usually fused to their common S2.
Type location of species. Maastrichtian of Antarctic Peninsula (López de Bertodano Formation, Seymour Island) .
Distribution. Maastrichtian of Antarctic Peninsula.
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.