Late Visean brachiopods from the eastern Tafilalt (Morocco), and more precisely from the area comprised between the Jebel Begaa to the southwest, and Gara El Itima to the northeast (close to the Algerian border), are described systematically for the first time. Despite the limited material available, 18 species belonging to 17 genera have been recognized within the limestone beds of the Merdani and Zrigat formations, in which the productides (Productidina) and spiriferides are the most diverse. Representatives of the subfamily Gigantoproductidinae, which are close, if not conspecific, to those present in contemporaneous rocks of the nearby Bechar Basin (Algeria), occur in the late Visean Zrigat Formation. Additional research based on more a...
The genus Dzieduszyckia is especially well represented and diverse in the Famennian strata of the Mi...
The Carboniferous sediments of the thrust structures between the Porma and Bernesga rivers (map 2) a...
The Kangal Phyllite-Slate Formation forms the basement rocks in Kangal-Cetinkaya-Alacahan-Divrigi (S...
A small-sized brachiopod fauna, representing an orthid, rhynchonellid and spiriferid community which...
Abstract: Based on previous systematic studies of productid, rhynchonellid and spiriferid bra-chiopo...
The Early Carboniferous Erdbach limestones I, II, and III, deposited in crevasses (karst, tectonics)...
Here we describe a Guadalupian brachiopod fauna from units III to V of the shallow water carbonate s...
Here we describe a Guadalupian brachiopod fauna from units III to V of the shallow water carbonate s...
Here we describe a Guadalupian brachiopod fauna from units III to V of the shallow water carbonate s...
New data on systematics, biostratigraphy and biogeography are presented in this paper. They concern ...
The northern flank of the Tindouf Syncline in southern Morocco exhibits a continuous, well exposed C...
A new early Visean coral assemblage has been recorded from turbidite facies in the southern part of ...
Potential foraminiferal markers for the Visean-Serpukhovian and Serpukhovian-Bashkirian boundaries- ...
The revision of Lower and Middle Devonian moroccan chonetacean brachiopods allows to recognize twent...
Carboniferous rocks from North Karakorum display sharp lateral variations in lithology and thickness...
The genus Dzieduszyckia is especially well represented and diverse in the Famennian strata of the Mi...
The Carboniferous sediments of the thrust structures between the Porma and Bernesga rivers (map 2) a...
The Kangal Phyllite-Slate Formation forms the basement rocks in Kangal-Cetinkaya-Alacahan-Divrigi (S...
A small-sized brachiopod fauna, representing an orthid, rhynchonellid and spiriferid community which...
Abstract: Based on previous systematic studies of productid, rhynchonellid and spiriferid bra-chiopo...
The Early Carboniferous Erdbach limestones I, II, and III, deposited in crevasses (karst, tectonics)...
Here we describe a Guadalupian brachiopod fauna from units III to V of the shallow water carbonate s...
Here we describe a Guadalupian brachiopod fauna from units III to V of the shallow water carbonate s...
Here we describe a Guadalupian brachiopod fauna from units III to V of the shallow water carbonate s...
New data on systematics, biostratigraphy and biogeography are presented in this paper. They concern ...
The northern flank of the Tindouf Syncline in southern Morocco exhibits a continuous, well exposed C...
A new early Visean coral assemblage has been recorded from turbidite facies in the southern part of ...
Potential foraminiferal markers for the Visean-Serpukhovian and Serpukhovian-Bashkirian boundaries- ...
The revision of Lower and Middle Devonian moroccan chonetacean brachiopods allows to recognize twent...
Carboniferous rocks from North Karakorum display sharp lateral variations in lithology and thickness...
The genus Dzieduszyckia is especially well represented and diverse in the Famennian strata of the Mi...
The Carboniferous sediments of the thrust structures between the Porma and Bernesga rivers (map 2) a...
The Kangal Phyllite-Slate Formation forms the basement rocks in Kangal-Cetinkaya-Alacahan-Divrigi (S...