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- W2176167611 abstract "1. IntroductionThree species of the genus Frechastraea Scrutton, 1968, namely F. phillipsastraeiformis (Moenke, 1954), F. coeni Coen-Aubert, 2012 and F. glabra Coen-Aubert, 2012, have been described by Coen-Aubert (2012) at the base of the Upper Frasnian from Belgium. In continuation of this paper, six species and one form of Frechastraea are revised herein; these are F. pentagona (Goldfuss, 1826), type species of the genus, F. minima (Rozkowska, 1953), F. micrommata (Roemer, 1852), F. kaisini (Tsien, 1978), F. cf. tungkanlingensis (Yoh, 1937), F. crassiseptata (Tsien, 1978) and F. limitata (Milne-Edwards & Haime, 1851). Most of these occurrences characterize the Upper Palmatolepis rhenana conodont Zone. As mentioned by Coen-Aubert (2012), the base of the Upper Frasnian has been fixed by the Subcommission on Devonian Stratigraphy, at the entry of the conodont Palmatolepis semichatovae. According to Sandberg et al. (1992), the entry of P. semichatovae is observed within the Lower Palmatolepis rhenana Zone, together with the first occurrence of Ancyrognathus triangularis, in bed 150 lying 2.6 m above the base of the Neuville Formation as it is exposed along the southern access road to the Lion quarry at Frasnes, on the south side of the Dinant Synclinorium. Additionally, the massive rugose coral Frechastraea coeni was noted as an excellent marker for the base of the Upper Frasnian in Belgium by Coen-Aubert (2012).During the revision of the geological map of Wallonia, several Pa" @default.
- W2176167611 created "2016-06-24" @default.
- W2176167611 creator A5030804491 @default.
- W2176167611 date "2015-10-19" @default.
- W2176167611 modified "2023-09-26" @default.
- W2176167611 title "Revision of the genus Frechastraea Scrutton, 1968 (Rugosa) in the Upper Frasnian of Belgium" @default.
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