MILIOLIDAE - Acta Palaeontologica Polonica
MILIOLIDAE - Acta Palaeontologica Polonica
MILIOLIDAE - Acta Palaeontologica Polonica
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<strong>MILIOLIDAE</strong> FROM MIOCENE OF POLAND 13<br />
did not differ from that presented in 1917. In the next editions (1928,<br />
1933, 1940 and 1948) there are already three families: Miliolidae,<br />
Ophthalmidiidae (including, among other groups, the subfamily Cornuspirininae)<br />
and Fischerinidae. The Miliolidae were not divided into subfamilies,<br />
instead they comprised all d'Orbigny's genera, Wiesner's two<br />
genera (Miliolinella and Biloculinella), Schlumberger's two genera (Massilina<br />
and Sigmoilina), single genera introduced by other authors, e.g.<br />
Nummoloculina Steinmann, Tubinella Rhumbler, Miliola Lamarck, and<br />
several new genera described by Cushman himself: Nubeculina, Ammomassilina<br />
and Flintina.<br />
Cushman initiated a period of keen interest in the genetic classification<br />
of the Foraminifera, which found its reflection in new elaborations appearing<br />
every several years. At first the authors grouped the known miliolid<br />
genera in one family, Miliolidae, after the fashion of earlier writers<br />
(Galloway, 1933), and in three families, after the fashion of Cushman<br />
(Chapman & Parr, 1936). Glaessner (1945) introduced a higher taxonomic<br />
unit, i.e. the super-family Miliolidea divided into four families, with two<br />
of which, the Miliolidae and Ophthalmidiidae, we are concerned. Sigal<br />
(1952) and Pokorny (1958) applied the same division, in which they made<br />
only small changes within the subfamilies. The classification proposed by<br />
Bogdanowich and Voloshinova (in Rauser-Chernousova & Fursenko, 1959)<br />
was characterized by the introduction of a still higher rank, i.e. the order<br />
Miliolida comprising the superfamily Miliolidea and the families Cornuspiridae,<br />
Ophthalmidiidae, Miliolidae and Familiae incertae. In the more<br />
recent classification of Loeblich & Tappan (1964) the taxonomic unit of<br />
the highest rank is the suborder Miliolina, which contains the superfamily<br />
Miliolacea and the families Squamulinidae, Fischerinidae, Nubeculariidae<br />
and Miliolidae. The families except the first one, split into subfamilies,<br />
e.g. the Miliolidae into the Quinqueloculininae, Miliolinellinae, Miliolinae,<br />
Fabulariinae and Tubinellinae, which differ from each other in aperture<br />
type and also, partly, in wall structure.<br />
Critical remarks on the division of the family Miliolidae in Loeblich &<br />
Tappan's classification are given in Part I (1972).<br />
BIOSTRATIGRAPHY<br />
The Miocene sediments from which the Miliolidae under study come<br />
are referred to two stages: the Tortonian (Badenian 2») and Sarmatian.<br />
2) The conception of replacement of the term "Tortonian" with "Badenian" in<br />
\.he Vienna Basin was put forward in the revision of the stratotypes and terms used<br />
so far in the geochronological and lithostratigraphical scale for the Central<br />
Paratethys region, initiated by the Congress of the Committee on Mediterranean<br />
Neogene Stratigraphy in Bologna in 1967 (Papp. et al., 1968). This conception was<br />
upheld by the CMNS Congress in Lyon in 1971 (Carloni et al., 1971) and the term<br />
was recommended for the Central Paratethys region.