Fistulipora sakagamii, Ernst, 2016
publication ID |
https://doi.org/ 10.26879/585 |
publication LSID |
lsid:zoobank.org:pub:6F0DE44D-32BD-4882-9C38-FF76446D15EA |
persistent identifier |
https://treatment.plazi.org/id/2F15F14D-FF95-FF9C-0690-AB8EFE2BF9EF |
treatment provided by |
Felipe |
scientific name |
Fistulipora sakagamii |
status |
sp. nov. |
Fistulipora sakagamii View in CoL n. sp.
Figures 3.9-10, 4.1-2 View FIGURE 3 View FIGURE 4 View FIGURE 5 View FIGURE 6 View FIGURE 7 View FIGURE 8 View FIGURE 9 View FIGURE 10 ; Table 3
zoobank.org/ 08AABC94-467F-4885-86D3-8549C9134902
1975 Fistulipora sp. indet. Sakagami, p. 35, pl. 4, figs. 5-6.
Etymology. The species is named in honour of Sumio Sakagami, who has contributed greatly to the research on Palaeozoic bryozoans.
Holotype. SMF 23.028 About SMF .
Paratype. SMF 23.029 About SMF .
Type locality. Zhongba area of southwestern Tibet (E 84.31536, N 29.74233) GoogleMaps .
Type stratum. Zhongba Formation, Permian (upper Cisuralian–Guadalupian).
Diagnosis. Thin encrusting colony; lunaria well-developed, horseshoe-shaped; apertures separated by 1–3 rows of vesicles; 8–10 vesicles surrounding each aperture.
Description. Thin encrusting colony. Autozooecia growing from thin epitheca, bending at their bases to the colony surface. Autozooecial diaphragms rare to absent, thin. Autozooecial apertures circular to oval. Lunaria well-developed, long, horseshoe-shaped; ends of lunaria slightly indenting into autozooecia. Vesicles small to medium, high, separating autozooecia in 1–3 rows, 8–10 surrounding each autozooecia aperture, with rounded to flat roofs, polygonal in tangential section. Autozooecial walls granular prismatic, 0.005 –0.015 mm thick. Maculae not observed.
Remarks. Fistulipora sakagamii n. sp. differs from F. rutogensis Xia, 1991 from the Chainaha Formation (Middle Permian) of southwestern Tibet, in smaller autozooecial apertures (0.14–0.19 mm vs. 0.24–0.30 mm in F. rutogensis ).
Occurrence. Lower Permian (Artinskian); Khao Hin Kling, Thailand. Zhongba Formation, Permian (upper Cisuralian–Guadalupian); Zhongba area of southwestern Tibet.
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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