Page:A Treatise on Geology, volume 1.djvu/238

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222
A TREATISE ON GEOLOGY.
CHAP. VI.

which has been ascribed to the deposition of formations, from considerations founded merely on the state of conservation of organic remains.

Organic Remains.—The numerous remains of plants, zoophyta, mollusca, articulosa, and vertebral animals, belonging to the oolitic system, have long been celebrated and represented in many works of merit in England and Germany. Some general considerations arise from a contemplation of them, which deserve attention. The following estimate of the numbers of specific forms in the whole system (exclusive of the wealden formations), drawn up by the author, is at this time undoubtedly below the truth. (Encycl. Metrop. p. 653.)

Plants — marine 4 — In limestone chiefly
terrestrial cryptogamous 39 In sandstones and shales chiefly.
monocotyledonous 33
gymnospermous 4
uncertain
Polyparia — fibrous 75 Chiefly in limestones, but rarely in the lias.
corticiferous and celluliferous 44
lamelliferous 59
Kadiaria — crinoidea 31
stellerida 17
echinida 47 Chiefly in limestone, rarely in lias.
Conchifera — plagimyona 189
mesomyona 134
brachiopoda 61
Mollusca — gasteropoda 114
cephalopoda 273
annulosa 55
Crustacea 22 — Chiefly astacidæ
insects 20 — Solenhofen and Stonesfield.
fishes 20
reptiles 40
mammalia 2 or 3 Only in the lower oolite formation at Stonesfield.

In the wealden formation, are no zoophyta, no cephalopoda—various land plants—some fresh-water bivalves and univalves—a few estuary shells—cyprides, lepidotus, and other fishes—iguanodon, hylsæosaurus plesiosaurus, &c., with various chelonida, both of fresh and salt water.

The most characteristic of the plants are the group of cycadeæ, of which stems in the isle of Portland, and leaves and fruits in Yorkshire, show considerable analogy to the existing forms of the tribe, at the Cape of Good Hope, and in India and Australia. Compared with