Stratigraphy and conodonts of the Lower Carboniferous of the Shishkat section (southern Tien Shan, Tajikistan)

Author:

Bardasheva Nina P.,Bardashev Igor A.,Weddige Karsten,Ziegler Willi

Publisher

Springer Science and Business Media LLC

Subject

Paleontology

Reference102 articles.

1. Adrichem Boogaert, H. A. van, (1967): Devonian and Lower Carboniferous conodonts of the Cantabrian Mountains. — Leidse Geol. Med.,39: 129–192, 68 text-figs, 9 tables, 6 encls., 3 pls, Leiden.

2. Aristov, V. A., Alekseev, A. S. (1976): Pozdneturneiskie konodonty zonyScaliognathus anchoralis iz vostochnogo Kazahstana. — Dokl. AN SSSR,229 (1): 189–192, 1pl.

3. Austin, R. L., Groessens, E. (1973): The origin and evolution of the Middle Dinantian conodont generaDoliognathus, Dollymae, Scaliognathus and related forms. — Ann. Soc. Geol. Belg.,85: 229–238, 2 text-figs, 1 pl., Brussels.

4. Babkina, L. A.,Shchipanov, S. V. (1989): Sootnoshenie bio-i litostratigraficheskih kompleksov v nizhnekamennougol’nych otlozheniyach raiona s. Shishkat (Yuzhnyi Tyan-Shan). — Zonal’naya stratigrafiya po mikroorganizmam i metody ee razrabotki: 29,30, VNIGRI, Leningrad.

5. Bardashev, I. A. (1982): Lower Devonian conodonts of western part of Zeravshan — Hissar Region and their stratigraphic significance. — Autoref. candidate degree (PhD): 1–25, 1 text-fig., 2 tabs, Dushanbe.

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