MIOCENE OOLITE OF SOUTH RUSSIA. 
293 
Shells found at Korinitza in Poland. 
Buccinum semistriatum, Brocchi 
Si- 
Other Localities. 
Vienna, Sub-Apennines. English, crag 
cilian beds. Still living in Mediterranean 
Vienna, Sub-Apennines. 
Sub-Apennines. 
— costulatum, Brocchi 
— serratum, Brocchi, t. 5. f. 4 
Nassa columboides. Bast. t. 2. f. 6 Bordeaux, Vienna. 
Cassis texta. Brown, Dubois, 1. 1. f. 4, 5 Vienna, Volhynia? 
— Italica, Desk. (Bucc. Ital. Brocchi) Sub-Apennines. 
Rostellaria pes-carbonis, Brony. t. 4. f . 2 Vienna, Bordeaux, Volhynia, 
Cancel laria varicosa, Brocchi Vienna, Sub-Apennines. 
uniangulata. Desk. Encycl. Method, p. 181. No. 5. ... Asti. 
— mitrseformis, Andreiofshy, Bull, de Moscou Volhynia. 
Murex spinicosta, Bruy., M. triacanthus, Linn., Pusch, \ y; enna 
1. 11. f. 20 / 
— plicatus, Brocchi 
Triton affinis, Desh 
Ranella marginata, Linn 
Fusus Stutzii, Partsch 
— Zahlbruckneri, Partsch. 
Fasciolaria Polonica, Pusch, t. 12. f. 2 
Pleurotoma tuberculosa. Bast. t. 3. f. 11 
— interrupta, Brocchi 
Pyrnla rusticola, Bast. t. 7. f. 9 
Cerithium aleucoides, Brocchi 
Cytherea multilamella, Lam 
Area diluvii, Lam. 
Sub-Apennines. 
Morea. 
Vienna, Bordeaux. 
Vienna. 
Vienna. 
Vienna. 
Vienna, Bordeaux. 
Sub-Apennines. 
Bordeaux, Vienna. 
Vienna. 
Vienna, Rome. 
Vienna, Bordeaux, Volhynia, Touraine. 
In addition to these thirty-three species, all well known in other parts of Europe, 
one or two forms only of our collection, including a Natica, seem to have been 
undescribed, and the list therefore most clearly establishes, that the tertiary accu- 
mulations of the Upper Vistula, Wieliczka, &c., which range along the northern 
Hanks of the Carpathians, are of miocene age, and perfectly analogous to certain 
deposits of the Sub-Apennines in Italy and the basins of Vienna and Bordeaux. 
Miocene Deposits in Southern Russia . — Strata similar to these just mentioned, 
and containing a similar group of fossils, extend through Volhynia, Podolia, &c., 
where they have been described by MM. Eicliwald, Dubois, and other geologists, 
and have more recently been observed by M. Hommaire de Hell in Bessarabia. 
M. Dubois, however, was the first author who showed, by the publication of his 
work 1 upon the fossil conchology of the plateau of Volhynia and Podolia, accom- 
panied by illustrative plates, that this great mass of shelly deposits was the equi- 
valent of the beds of the Sub-Apennines and of Bordeaux. In sustaining this 
view by the examination of adjacent and similar strata in Poland and along the 
1 Conchiologie Fossile du Plateau Wolhyni-Podolien. Berlin, 1831. 
2 Q 
