Heterostraci

Heterostraci (Ancient Greek, ἕτερος+ὄστρακον "those [with] a different shell" [-i is pl. of -us]) is an extinct subclass of pteraspidomorph jawless vertebrate that lived primarily in marine and estuary environments. Heterostraci existed from the mid-Ordovician to the conclusion of the Devonian. The Heterostracans differed from other Paleozoic agnathan taxa both in the arrangement and histology of their scales. Most heterostracans had two plates which form a large dorsal shield and a large ventral shield, and had series of scales arranged in various patterns on the sides of their bodies, the exact pattern differing from one group to another. In a few primitive forms, such as Lepidaspis, the dorsal and ventral shields are composed of a mosaic of tiny scales. In most other known forms, though, these tiny scales have fused together to form the shield-plates. The scales of heterostracans are histologically distinct from other vertebrates, having three layers composed of dentine and aspidine, an acellular bony tissue unique to animals of this class and Thelodonti. The middle layer was honeycombed with tiny spaces called "cancella." As with many agnathan groups, heterostracans had no fins besides the tail or caudal fin. In some pteraspids, especially in the psammosteids, the ends of the branchial plates (the plates that covered the gills) is drawn out to form wing-like extensions. Heterostraci are divided into several orders, including the two most diverse orders, Cyathaspidiformes ("Cup Shields"), and Pteraspidiformes ("Wing Shields"), as well as the Cardipeltida, Corvaspidida, Tolypelepidida, Tesseraspidida, and the Traquairaspidiformes. The predominantly Silurian Tolypelepidida (the best known member being Athenaegis), is regarded as being a sister group of the Cyathaspids and Pteraspidids, while the Early Devonian Lepidaspis is regarded as being incertae sedis, possibly close to the original basal forms. Cyathaspidiformes is divided into two main subgroups: the Amphiaspidida of Early Devonian Siberia (i.e.