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37. [208] Quart. Journ. Geol. Soc. 1852, p. 62. [209] Proceedings Roy. Astronom. Soc. No. iii. Jan. 1840. [210] See a Memoir on the Temperature of the Terrestrial Globe, and the Planetary Spaces, Ann. de Chimie et Phys. tom. xxvii. p. 136. Oct. 1824. [211] Sir H. Davy, Consolations in Travel: Dialogue III. "The Unknown." [212] Quart. Journ. Geol. Soc. 1852. [213] Buckland's Bridgewater Treatise, p. 409. [214] Owen's Report on "British Fossil Reptiles, to Brit. Soc." 1841, p. 200. [215] Quart. Journ. Geol. Soc. No. 6, p. 96. [216] See Hitchcock's Report on Geol. of Massachusetts, and Lyell's Travels in North America, chap. 12. [217] See Manual of Geol. by the Author, index _Microlestes_. [218] This figure (No. 8) is from a drawing by Professor C. Prevost, published Ann. des Sci. Nat. Avril, 1825. The fossil is a lower jaw, adhering by its inner side to the slab of oolite, in which it is sunk. The form of the condyle, or posterior process of the jaw, is convex, agreeing with the mammiferous type, and is distinctly seen, an impression of it being left on the stone, although in this specimen the bone is wanting. The anterior part of the jaw has been partially broken away, so that the double fangs of the molar teeth are seen fixed in their sockets, the form of the fangs being characteristic of the mammalia. Ten molars are preserved, and the place of an eleventh is believed to be apparent. The enamel of some of the teeth is well preserved. [219] A colored figure of this small and elegant quadruped is given in the Trans. Zool. Soc. vol. ii. pl. 28. It is insectivorous, and was taken in a hollow tree, in a country abounding in ant-hills, ninety miles to the southeast of the mouth of Swan River in Australia.--It is the first living marsupial species known to have nine molar teeth in the lower jaw, and some of the teeth are widely separated from others, one of the peculiarities in the thylacotherium of Stonesfield, which at first induced M. Blainville to refer that creature to the class of reptiles. [220] This figure (No. 10) was taken from the original, formerly in Mr. Broderip's collection, and now in the British Museum. It consists of the right half of
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