. Note on Carboniferous Entomostraca from Nova Scotia, in the Peter Redpath Museum, determined and described by Prof. T. Rupert Jones, S., and Mr. Kirby [microform]. Paleontology; Geology, Stratigraphic; Paléontologie; Géologie stratigraphique. KiR. 8, X a. 2. Carhonia hairdhides, J. & K. (Fig. 8.) Less almndant than the preceding, at the Joggins and also at Mabou, where it was collected along with the preceding by Mr. Foord, but it is abundant in the Upper Coal Formation of Smelt Brook, East Itiver, Pietou. It is also a common Scottish Fig. 9, X 25. 3. Gandona elotigata, J.


. Note on Carboniferous Entomostraca from Nova Scotia, in the Peter Redpath Museum, determined and described by Prof. T. Rupert Jones, S., and Mr. Kirby [microform]. Paleontology; Geology, Stratigraphic; Paléontologie; Géologie stratigraphique. KiR. 8, X a. 2. Carhonia hairdhides, J. & K. (Fig. 8.) Less almndant than the preceding, at the Joggins and also at Mabou, where it was collected along with the preceding by Mr. Foord, but it is abundant in the Upper Coal Formation of Smelt Brook, East Itiver, Pietou. It is also a common Scottish Fig. 9, X 25. 3. Gandona elotigata, J. & K. (Fig. 0.) Larger and more elongated than the preceding forms, but much less abun- dant. It attains the length of -j\fth of an inch. Prof. Jones has some interesting remarks on the very wide distribution oi all these species in the Northern Hemisj)here, in connection with the fact that they were probably shallow-water, or even brackish-water species. This indicates means of transit for such animals, by shallow areas either now oceanic or now land. It concurs with many other facts in showing that the comparative rarity of great ocean depths and high mountain ranges. 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, J. W. (John William), Sir, 1820-1899. Montreal : [s. n. ]


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