Arthur Smith Woodward,
1911 Encyclopædia Britannica, Volume 20…
(1911)
“ Another family, known only by nearly complete skeletons from the Upper Silurian mud stones of Lanarkshire, is that of the Birkeniidae, comprising small fusiform species which are covered with granules disposed in curiously-arranged rows. The highest Ostracoderms are the Asterolepidae, which occur only in Devonian rocks and include the familiar Pterichthys (fig. 4) from the Middle Old Red Sandstone of Scotland. In this family the primitive skin-tubercles seem to have fused, not into polygonal plates, but along the lines of the slime-canals. ”
