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NARROW
GeoRef Subject
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Pentland Hills
Addenda to the record of machaeridian shell plates in the Wether Law Linn Formation (Late Llandovery), Pentland Hills, Scotland
Notes on the brachiopod species from the Silurian of the Pentland Hills described by Lamont (1978)
Revision of Plumulites ruskini Lamont, and new data from the Silurian of the Pentland Hills, Scotland
Upper Llandovery–Wenlock (Silurian) palynology of the Pentland Hills inliers, Midland Valley of Scotland
Clarkson, E. N. K., Harper, D. A. T., Taylor, C. M. & Anderson, L. I. (eds) 2007. Silurian Fossils of the Pentland Hills, Scotland. Palaeontological Association Field Guides to Fossils no. 11. 218 pp.: London: The Palaeontological Association. Price £15.00 (paperback). ISBN 9781 4051 7715 3; ISSN 0031-0239.
Kiaeropterus (Eurypterida; Stylonurina) recognized from the Silurian of the Pentland Hills
An Upper Llandovery Konservat–Lagerstätte in a depositional context: the Pentland Hills Eurypterid Bed, Midlothian
Silurian cephalopods from the Pentland Hills
Ordovician limestone clasts in the Lower Old Red Sandstone, Pentland Hills, southern Midland Valley Terrane
Gala-Tarannon beds in the Pentland hills, near Edinburgh [Scotland]
Pentland Hills on Map Y (left) courtesy of National Museum of Wales, and (r...
( a ) Location of Pentland Hills (inset right). ( b ) Geological sketch map...
Geological map of the North Esk Inlier, Pentland Hills.
Geological map of the Bavelaw Castle and Loganlee inliers, Pentland Hills.
Amphispongia oblonga Salter, topotypes, Llandovery of the Pentland Hills, ...
Nautiloid cephalopods from the Pentland Hills, Scotland, (a) Geisonoceras...
A field guide to the Silurian Echinodermata of the British Isles: Part 2 – Crinoidea, minor groups and discussion
Abstract Conodont-bearing limestone clasts in Lower Old Red Sandstone conglomerates in the Lanark and Strathmore basins and the Pentland Hills Inlier, Midland Valley, Scotland, indicate a source in a cryptic arc terrane with a mid-Ordovician (P. serra – P. anserinus Biozone) limestone cover. Simpson coefficients of similarity indicate that the faunas from the limestone clasts are closer to conodont faunas from the Holy Cross Mountains, Poland, and the Wrae Limestone in the Northern Belt of the Southern Uplands, than to those in coeval strata from the Laurentian margin including Girvan. Conodont colour alteration index values indicate separate thermal histories for the limestone clasts and coeval strata in the Girvan Inlier. The cryptic arc was located to north of the Northern Belt of the Southern Uplands during Ashgill time and to south of the Midland Valley in Late Silurian–Early Devonian time and clearly had a complex tectonic history.