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MILIOLIDAE - Acta Palaeontologica Polonica

MILIOLIDAE - Acta Palaeontologica Polonica

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16 EWA LUCZKOWSKA<br />

Sigmoilopsis foeda, Pyrgo amphiconica and Pyrgoella ventruosa. In other<br />

regions, e.g. in the Bochnia-Gd6w area and in the Holy-Cross Mts, the<br />

Miliolidae of this zone are still poorer in species and represented only by<br />

small numbers of Cycloforina suturalis and Sigmoilinita tenuis.<br />

Upper Tortonian<br />

Zone with Neobulimina longa. - Between the Lower Tortonian zone<br />

with Uvigerina costai and Upper Tortonian zone with Neobulimina longa<br />

there was a period of formation of chemical deposits, in which no microfauna<br />

developed. Its slow development occurs after this period, but the<br />

Miliolidae do not playa major role yet. The microfaunaI assemblages<br />

of this zone are composed partly of the species existing earlier in the zone<br />

with Uvigerina costai and partly of new species. This is not the case with<br />

the Miliolidae, among which the species known from the Lower Tortonian,<br />

like Quinqueloculina regularis, Sigmoilinita tenuis, Pyrgo inornata and<br />

P. truncata, are still observed.<br />

Zone with Hanzawaia crassiseptata. - It come to a great development<br />

of the Upper Tortonian microfauna in this zone, at which there also appear<br />

a number of new miliolid species. In the coastal region the boundary<br />

between the two zones of the Upper Tortonian is not sharp, there being<br />

transitions between them or a direct succession of a great development<br />

of the benthonic microfauna, comprising new species, after the period of<br />

formation of chemical deposits. The Miliolidae develop more abundantly<br />

than previously and, although the species of the lower zone of the Upper<br />

Tortonian still persist among them, a few species not encountered before<br />

appear as well. The Miliolidae from Gliwice Stare in Upper Silesia make<br />

a typical example. The most characteristic species of this assemblage are:<br />

Quinqueloculina buchiana QS and MS, Q. parakneriana QS and MS,<br />

Q. regularis, Q. pygmaea and Q. spondiungeriana - as relicts of the Lower<br />

Tortonian forms; Cycloforina contorta, C. gracilis, C. lachesis, C. lucida<br />

(a group of related forms, characterized by a rough surface with short<br />

incised lines and a tendency to carinate peripheries of the chambers) and<br />

C. suturata; a group of several species of the genus Hauerina, i.e.<br />

H. aspergilla, H. compressa, H. plana, H. podolica, H. tumida and Pseudohauerina<br />

ornatissima, of which only P. ornatissima and H. tumida were<br />

recorded from lower layers; Sigmoilopsis foeda, Siphonaperta granulata,<br />

S. mediterranensis, Miliolinella selene, M. valvularis, Affinetrina gualtieriana,<br />

A. planciana, Biloculinella labiata, Pyrgo clypeata, P. inornata,<br />

P. lunula, P. truncata, Pyrgoella controversa, P. globiformis, P. ventruosa,<br />

Sinuloculina consobrina, S. microdon, S. nitens, Triloculina angularis,<br />

T. eggeri, Sigmoilinita tenuis and Nummoloculina contraria, out of which<br />

Cycloforina suturata, Siphonaperta granulata, Affinetrina gualtierana,

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