Zieglerodina paucidentata ( Murphy and Matti, 1982 )

Drygant, Daniel & Szaniawski, Hubert, 2012, Lochkovian conodonts from Podolia, Ukraine, and their stratigraphic significance, Acta Palaeontologica Polonica 57 (4), pp. 833-861 : 854-856

Zieglerodina paucidentata ( Murphy and Matti, 1982)

Fig. 11R.

Q. Mazurivka−37B/1, SMNH D1431. R. Khudykivtsi−16/1v, SMNH D1427. L, O, S, T. Transitional forms between Zieglerodina remscheidensis ( Ziegler, 1960) and Z. mashkovae ( Drygant, 1984) . L. Khudykivtsi−16/3, SMNH D 1428. O. Tseliyiv−37/1b, SMNH D 1425. S. Khudykivtsi−16/3, SMNH D 1426. T. Syn'kiv−45/ 190 m, ZPAL C.20/10.19. U. Zieglerodina mashkovae ( Drygant 1984) ; Syn'kiv−45/ 190 m, ZPAL C.20/10.22. V, Y. Pandorinellina ? parva sp. nov. V. Dobrivlyany−11/4, SMNH D1420, holotype. Y. Ivanye Zolote−52/ 525 m, ZPAL C.20/9.5. W, Z, AA. Zieglerodina serrula ( Drygant, 1984) . W. Ivanye Zolote−52/ 525 m, ZPAL C.20/9.2. Z. Zalishchyky−1/1, SMNH D1433. AA. Zalishchyky−2/1v, SMNH D1434. X. Transitional form between Zieglerodina serrula ( Drygant, 1984) and Pandorinellina ? parva sp. nov.; Ivanye Zolote−52/ 525 m, ZPAL C.20/9.16. AB. Wurmiella excavata maxima ( Drygant, 1984) ; Khudykivtsi−16/1v, SMNH D1436. A–D, E 1, F–O, P 1, Q, T–Y, AA, AB lateral view; E 2, P 2, R, S, Z upper view.

http://dx.doi.org/10.4202/app.2011.0124

1975 Ozarkodina sp. nov. E; Klapper and Murphy 1975: 44, pl. 7: 6, 9, 10.

1982 Ozarkodina paucidentata n. sp.; Murphy and Matti 1982: 9, pl. 1: 25–32, 39, 40.

Material.—Three complete Pa elements from upper part of the Ivanye Formation. Section and samples: 52/490 and 510 m.

Remarks.—The specimens from Podolia do not differ significantly from the holotype. They have comparatively small size, high cusp and differentiated height of the blade sections, of which the anterior one is much higher.

Stratigraphic and geographic range.—Pragian? in Podolia. Uppermost Silurian and lower Lochkovian, to the top of Ozarkodina eurekaensis Zone in North America.