Kettnerites kosoviensis ŽEBERA, 1935

Tonarová, Petra & Introduction, 2008, Revision Of Kettnerites Žebera, 1935 (Scolecodonta, Silurian Of The Barrandian Area, Czech Republic): Preliminary Results, Acta Musei Nationalis Pragae Series B 64 (2 - 4), pp. 185-192 : 188

publication ID

https://doi.org/ 10.5281/zenodo.13182923

persistent identifier

https://treatment.plazi.org/id/C26E87D2-FFC8-9B70-2F3C-FC2E0EEB0805

treatment provided by

Felipe

scientific name

Kettnerites kosoviensis ŽEBERA, 1935
status

 

Species Kettnerites kosoviensis ŽEBERA, 1935

Pl. 1, figs 1-11

1935? Ebetallites ancoraeformis ŽEBERA , p. 9, pl. II, fig. 10

1935 Arabellites perneri ŽEBERA , p. 3, pl. 1, figs. 1, 2

1935 Arabellites innaequidens ŽEBERA , p. 5, pl. I, fig. 3

1935 Arabellites kettneri ŽEBERA , p. 6, pl. I, fig. 4

1935 Arabellites angustidens ŽEBERA , p. 6, pl. I, fig. 5

1935 Pronereites naviculiformis ŽEBERA , p. 7, pl. II, fig. 6

1935 Kettnerites kosoviensis ŽEBERA , p. 8, pl. II, fig. 7

1935 Kettnerites depressus ŽEBERA , p. 8, pl. II, fig. 8

1966 Paulinites kosoviensis (ŽEBERA) ; Kielan-Jaworowska, p. 124, 125

1967 Kettnerites kosoviensis ŽEBERA ; Taugourdeau, p. 471, pl. XV, figs. 11-13, pl. XVI, figs. 4, 12

1970 Paulinites kosoviensis (ŽEBERA) ; Szaniawski, p. 466

1972 Kettnerites kosoviensis ŽEBERA ; Taugourdeau, p. 240, tab. 1

1989 Kettnerites kosoviensis ŽEBERA ; Bergman, p. 49

H o l o t y p e: pl. 2, fig. 7 in Žebera (1935) – the specimen was not found

L o c u s t y p i c u s: Kosov, quarry “pod Koledníkem“

S t r a t u m t y p i c u m: “Budňany Limestone” after original designation of Žebera (1935) = in actual terminology: Požáry Formation, Přídolí, Silurian

H o l o t y p e: ( Žebera 1935, p. 95, translation of Czech and French version)

From a carinate basis (with an elliptical cross profile) extends a massive solid hook-like denticle followed by smaller ones. The denticles’ length is about ¼ of the hook and they are conical, unpointed and usually sloping posteriorly. The inner margin – denticulated – is separated by a shallow depression from the posterior part of the base. At one third of the posterior part of the outer margin is a mould representing a transition to a spur. A more distinct spur is a typical character of MII of the genus Arabellites . Length 1.8 mm.

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