Tarphycerids of the suborder Barrandeocerina are striking owing to the large size of the shell and similarity with the recent <i>Allonautilus</i> Ward & Saunders, 1997. They are widely distributed in the Silurian rocks of Europe. They were originally classified within the genus <i>Nautilus</i> Linnaeus, 1758 but generic assignment remained questionable despite the detailed description and excellent illustration provided by Barrande in 1865. Species belonging to this group have been assigned to the genera <i>Barrandeoceras</i> Hyatt, 1884, <i>Heracloceras</i> Teichert, 1940, or <i>Cumingsoceras</i> Flower, 1950 but none of them is appropriate considering their morphology, phylogenetic trends and stratigraphic range. Therefore, a new genus <i>Boionautilus</i> is established here. An evolutionary trend is discerned, expressed especially in the tighter coiling of the shell - a transition from an evolute shell (gyroceracone at the beginning of the second whorl) with subelliptic cross section, to a slightly involute shell with a subtrapezoidal cross section. The dorsoventral diameter of the whorl increased more rapidly, and septa became more densely spaced. <i>Boionautilus tyrannus</i> (Barrande, 1865) is now known to occur in North Africa (Algeria, the Ougarta Range). Previously-mentioned finds in peri-Gondwanan sediments of the Carnic Alps are here rejected. Differences in the colour of septa and connecting rings in one exceptionally well-preserved specimen of this taxon from Algeria and one Bohemian specimen of <i>B. sternbergi</i> (Barrande, 1865) are remarkable and indicate high primary content of organic matter within the connecting rings