America. They are so named (Gr. shell-skins or shell-bearers) in allusion to the nacreous shell-like appearance of the inner face of the plates of armour which cover the more common members of the group. The Ostracoderms are, indeed, known only by the hard armature of the skin, but this sometimes bears impressions of certain internal soft parts which have perished during fossilization. They agree with fishes in the possession of median fins, and resemble the large majority of early fishes in their unequal-lobed (heterocercal) tail, but they have no ordinary paired fins. They must also have been provided with the usual gill-apparatus, but there is reason to believe that their lower jaw was not on the fish plan. They are, therefore, at least as low in the zoological scale as the existing lampreys, with which Cope, Smith, Woodward and others have associated them. They are all small animals, many of them only a few centimetres in length.
From British Museum, Catalogue of Fossil Fishes, by permission of the Trustees.
Fig. 3. — Pteraspis rostrata, from the Lower Old Red Sandstone of Herefordshire, restored by Dr A. S. Woodward; about one-third nat. size.
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Fig. 4.—Pterichthys milleri, from the Middle Old Red Sandstone of Scotland, restored by Dr R. H. Traquair; upper (A), lower (B), and left-side view (C), about one-half nat. size. | |||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
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The oldest and lowest family of Ostracoderms, that of Coelolepidae, is known by nearly complete skeletons of Thelodus (fig. 1) and Lanarkia from the Upper Silurian mud stones of Lanarkshire, Scotland. The Ixjdy is completely and uniformly covered with minute granules which resemble the shagreen of sharks, and were erroneously ascribed to sharks when they were first discovered in the Upper Silurian bone-bed at Ludlow, Shropshire. The head and anterior part of the trunk are depressed and shown from above or below in the fossils, and this region sharply contracts behind into the slender tail, which is generally seen in side view, with one small dorsal fin and a forked heterocercal tail. The eyes are far forwards and wide apart. In another family, that of the Cephalaspidae (fig. 2), the animals resemble the Coelolepids in shape, but their skin granules are fused into small plates, which are polygonal where there must have been much flexibility, and in rings round the tail where the underlying successive plates of muscle necessitated this arrangement. The eyes are close together. At the opening of the gill-cavity on each side at the back of the head, there is a flexible flap, which is sometimes interpreted as a paired limb. Part of the armour of the Cephalaspidians contains bone-cells, but the dermal plates of two other families, the Pteraspidae (fig. 3) and Drepanaspidae, consist merely of fused shagreen granules without any advance towards bone. The Pteraspidae are interesting as showing on the inner side of the dorsal shield impressions which suggest that the gill-cavities extended unusually far forwards to the front of the head. 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. The Asterolepid armour consists of symmetrically arranged, overlapping plates on the top of the head and round the body, with a pair of flippers similarly armoured and appended to the latter. The tail resembles that of other Ostracoderms and is sometimes covered with scales.
See E. Ray Lankester, The Cephalaspidae (Monogr. Palaeont. Soc. 1868, 1870); R. H. Traquair, The Asterolepidae (Monogr. Palaeont. Soc. 1894, 1904, 1906) and papers in Trans. Roy. Soc. Edinb. vol. xxxix. No. 32 (1899), vol. xl. Nos. 30, 33 (1903, 1905); A. S. Woodward, Catal. Foss. Fishes, B.M. pt. ii. (1891); W. H. Gaskell, Origin of Vertebrates (London, 1908). (A. S. Wo.)
OSTRAU, the name of two Austrian towns in the Ostrau-Karwin coal-mining district, (1) Mährisch-Ostrau (Moravian Ostrau), a town in Moravia, 95 m. N.E. of Brünn by rail. Pop. (1900) 30,125. It is situated on the right bank of the Ostrawitza, near its confluence with the Oder, and it derives its importance from the neighbouring coal mines, and the blast furnaces and iron-works which they have called into existence. The manufactures comprise sheet-iron, boilers, zinc, brick and tiles, paraffin, petroleum, soap and candles. The Rothschild iron-works at Witkowitz are in the vicinity. (2) Polnisch-Ostrau (Polish Ostrau), a mining town in Austrian Silesia, opposite Mährisch-Ostrau. Pop. (1900) 18,761, mostly Czech. It has large coal mines, which form the south-western portion of the extensive Upper Silesian coal fields, the largest Austrian deposit.
OSTRICH (O. Eng. estridge; Fr. autruche; Span. avestruz; Lat. avis struthio; Gr. στρουθίων or ὁ μέγας στρουθός); the Struthio camelus of Linnaeus, and the largest of living birds, an adult male standing nearly 8 ft. high and weighing 300 ℔.
The genus Struthio forms the type of the group of Ratite birds, characterized chiefly by large size, breast-bone without a keel, strong running legs, rudimentary wings and simple feathers (see Bird). The most obvious distinctive character presented by the ostrich is the presence of two toes only, the third and fourth, on each foot—a character absolutely peculiar to the genus Struthio. In South America another large Ratite bird, the rhea, is called ostrich; it can be distinguished at once from the true ostrich by its possession of three toes.
