Arkell.1956.Jurassic..

196 THE BALKAN PENINSULA
(Renz, 1910, p. 599). The outcrops occur especially in the Ionian Isles of
Corfu, Leucas, Cephalonia and Ithaca, and on the adjoining mainland
of Epirus and Acarnania (fig. 21). (For comprehensive summaries see
Renz, 1909, 1910, 1913; for Epirus 1913, 1925a, 1927; for Acarnania,
19116, 1925; for Cephalonia, 19136; for Kalamos, 1932a; for Leucas,
1905a, 1911a, 1936; for Ithaca, 1911; for Corfu, 1906, 1910, 1926.)
FIG. 21.—Sketch-map of the Ionian Isles, Hellas and Albania, showing the distribution
of facies-types in the Toarcian and Lower Bajocian. After Renz, 1927.
TITHONIAN AND KIMERIDGIAN
Under Cretaceous Rudistid limestones, Eocene limestones and flysch,
is a thick series of flaggy limestones and shales with chert, the Viglaes
Beds, called after Viglaes Mountain on Corfu. They may embrace most
of the Upper Jurassic and part of the Lower Cretaceous, but all the fossils
hitherto recorded are Tithonian and Kimeridgian. The only common
macroscopic fossils are aptychi: A. lamellosus (Park.), A. punctatus (Voltz),
A. beyrichi Oppel, A. latus (Park.), A. laevis Meyer, A. obliquus Quenst.
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