Fig. 324: Ostrea gregaria. Fig. 325: Nerinæa Goodhallii. In Fig. 323 of a _Thamnastræa_ from this formation, it will be seen that the cup-shaped cavities are deepest on the right-hand side, and that they grow more and more shallow, until those on the left side are nearly filled up. The last-mentioned stars are supposed to represent a perfected condition, and the others an immature state. These coralline strata extend through the calcareous hills of the north-west of Berkshire, and north of Wilts, and again recur in Yorkshire, near Scarborough. The _ Ostrea gregarea_ (Fig. 324) is very characteristic of the formation in England and on the Continent. One of the limestones of the Jura, referred to the age of the English Coral Rag, has been called “Nerinæan limestone” (Calcaire à Nérinées) by M. Thirria; _Nerinæa_ being an extinct genus of univalve shells (Fig. 325) much resembling the _Cerithium_ in external form. The section shows the curious and continuous ridges on the columnella and whorls. Oxford Clay.—The coralline limestone, or “Coral Rag,” above described, and the accompanying sandy beds, called “calcareous grits,” of the Middle Oolite, rest on a thick bed of clay, called the “Oxford Clay,” sometimes not less than 600 feet thick. In this there are no corals, but great abundance of cephalopoda, of the genera Ammonite and Belemnite (Figs. 326 and 327). In some of the finely laminated clays ammonites are very perfect, although somewhat compressed, and are frequently found with the lateral lobe extended on each side of the opening of the mouth into a horn-like projection (Figure 327). These were discovered in the cuttings of the Great Western Railway, near Chippenham, in 1841, and have been described by Mr. Pratt (_An. Nat. Hist.,_ Nov., 1841). Fig. 326: Belemnites hastatus. Fig. 327: Ammonites Jason. Similar elongated processes have been also observed to extend from the shells of some Belemnites discovered by Dr. Mantell in the same clay (see Figure 328), who, by the aid of this and other specimens, has been able to throw much light on the structure of singular extinct forms of cuttle-fish.[3] Kelloway Rock.—The arenaceous limestone which passes under this name is generally grouped as a member of the Oxford clay, in which it forms, in the south-west of England, lenticular masses, 8 or 10 feet thick, containing at Kelloway, in Wiltshire, numerous casts of ammonites and other shells. But in Yorkshire this calcareo-arenaceous formation thickens to about 30 feet, and constitutes the lower part of the Middle Oolite, extending inland from Scarborough in a southerly direction. The number of mollusca which it contains is, according to Mr. Etheridge, 143, of which only 34, or 23½ per cent, are common to the Oxford clay proper. Of the 52 Cephalopoda, 15 (namely 13 species of ammonite, the _Ancyloceras Calloviense_ and one Belemnite) are common to the Oxford Clay, giving a proportion of nearly 30 per cent. Fig. 328: Belemnites Puzosianus.