. Acadian geology : the geological structure, organic remains, and mineral resources of Nova Scotia, New Brunswick, and Prince Edward Island. Geology -- New Brunswick; Geology -- Nova Scotia; Geology -- Prince Edward Island; Paleontology -- New Brunswick; Paleontology -- Nova Scotia; Paleontology -- Prince Edward Island. 358 THE CARBONIFEROUS SYSTEM. of the footprints. Tlie stride is considerably greater than the breadth of the body. The toes are somewhat turned inward. The figure is reduced to one-sixth, so that the animal must have been rather larger than Dendrerpeton Acadianum, with shorter


. Acadian geology : the geological structure, organic remains, and mineral resources of Nova Scotia, New Brunswick, and Prince Edward Island. Geology -- New Brunswick; Geology -- Nova Scotia; Geology -- Prince Edward Island; Paleontology -- New Brunswick; Paleontology -- Nova Scotia; Paleontology -- Prince Edward Island. 358 THE CARBONIFEROUS SYSTEM. of the footprints. Tlie stride is considerably greater than the breadth of the body. The toes are somewhat turned inward. The figure is reduced to one-sixth, so that the animal must have been rather larger than Dendrerpeton Acadianum, with shorter toes and broader ; Fig. 140.—Footprints of Sauropus Sydnensis {reduced).. These footprints are quite different in form from those previously found by Sir W. E. Logan, Dr Harding, and the writer. They more nearly resemble those figured by Dr King and Mr Lea from the Carboniferous of Pennsylvania; and may have been produced by an animal generically related to that which has left the traces named Sauropus primcevus by the latter author. For this reason, until we shall obtain some knowledge of the animal from more definite remains, I propose for it the name of Sauropus Sydnensis. The specimen was found by Mr Brown in the Coal formation at North Sydney. These footprints add a ninth species to the reptilian fauna of the Coal formation of Nova Scotia, and are the first traces of this kind discovered in the Cape Breton Coal-field. The footprint already mentioned as having been found by Mr Jones of Halifax at Parrsboro', is almost precisely of the same size and form with the preceding, and may possibly have belonged to the same species. It has five distinctly marked 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, John William, Sir, 1820-1899. London : Macmillan


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