. The chain of life in geological time [microform] : a sketch of the origin and succession of animals and plants. Paleontology; Paleobotany; Paléontologie; Paléobotanique. Fig. 7^.—Belemnitc.— Ahtr Philips. less perfectly known as fossils. So far as known, they are vastly younger than the Nautiloids, for no examples whatever have been found in the Palaeozoic. They appear abundantly in. Fig. 74/1.—Belemnoteuthis antiquus. Supposed to be a Belemnite, with soft parts preserved.—Jurassic.—After Mantell. the Mesozoic, but are there represented principally by an extinct group of squids (Belemnites a
. The chain of life in geological time [microform] : a sketch of the origin and succession of animals and plants. Paleontology; Paleobotany; Paléontologie; Paléobotanique. Fig. 7^.—Belemnitc.— Ahtr Philips. less perfectly known as fossils. So far as known, they are vastly younger than the Nautiloids, for no examples whatever have been found in the Palaeozoic. They appear abundantly in. Fig. 74/1.—Belemnoteuthis antiquus. Supposed to be a Belemnite, with soft parts preserved.—Jurassic.—After Mantell. the Mesozoic, but are there represented principally by an extinct group of squids (Belemnites and their allies. Figs. 74, 74«), remarkable for the great and complicated development of their internal support, which has a chambered float as well as a solid sheath. This family becomes extinct at the close of the ^ ?' Un produit de I'imagination, sans aucun fondement dans la ;. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original Dawson, J. W. (John William), Sir, 1820-1899. London : Religious Tract Society
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Keywords: ., bookcentury1800, bookdecade1880, booksubjectpaleontology, bookyea
