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MILIOLIDAE - Acta Palaeontologica Polonica

MILIOLIDAE - Acta Palaeontologica Polonica

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20 EWA LUCZKOWSKA<br />

equally abundant Varidentella reussi, Cycloforina predcarpatica, Articulina<br />

problema and Articularia articulinoides. As can be seen, the species are<br />

few in number although the number of specimens is large.<br />

The above-mentioned species abound in the northern coastal zone,<br />

e.g. in the region of Tarnobrzeg (Luczkowska, 1964), whereas in the deeper<br />

zone of the Foredeep, where the Sarmatian deposits exceed 1000 m in<br />

thickness, they are met with more rarely. The microfauna found in the<br />

Sarmatian layers of the Foredeep is mostly a redeposited fauna washed<br />

out of the deposits of the Upper or Lower Tortonian and even those of<br />

the Cretaceous.<br />

Zone with Elphidium hauerinum. - This zone, overlying the zone with<br />

Varidentella sarmatica has hardly any miliolids. From among the<br />

Sarmatian species, only dwarfish Varidentella reussi is encountered in it;<br />

however, it may well be that the rare specimens of this species come<br />

from the lower layers that have been washed away. The range of this<br />

zone is not known exactly, supposedly it occurs only locally in the region<br />

of Tarnobrzeg.<br />

PALAEOECOLOGY<br />

The Miliolidae are a foraminiferal group having small requirements in<br />

respect of water salinity, for they may be found in both salt and brackish<br />

waters, but their occurrence is frequently restricted to only certain depths<br />

and temperatures. In the contemporary seas they prevail over inner shelf<br />

and in open gulfs, in warm and shallow tropical and subtropical waters,<br />

at depths from zero to about 100 m (Norton, 1930; Lowman, 1949; Sigal,<br />

1952; Matthes, 1956; Bandy & Arnal, 1960; Loeblich & Tappan, 1964;<br />

Bandy, 1964 b; Boltovskoy, 1965), where they may form 50 per cent or<br />

more of the whole population. They belong chiefly to different species<br />

of Quinqueloculina and Triloculina 3), which are good indicators of conditions<br />

in the vinicity of coasts. These genera are not dominant in the<br />

region of central and outer shelves, but here Biloculinella appears beside<br />

them. In the bathyal zone the miliolids are scarce except Pyrgo and<br />

Pyrgoella, which here develop various groups of species and grow to<br />

a large size (above 5 mm), whereas the shelf forms of Pyrgo do not<br />

usually exceed 1 mm.<br />

Such a pattern of distribution of the Miliolidae is generally noted in<br />

tropical regions and those of warm water all over the world. In the Gulf<br />

of Mexico the Miliolidae are abundant at depths of 30 m (Shifflett, 1961),<br />

70-100 m (the genus Quinqueloculina chiefly in the inner turbulent zone<br />

at 20-30 m; Phleger, 1960), or even down to 150 m (Parker, 1954), and<br />

do not descend below 180-220 m (Phleger & Parker, 1951). In Florida the<br />

3) The generic names are given after the authors cited.

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