Arenigian and Llandeilian cherts identified in the Southern Uplands of Scotland by means of conodonts, etc.
- 1 January 1957
- journal article
- Published by Geological Society of London in Transactions of the Edinburgh Geological Society
- Vol. 17 (1) , 60-70
- https://doi.org/10.1144/transed.17.1.60
Abstract
Light-coloured cherts and associated shales in the Southern Uplands of Scotland have yielded Arenigian and Llandeilian conodont faunas largely identical with faunas of these ages in Sweden. Some of the localities are type localities of John Smith's (1907), yet none of his species could be identified with certainty.This publication has 2 references indexed in Scilit:
- Two Ordovician Conodont Faunas found with Zonal GraptolitesGeologiska Föreningen i Stockholm Förhandlingar, 1957
- Conodonts from the lowermost Ordovician strata of South-Central SwedenGeologiska Föreningen i Stockholm Förhandlingar, 1954