Also known as Halfway Quarry
Where: Wales, United Kingdom (51.0° N, 3.0° W: paleocoordinates 26.0° S, 11.9° W)
• coordinate estimated from map
• small collection-level geographic resolution
When: Long Quarry Beds Member (Downtonian Formation), Ludfordian to Ludfordian (425.6 - 419.2 Ma)
• Fossils come from siltstone 10 m above the base of the Downtonian Stage and from the spoil heap below this layer. Ages given by Cleal & Thomas, 1995.
• bed-level stratigraphic resolution
Environment/lithology: coastal; gray siltstone
Size classes: macrofossils, microfossils
Preservation: adpression, coalified, original carbon, original sporopollenin
Collection methods: quarrying, surface (in situ), chemical, peel or thin section,
Primary reference: D. Edwards. 1970. Fertile Rhyniophytina from the Lower Devonian of Britain. Palaeontology 13(3):451-461 [P. Gensel/M. Kotyk]more details
Purpose of describing collection: taxonomic analysis
PaleoDB collection 10635: authorized by Pat Gensel, entered by Michele Kotyk on 08.06.2001
Creative Commons license: CC BY (attribution)
Taxonomic list
unclassified | |
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Retusotriletes | |
Psilophytopsida | |
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Rhyniaceae | |
Steganotheca striata n. gen. n. sp.
Steganotheca striata n. gen. n. sp. Edwards 1970 | |
Rhyniopsida | |
cf. Renalia sp.1 Gensel 1976 Described Edwards & Rogerson 1979 as being similar to C. hemisphaerica sensu Ananiev & Stepanov. Left unnamed in this paper.
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