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By S M. Gasiorowski
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Extra resources for Aptychi from the Dogger, Malm and Neocomian in the Western Carpathians and their stratigraphical value
Typ. Trauth, L. ) em. Trauth f. typ. Trauth, Ł. ) em. Trauth var. ), Punctaptychus punctatus (Voltz) f. typ. Trauth, and probably also P. cinctus Trauth. It seems that Trauth (1938, p. c. Taf. X. Fig, 13), and Blaschke's specimen (1911, Taf. I, Fig. 5; Aptychus moravicus). ) em. Trauth, while the former specimen evidently belongs to this „species". ) em. Trauth var. moravica (Trauth)". The assemblage of Aptychi from the Stramberg Limestone at Stramberg represents Subhorizon VI 2o . Silesian Series According to Hohenegger (1861, p.
50. tra Mts. According to Andrusov (1959, II, p. 208) in the red Radioisria limestones of the High Tatric Series in the Velka Fatra Mts. occurs Lamellaptychus sparsilamellosus. If the determination is correct, this Aptychus most probably represents Horizon IV. Lower Subtatric Series, Tatra Mts. According to Rabowski & Goetel (1925, stratigraphieal table) in the nodular limestones of the Malm of the Lower Subtatric Series occurs Aptychus sparsilamellosus. ), then it derives most probably from Horizon IV.
Trauth, forms without concentrical furrows Laevaptychus (Hoplisuslaevaptychus) cf. hoplisus Spath . . ) cf. ) Laevaptychus (Tenuibrevislaevaptychus) cf. tenuibrevis Trauth . ) em. Trauth f. typ. Trauth r „sp. l ex gr. ) em. Trauth /. typ. ) em. Trauth var. ) . . ) em. Trauth var. ) . . ) f. typ. ) var. clasmopleura Trauth . . ) var. " l aff. " 2 aff. kachhensis Trauth . ), forms without concentrical furrows . . ), forms with concentrical furrows r 4* 52 APTYCHI HORIZON V latus (Park,), forms without coneentrical furrows .