MILIOLIDAE - Acta Palaeontologica Polonica
MILIOLIDAE - Acta Palaeontologica Polonica
MILIOLIDAE - Acta Palaeontologica Polonica
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<strong>MILIOLIDAE</strong> FROM MIOCENE OF POLAND 33<br />
and tooth, not to the internal structure. To be sure, this leads to the<br />
separation of two subgenera of Quinqueloculina (see Part I, p. 351), but<br />
certain species remain in the nondescript group "Quinqueloculina sensu<br />
lato". Prell-Miissig (1965) gives more attention to the internal structure,<br />
but states that it is difficult to tell Quinqueloculina from Triloculina.<br />
Thus, she arrives at the conclusion that the triloculine forms that have<br />
a "quinqueradiate" internal structure (later termed "cryptoquinqueloculine"<br />
by Bogdanowich, 1969; see Part I, p. 353), should be included in<br />
the genus Quinqueloculina. Therefore, reverting partly to Williamson's<br />
conceptions from 1858, she pays no attention to the shape of aperture and<br />
the relations between this shape and the internal structure, and within one<br />
genus combines the forms which might be referred to at least three<br />
genera - Quinqueloculina, Cyclojorina and Sinuloculina - and perhaps<br />
also to Varidentella.<br />
The existence of intergeneric transition forms has also been demonstrated<br />
by Hofker (1971), who used the orthogeny of the species "Miliolina<br />
antiqua" Franke from the Albian of Holland and north-western Germany<br />
as an example. Although his studies concern the development of these<br />
forms with time in the layers about 200 m thick, an analogous phenomenon<br />
can be observed in layers of one and the same age or even in a single<br />
sample. Hofker shows that the species studied, numbered by him in the<br />
genus Quinqueloculina, traced from the lowest layer to the highest one,<br />
passes through the genus Sigmoilina into Spirosigmoilina without any<br />
distinct boundaries between them. In consequence, he disputes the value<br />
of these genera and proposes a unit superior to genus, i.e. the "gens", as<br />
a genuine biological unit. Exemplified by "Miliolina antiqua" the "gens"<br />
develops from a certain form and evolves in a definite direction to become<br />
another form different from the initial one. Hofker illustrates this evolutionary<br />
series with sections of the forms mentioned.<br />
An analysis of Hofker's conception calls in question the genera determined<br />
by him, in which he includes the group of forms examined. In view<br />
of the round toothless aperture, the juvenile stage of quinqueloculine<br />
structure and the sigmoiline adult stage, at least two genera, i.e. Quinqueloculina<br />
and Sigmoilina, may be excluded. Spirosigmoilina has not an<br />
aperture at the end of a neck, either. A close analysis will supposedly<br />
show that they belong to still another genus. This, however, is not essential<br />
to our problem, but the fact that intermediate forms can analogously<br />
be observed in series representing the ontogenetic development in several<br />
species of Quinqueloculina derived from a single sample from the Miocene<br />
layers at Korytnica. They, too, comprise quinqueloculine forms together<br />
with massiline ones, the sections of which show intermediate stages<br />
between them (e.g. Q. anagallis, Text-figs 7, 8; Q. buchiana, Text-figs 12,<br />
13; see section "Ontogeny"); nevertheless, they cannot be treated otherwise<br />
than as developmental stages of one species. We can hardly speak about<br />
3 <strong>Acta</strong> Palaeontologlca nr 1/74