Hostname: page-component-848d4c4894-ttngx Total loading time: 0 Render date: 2024-06-09T13:22:20.750Z Has data issue: false hasContentIssue false
  • English
  • Français

Stromatolites from the Tiout section, Precambrian–Cambrian boundary beds, Anti-Atlas, Morocco

Published online by Cambridge University Press:  01 May 2009

M. Schmitt
M. Schmitt
Affiliation:
Institut für Paläontologie, Universität Würzburg, 8700 Würzburg, Bundes Republik Deutschland
Get access Rights & Permissions [Opens in a new window]

Summary

Stromatolites of the groups Linella, Tungussia and Tifounkeia in association with thrombolites occur in abundance throughout the whole Lie de Vin Series, the middle part of the Adoudounian Group which consists of Calcaire lnférieur, Lie de Vin Series and Calcaire Supérieur. A Late Precambrian age is suggested for these stromatolites.

Type
Articles
Information
Geological Magazine , Volume 115 , Issue 2 , March 1978 , pp. 95 - 100
Copyright
Copyright © Cambridge University Press 1978

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

Bertrand-Sarfati, J. 1972. Stromatolites columnaires du Précambrien Supérieur. Sahara nord-occidental. Editions du Centre National de la Recherche Scientifique. Série Géologie 14, 245 pp.Google Scholar
Krylov, I. N. 1967. Riphean and Lower Cambrian stromatolites of Tien-Shan and Karatau. Trud geol. Inst., Leningr. 171, 76 pp. [In Russian.]Google Scholar
Semikhatov, M. A. 1962. The Riphean and lower Cambrian of the Yenisei Mountains. Trud Geol. Inst. Akad. Nauk S.S.R. 68, 242 pp. [In Russian.]Google Scholar
Walter, M. R. 1972. Stromatolites and the biostratigraphy of the Australian Precambrian and Cambrian. Spec. Pap. Palaentol. 11, 190 pp.Google Scholar