Cyphotrypa sp.
publication ID |
https://doi.org/ 10.11646/zootaxa.5196.2.6 |
publication LSID |
lsid:zoobank.org:pub:45D52870-ADB1-42AA-883D-A1D1D31B5AEF |
DOI |
https://doi.org/10.5281/zenodo.7231816 |
persistent identifier |
https://treatment.plazi.org/id/03CE0E5C-FF91-3A30-16CC-FD66FB0DFAB2 |
treatment provided by |
Plazi |
scientific name |
Cyphotrypa sp. |
status |
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Figs 3A–E View FIGURE 3 , Table 2 View TABLE 2
Material. SibGIU 12/25 (sections).
Description. Massive (?ramose) colony with poorly defined exozone.Autozooecia prismatic, containing straight, slightly curved diaphragms. Distance between diaphragms 0.10–0.42 mm. Autozooecial apertures polygonal, 4 spaced per 1 mm. Exilazooecia rare, small. Acanthostyles abundant, 0.02 mm in diameter, 3–5 surrounding each aperture. Autozooecial walls laminated, merged without visible autozooecial boundaries, 0.04 mm thick in exozone.
Comparison. The present material is similar to C. olgae Tolokonnikova, 2010 from the lower Famennian of Gorny Altay ( Tolokonnikova 2010), but differs in presence of diaphragms in each autozooecial chamber and in larger distance between them (0.10–0.42 mm vs. 0.10–0.27 mm in C. olgae ), smaller exilazooecia (0.03–0.04 mm vs. 0.056 –0.098 mm in C. olgae ) and acanthostyles (0.02 mm vs. 0.042 –0.056 mm in C. olgae ). The present material differs from C. minuscula Volkova, 1974 ( Volkova 1974) from the lower Famennian of Gorny Altay in smaller apertures (0.16–0.24 mm vs. 0.20–0.30 mm in C. minuscula ) and exilazooecia (0.03–0.04 mm vs. 0.10 mm in C. minuscula ), abundant acanthostyles vs. rare ones in C. minuscula . The available material is not sufficient to make a comprehensive comparison.
Stratigraphical and geographical ranges. Ermaksy Formation, lower-middle Famennian (upper Devonian); Karatau, Zhankurgan outcrop, Kazakhstan.
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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