MILIOLIDAE - Acta Palaeontologica Polonica
MILIOLIDAE - Acta Palaeontologica Polonica
MILIOLIDAE - Acta Palaeontologica Polonica
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<strong>MILIOLIDAE</strong> FROM MIOCENE OF POLAND 31<br />
(e.g. Serova, 1955, PI. 9, Figs 13-15). It follows that, excepting the genus<br />
Quinqueloculina, the juvenile stage of other genera has no differentiated<br />
diagnostic characters.<br />
4) Within the genus Sinuloculina there are species whose juvenile stage<br />
differs so much from the adult stage that these two stages are often<br />
identified as separate species (e.g. in Sinuloculina microdon, Part 1 1<br />
Textfig.<br />
10).<br />
As regards the aperture and tooth, their shape in the juvenile stage<br />
may differ from that in the adult stage, which can be exemplified by the<br />
genus Varidentella. In V. sarmatica and V. reussi there occur adult specimens<br />
which have a toothless aperture, but removing their external chambers<br />
successively, one can find that in the juvenile stage the aperture is<br />
furnished with a well-developed broad tape-shaped tooth. Hauerina and<br />
Miliola have two types of the aperture and tooth; in the juvenile stage<br />
the aperture is round with a simple tooth, as in Siphonaperta or Cycloforina,<br />
whereas in the adult stage of both genera a cribrate plate develops<br />
and covers both the aperture and the tooth. (e.g. Miliola fabularoides,<br />
PI. XIV, Figs 1-3). This fact has also been stated by Serova (1953 and<br />
1960).<br />
RELATED FORMS<br />
It has been found that groups of such forms that their affinity is<br />
visible both in the similar structure of the juvenile stage and in some<br />
morphological characters in the adult stage and also in the similar nature<br />
of the walls can be distinguished in the Miliolidae from the Miocene of<br />
Poland. As early as 1912 Wiesner paid attention to the existence of<br />
different types of walls in the contemporary Miliolidae and tried to utilize'<br />
this fact in classification (see the section "History of Studies on the Miliolidae").<br />
The group mentioned in the preceding section and composed of Cycloforina<br />
contorta, C. lachesis, C. lucida and C. gracilis, which occur together<br />
in the deposits of the Upper Tortonian at Gliwice Stare, is conspicuous<br />
among the Miocene forms under study. As has been mentioned, this group<br />
is characterized by a similar juvenile stage, consisting of identical tubular<br />
chambers, whereas the adult stage shows a character developing from<br />
species to species, namely, the edges along the chambers. The initial form is<br />
completely void of edges and has tubular chambers in both juvenile and<br />
adult stages - C. gracilis. The next link, Cycloforina lucida, is less regular<br />
and more elongate, with signs of flattenings in the periphery of chambers.<br />
This feature develops further through the forms with two rounded edges<br />
belonging to C. contorta and typical forms of this species with sharp edges,<br />
to the last form of this row, C. lachesis, with a single keel, split only in<br />
the lower portion of the chambers.