TL;DR: In this paper, a detailed description of new ammonoid specimens from the Lower Muschelkalk (Anisian, Middle Tnassic) of Silesia (southern Poland) is presented.
Abstract: Adescription of new ammonoid specimens (Acrochordiceras aff. damesi,cf . Acrochordiceras sp. indet., DiscopĘchites cf. dux, ?Paraceratites sp., cf. Balatonites sp. indet., Beneckeia buchi) from the Lower Muschelkalk (Anisian, Middle Tnassic) of Silesia (southern Poland) is presented. The detailed stratigraphic position of the new finds is given. The description is supplemented with a list of all species of ammonoids found hitherto in Silesia, which was a southern part of the Germanic Basin during the Anisian. Beneckeia and Noetlingites were typical of epicontinental seas and usually appeared in the early part of fransgressions. Other ammonoids entered from the Tethys into the epicontinental sea of the Germanic Basin during the maxima of fransgressions. Some of them (balatonitids, paraceratitids, bulogitids, Discoptychites and probably Acrochordiceras) were successful colonizers which established their own populations in the Germanic Basin and evolved towards morphologies typical of epicontinental seas. Other (Beyrichites sp., Paraceratites binodosus, and'Trachyceras' sp.) are regarded as unsuccessful immigrants or empĘ shells drifted post-mortem from the Tethys.
TL;DR: The identification of the ammonoid Nevadites merriami Smith (now known as Nevads hyatti (Smith), 1904, in a collection from the Beyrichites "Gynmotoceras"-Parapopanocers faunal zone of the Toad Formation confirms the upper Anisian age originally inferred for this zone by McLearn (1946).
Abstract: The identification of the ammonoid Nevadites merriami Smith (now known to be Nevadites hyatti (Smith), 1904, in a collection from the Beyrichites "Gynmotoceras"-Parapopanoceras faunal zone of the Toad Formation confirms the upper Anisian age originally inferred for this zone by McLearn (1946).
TL;DR: In this article, a Evoluto-spinosus Biozone that includes a Olesites-
Abstract: The Spanish triassic ammonoids have been found almost without exception in the carbonates of the Middle Triassic. The Anisian Ammonites come from the Lower Muschelkalk of Catalonia. The «Paraceratites» are the most frequent forms sueh as oP.» occidentalis y oP.» evoluto-spinosu,s; ali of their macroshelis, and oP.» catalaunicus, oP.» guerini and «1’.» almerai, that are microshelis or young individuals. There are also Olesites (O. villaltab and Beyrichites (B. cognatus,). In general, they have been considered of Middle Anisian age (Pelsonian) but their morphologies and reduced sutures show affinities with the Paraceratitinae of the Trinodosus Zone. In this paper, a Evoluto-spinosus Biozone that includes a Olesites-