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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.

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