MILIOLIDAE - Acta Palaeontologica Polonica
MILIOLIDAE - Acta Palaeontologica Polonica
MILIOLIDAE - Acta Palaeontologica Polonica
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100 EWA LUCZKOWSKA<br />
Remarks. - This species differs from Recent .Sigmoilopsis arenaria<br />
(Brady), in having a thicker wall imd a shorter neck. Reuss claims that<br />
S. foeda is abundant in the Miocene of Wieliczka and this is also true of<br />
our materials from that locality. The illustration of Reuss is not clear<br />
enough and for this reason the topotype is figured in the present paper<br />
(PI. XV, Fig. 5). Sigmoilina plana Smigielska, 1957, from the Miocene of<br />
Gliwice Stare does not differ from the specimens of this species from<br />
Wieliczka. It differs from Sigmoilina abbreviata Vehglinsky, 1967, from<br />
the Burdigalian of the Transcarpathians, in having a much broader test,<br />
more coarse-grained wall, and much shorter, poorly developed neck. From<br />
Sigmoilopsis wanganuiensis Vella, 1957, from the ·Holocene· of New<br />
Zealand it hardly differs at all, but it is difficult to state if it is synonymous<br />
with S. foeda because of the lack comparative materials from<br />
New Zealand. S. foeda is often determined as S. coelata (Costa, 1855), from<br />
the Tertiary of Italia, which species however seems different.<br />
Distribution. - Poland: Tortonian (Gliwice Stare, Grabki Duze, Karsy,<br />
Korytnica, Krywald, Ligota Zabrska, L~ki Dolne, Wieliczka). Austria:<br />
Miocene, M611ersdorf, Vienna Basin. Czechoslovakia: Tortonian, Devinska<br />
Nova Ves, Zidlochovice.<br />
Genus Siphonaperta Vella, 1957<br />
* Siphonaperta granulata (Smigielska, 1957)<br />
(PI. XIV, Figs. 5a, b, 6a, b; Text-fig. 34/2)<br />
1957. Sigmoilina granulata Smigielska; T. Smigielska, p. 260, PI. 16, Fig. 14a, b.<br />
Material. -130 specimens (ColI. No. F-153, Sec. No. 417).<br />
Dimensions: L 0.6-1.1; B 0.4-0.6; T 0.25-0.4.<br />
Description. - Test oval, tapering at both ends, irregular, occasionally<br />
S-shaped, triangular in cross-section, periphery subrounded; chambers<br />
narrow, tubular, the basal end of the last chamber usually protruding and<br />
curved, the apertural end sometimes bent to the back and giving the<br />
chamber its S-shaped appearance, middle chambers large, tubular,<br />
elongated and strongly projecting beyond the surface of the test; sutures<br />
strongly depressed; wall with a number of coarse sand grains in the<br />
surface layer of calcareous cement; surface very rough, studded with sand<br />
particles of different size and shape in a disorderly manner; aperture<br />
circular, at the end of a very short neck, extending beyond the outline of<br />
the test, with an exserted lip and a short narrow or quadrate tooth.<br />
Variability and ontogeny. The test shape varies from oval to S-shaped.<br />
The extension of the chamber is also variable, being very short or lacking<br />
at all. The characteristic features of the species are very prominent<br />
chambers, with deep grooves between them. The internal structure is<br />
irregularly quinqueloculine, the chambers increase considerably in size