Hostname: page-component-cd9895bd7-8ctnn Total loading time: 0 Render date: 2024-12-18T04:39:58.128Z Has data issue: false hasContentIssue false
  • English
  • Français

Cambrian–Ordovician Boundary beds at Tônismägi, Tallinn, North Estonia

Published online by Cambridge University Press:  01 May 2009

D. Kaljo ,
H. Heinsalu ,
K. Mens ,
I. Puura  and
V. Viira
D. Kaljo
Affiliation:
Institute of Geology, Academy of Sciences of the Estonian S.S.R., Estonia pst. 7, Tallinn, 200101, U.S.S.R.
H. Heinsalu
Affiliation:
Institute of Geology, Academy of Sciences of the Estonian S.S.R., Estonia pst. 7, Tallinn, 200101, U.S.S.R.
K. Mens
Affiliation:
Institute of Geology, Academy of Sciences of the Estonian S.S.R., Estonia pst. 7, Tallinn, 200101, U.S.S.R.
I. Puura
Affiliation:
Institute of Geology, Academy of Sciences of the Estonian S.S.R., Estonia pst. 7, Tallinn, 200101, U.S.S.R.
V. Viira
Affiliation:
Institute of Geology, Academy of Sciences of the Estonian S.S.R., Estonia pst. 7, Tallinn, 200101, U.S.S.R.
Get access Rights & Permissions [Opens in a new window]

Abstract

The Cambrian–Ordovician Boundary beds at the Tônismägi section in Tallinn, North Estonia, are represented by siltstones and sandstones with interlayers of clay and kerogenous argillites. In this section, three conodont zones – Cordylodus proavus, C. intermedius and C. rotundatus-angulatus – were established. Graptolites of the Rhabdinopora flabelliforme group were found in the upper part of the C. proavus Zone. This section demonstrates that in suitable facies, species of Rhabdinopora may appear earlier than usually considered.

Type
Articles
Information
Geological Magazine , Volume 125 , Issue 4 , July 1988 , pp. 457 - 463
Copyright
Copyright © Cambridge University Press 1988

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Bagnoli, G., Barnes, C. R. & Stevens, R. K. 1987. Tremadocian conodonts from Broom Point and Green Point, Western Newfoundland. Bollettino delta Società Paleontologica Italiana 25 (2), 145–58.Google Scholar
Kaljo, D., Borovko, N., Heinsalu, H., Khazanovich, K., Mens, K., Popov, L., Sergeyeva, S., Sobolevskaya, R. & Viira, V. 1986. The Cambrian–Ordovician boundary in the Baltic–Ladoga Clint area (North Estonia and Leningrad Region, U.S.S.R.). Proceedings of the Academy of Sciences of the Estonian SSR, Geology 35, 3, 97–108.Google Scholar
Nowlan, G. S. 1985. Late Cambrian and Early Ordovician conodonts from the Franklinian Miogeosyncline, Canadian Arctic Islands. Journal of Palaeontology, 59, 96–122.Google Scholar
Stouge, S., Stouge, B. G. & Albani, R. 1985. Lower Ordovician conodonts from Washington Land, western North Greenland. Bulletin of the Geological Society of Denmark, 33, 261–71.Google Scholar
Tjernvik, T. E. 1958. The Tremadocian Beds at Flagabro in South-Eastern Scania (Sweden). Geologiska Föreningens i Stockholm Förhandlingar 80, 3, 259–76.CrossRefGoogle Scholar