An analogue model of melt segregatsion and accumulation processes in the Eart's crust
Aasta | 2007 |
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Ajakiri | Estonian Journal of Earth Sciences |
Köide | 56 |
Number | 1 |
Leheküljed | 3-10 |
Tüüp | artikkel ajakirjas |
OpenAccess | |
Litsents | CC BY 4.0 |
Eesti autor | |
Keel | inglise |
Id | 13553 |
Abstrakt
More than 150 Ordovician and Early Silurian brachiopod species have been assigned to the genus Platystrophia King, 1850 mainly on the basis of their Spirifer-like shell exteriors. King’s concept of the genus was based on Platystrophia biforata King, which is not conspecific with Terebratulites biforatus Schlotheim, traditionally regarded as the type species of Platystrophia. Porambonites costatus Pander, 1830 is formally proposed as the type species of the genus to replace P. biforata; the latter is considered to be a nomen dubium. In our revised diagnosis, Platystrophia is restricted to a group of Arenig to upper Caradoc species from Baltica and Avalonia, whereas the Ashgill and lower Silurian taxa of these regions, hitherto assigned to Platystrophia, are placed in the new genus Neoplatystrophia. Platystrophia ponderosa Foerste, 1909 from the Upper Ordovician of North America is proposed as the type species of a new genus Vinlandostrophia. Two new species, Platystrophia baltica and Platystrophia pogrebovi from the Llanvirn–Caradoc of the East Baltic are also described.