Some new acanthodian material from the Lower Devonian of Europe

The following material is described: (a) a climatiid shoulder girdle from the Old Red of Podolia and the British Lower Old Red Sandstone, and (b) ischnacanthid jaw-elements and a fin spine from the Lower Devonian of Vestspitsbergen. A discussion is given of the shoulder girdle in Climatius reticulatus and of the characters distinguishing the dentigerous jaw-bones of the Ischnacanthidae from those of the early Climatiidae. It is pointed out that in the dermal skeleton of the Climatiidae one may trace phylotie changes in the structure of mesodentine and bone tissue closely paralleling those of the corresponding hard tissues in the Osteostraei. A trend towards the emergence of acellular bone tissue is traceable not only in the Climatiidae but also in certain parts of the dermal skeleton of the Ischnacanthidae.