The last whorls of some of the compressed spiral Foraminifera of the Porcellanous order so nearly encompass all their predecessors, that the transition from a flat spiral to the Orbitolite with its flat disk of concentric rings is not so abrupt as might at first appear. The gradual change may be distinctly traced in the species of the genus Orbiculina. The exteriors of the shells of the genus Orbitolites have less of the opaque whiteness than many others of its family. In its simplest form it is a disk about the 1/500 of an inch in diameter, consisting of a central nucleus surrounded by from ten to fifteen concentric circular rings. The surface is usually plane, though sometimes it is concave on both surfaces in consequence of the rings increasing in thickness towards the circumference. The rings or zones are distinctly marked by furrows on the exterior of the shell, and each of these zones is divided by transverse furrows into ovate elevations with their greatest diameter transverse to the radius of the disk, so that the surface presents a number of ovate elevations arranged in consecutive circles round the central nucleus. The margin of the disk exhibits a series of convexities with depressions between them; in each of these depressions there is a circular pore surrounded by a ring of shell: these pores are the only means the animal possesses of communicating with the water in which it lives. [Illustration: Fig. 98. Simple disc of Orbitolites complanatus.] [Illustration: Fig. 99. Animal of Orbitolites complanatus.] Fig. 98 is a horizontal section of the simple Orbitolite showing the internal structure of the disk. A pear-shaped chamber with a circumambient chamber forms a nucleus which is surrounded by series of concentric rings of ovate cavities. The chambers of the nucleus and all the cavities are filled with segments of homogeneous semi-fluid sarcode, which constitute the body of the animal (fig. 99). The segments in the rings are connected circularly by gelatinous bands of sarcode extending through passages which connect the cavities laterally. The segments are also connected radially by similar sarcode bands, which originate in the mass of sarcode filling the nucleus, and extend to the pores in the margin of the disk. The cavities of each zone alternate in position with those of the zones on each side of it. The animal sends out its pseudopodia through the marginal pores in search of food, which consists of Diatoms and Desmidiaceæ; they are drawn in, digested without any stomach, and the nutritious liquid is conducted by the gelatinous bands from segment to segment and from zone to zone, even to the innermost recesses of the shell.