. Outlines of natural theology for the use of the Canadian student [microform] : selected and arranged from the most authentic sources. Natural history; Natural theology; Sciences naturelles; Théologie naturelle. ? I * \ 444. hngirostris was of similar general proportions ; and that trilophedon augustidens was higher in its limbs, and of a comparatively light and slender shape. In his remarks on the geological age, and associated faunas of the formations in which each of these spe- cies severally occur, Dr. Falconer has noticed that trilophcdon augustidens is a characteristic species of the mi
. Outlines of natural theology for the use of the Canadian student [microform] : selected and arranged from the most authentic sources. Natural history; Natural theology; Sciences naturelles; Théologie naturelle. ? I * \ 444. hngirostris was of similar general proportions ; and that trilophedon augustidens was higher in its limbs, and of a comparatively light and slender shape. In his remarks on the geological age, and associated faunas of the formations in which each of these spe- cies severally occur, Dr. Falconer has noticed that trilophcdon augustidens is a characteristic species of the miocene falunian beds throughout Europe, and is associated with trilophodon tapiroides in the faluris (middle tertiary) of France, and the upper fresh- water molasse of Switzerland. The tetralophodon avernensis is characteristic of the pliocene fauna, and it had a very extended range over Europe, accom- panying loxodon (nesti) in Tuscany; trilophodon, borsoni, loxodon prisons, and elephas antiquusin Piedmont and Lombardy ; loxodon meridionalis at Montpellier ; and trilophodon borsoni, loxodon me- ridionalis, and loxodon prisons in Yelay and Au- vergne. Dr. Falconer concludes that,—1st. The mastodon remains which have been met with in the fluvio-marine crags, belong to a pliocene form, named tetralophodon avernensis. 2ndly. That the mam- malian fauna of the red and fluvio-marine crags, regarded as a whole, bears all the characters of a pliocene age, and is identical with the sub-Appenine pliocene fauna of Italy. 3rdly. The red and flnvio* marine crags, tested by their mammalian fauna, must be considered as a bed of the same age. Consider* ing these observations, so recently made by 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 Bovell, James, 1817-1880. [Toronto? : s. n. ]
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