Also known as Leptopleuron holotype site
Where: Scotland, United Kingdom (57.7° N, 3.3° W: paleocoordinates 34.0° N, 0.8° W)
• coordinate stated in text
• small collection-level geographic resolution
When: Lossiemouth Sandstone Formation, Carnian to Carnian (237.0 - 208.5 Ma)
• Age of the Lossiemouth Sandstone Formation is based upon vertebrate biostratigraphy, with comparisons made to the faunal assemblages from the lower part of the Maleri Formation (India), the upper part of the Santa Maria Formation (Brazil) and the Ischigualasto Formation (Argentina). This is suggestive of a late Carnian to early Norian age (Benton & Walker 2011).
• bed-level stratigraphic resolution
Environment/lithology: dune; lithified sandstone
Size class: macrofossils
Preservation: mold/impression
Collected by William Young in 1851; reposited in the BGS
• NMS (also RSM): National Museum of Scotland, Edinburgh
Primary reference: G. A. Mantell. 1852. Description of the Telerpeton elginense and observations on supposed fossil ova of batrachians in the Lower Devonian strata of Forfarshire. Quarterly Journal of the Geological Society of London 8:100-109 [R. Butler/R. Butler]more details
Purpose of describing collection: taxonomic analysis
PaleoDB collection 89011: authorized by Richard Butler, entered by Richard Butler on 28.04.2009
Creative Commons license: CC BY (attribution)
Taxonomic list
Reptilia | |
"Telerpeton elginense n. gen. n. sp." = Leptopleuron lacertinum
"Telerpeton elginense n. gen. n. sp." = Leptopleuron lacertinum Owen 1851 parareptile NMS 1891.92.528 (holotype; also the type of L. lacertinum), articulated skull and skeleton; additional BGS specimen
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