Colonial Rugosa from the Early Devonian (Pragian) of the Zeravshan Range, Tajikistan

Schröder, Stefan

doi:10.1080/03115510701305124

Cited by 2 publications

(1 citation statement)

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“…Discussion. -The genus Cyathopaedium -together with Stylopleura, Fletcheria, Maikottia and Pycnostylus are based on morphologically simple species displaying calinical buddings, short undifferenciated septa confined to the wall, widely-spaced tabullae and no dissepimentarium (Pedder 1976, Schröder 2007. Their very simple morphology makes them similar and without a revision of these forms (including habitus), synonymy can not be discarded.…”

Section: Cyathopaedium Paucitabulatum (Schlüter 1880)mentioning

confidence: 99%

The Kačák event (late Eifelian, Middle Devonian) on the Belgian shelf and its effects on rugose coral palaeobiodiversity

Jamart¹,

Denayer²

2020

Bull. Geosci.

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During the Devonian period, major continents/blocks were located in the southern hemisphere (e.g. Stampfli et al. 2002, 2013; Scotese 2014), with a major mountain range running on the northeastern margin of Laurussia to Gondwana: the Appalachian range (Fig. 1) (DeSantis 2010, Scotese 2014). This period of time is marked by one of the most significant modifications in palaeobiogeography with the precipitated end of the strong faunal endemism of the Emsian-Eifelian and the initiation of the Givetian-Frasnian cosmopolitanism (Oliver & Pedder 1979b). During the early Emsian to late Eifelian interval, three distinct faunal assemblages allow the definition of three different marine realms (Oliver & Pedder 1979a, 1979b, 1994; May 1995, 1997b), separated by various barriers. The Malvinokaffric Realm (MKR), located along the margins of Gondwana (Fig. 1), is relatively poor in corals and it is characterized by cold-water species (Oliver 1990;

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Section: Cyathopaedium Paucitabulatum (Schlüter 1880)mentioning

confidence: 99%