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Although the fossil record of biramous arthropods commences in the Lower Cambrian, unequivocal uniramous arthropods do not appear until the Upper Silurian, in association with terrestrial biotas. Here we report an Upper Cambrian marine arthropod from East Siberia that possesses some significant myriapodan features. The new arthropod,Xanthomyria spinosa n. gen., n. sp., closely resembles examples of...
Cambrian bivalves from the Middle East are reported here for the first time. They come from early “Middle Cambrian” and latest “Early Cambrian” limestones of the lower Çal Tepe Formation at the type locality (near Seydişehir, western Taurides). The majority of the new findings consists of Pojetaia runnegari Jell, 1980, but a few specimens of Fordilla sp. represent the first report of this genus from...
A new stylophoran (Ceratocystis prosthiakida sp. nov.) from the early Middle Cambrian of the Franconian Forest (north-east Bavaria, Germany) is described with the aid of computed tomography, a powerful means of visualizing fossil anatomy. Investigation in this manner enabled previously inaccessible, buried parts of the fossil to be imaged and studied. In addition, a procedure for digitally correcting...
A replacement name, Irakimaspis nom. nov., is proposed for the mid-Cambrian redlichiide trilobite Turkestanella Repina, 1975. The name was preoccupied by the tentaculite Turkestanella Klishevich, 1969 (Dacrioconarida).
A trace fossil associated with its assumed in situ maker, a holaspid specimen of the trilobite Agraulos ceticephalus (Barrande in Notice préliminaire sur le Systême Silurien et les trilobites de Bohême, Leipzig, 1846), is reported from the middle Cambrian Buchava Formation (Drumian Stage) of the Skryje-Týřovice Basin, Czech Republic. The ichnofossil is preserved on the surface of a mudstone, behind...
The core of borehole 1209/78 west of Doberlug–Kirchhain and south of Herzberg in the Torgau–Doberlug Syncline records an atypical lower part of the Tröbitz Formation with thin limestone horizons. These limestone layers include the remains of a low to moderately diverse fauna with the trilobites Protolenus (Hupeolenus) bergstroemi n. sp., Cambrunicornia saxonica n. sp., Ornamentaspis? aff. todraensis...
The Moroccan Atlas ranges provide sections that help reconstruct the earliest evolution of Paradoxides s.l. A fine-scale analysis of the basal part of the Jbel Wawrmast Formation in the eastern Anti-Atlas and comparisons with other sections in southern Morocco not only shows the abrupt appearance of Acadoparadoxides in nearly monofacial successions, but also illustrates a rapid diversification of...
The Moroccan Atlas ranges provide sections which not only permit fine-scale biostratigraphic analysis of the basal part of the Middle Cambrian by means of typical West Gondwanan faunal elements, but also include exotic trilobites well known from other Cambrian continents or at least extremely rare in West Gondwana. Such trilobites often permit intercontinental correlation that significantly improves...
Earliest middle Cambrian rocks in the Franconian Forest, formerly known as the ‘Galgenberg Formation’, include a moderately diverse fauna with a characteristic West Gondwanan, Atlas-type trilobite assemblage with often surprisingly well-preserved specimens. The hitherto inadequately characterised and poorly described assemblage includes Kingaspidoides frankenwaldensis, K. sp. aff. usitata, K. alberti...
Hyoliths are usually preserved as isolated skeletal elements consisting of conch, operculum, and helens. The occurrence of a conch associated with an operculum is ordinarily exceptional, and the co-occurrence of helens with other skeletal parts is a great rarity. The extraordinary finds of hyolithid conchs associated with opercula in situ are relatively abundant in the Cambrian and Ordovician clastic...
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