. 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. FLORA OF THE DEVONIAN. 137 (lant at St Jolin, both in tlic sandstone containing coniferous trees, and (he shales wliich aft'onl Ferns, Cordaites, etc. Some of the beds of tlie latter arc filled with flattened stems. This was one of the first fossils recognised in the St John r
. 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. FLORA OF THE DEVONIAN. 137 (lant at St Jolin, both in tlic sandstone containing coniferous trees, and (he shales wliich aft'onl Ferns, Cordaites, etc. Some of the beds of tlie latter arc filled with flattened stems. This was one of the first fossils recognised in the St John rocks, specimens having been shown to me in 1857 by the late Professor Kobb.* Fig. 186.—Calamiks ^^U Calamites canncefor7nis, Brongniart. This species, presenting the characters which it exhibits in the Coal measures, occurs in the ledges west of Carlton, associated with the last species, but in much less abundance. It is a widely distributed species, but has not, I believe, been found previously in rocks older than the Lower Carboniferous. [Asteroplit/Ilites, etc.) Asterophyllites aclcidaris, Dn. (Fig. 194, II and IP). Stems slender, striated, thickened at the nodes, leafy. Leaves one-nerved, linear, * Dr Gesner mentions (Second Report, 18-iO, p. 12) a Calamite (probably this species) IS occurring near Little 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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