. The geology of Nova Scotia, New Brunswick, and Prince Edward Island, or, Acadian geology [microform]. Geology; Geology, Stratigraphic; Paleontology; Geology, Economic; Géologie; Géologie stratigraphique; Paléontologie; Géologie économique. 244 THE CARBONIFEROUS SYSTEM. .li. Pala3opteris Ilarttii, Dawson, Coal Creek, Gran J Lake. Lepidodendron Pictoeiise, Dawson, „ Newcastle lliver, Grand Lake. Lepidostrobus scjuamosus, Dawson, „ „ „ Cordaites , Corda, C. simplex, Dawson, Cardiocarpum bisectatum, Dawson, „ Bale de Cbaleur. Newcastle Itiver, Fig. 73.—NaggeratUiix diapar. Ual/nat.
. The geology of Nova Scotia, New Brunswick, and Prince Edward Island, or, Acadian geology [microform]. Geology; Geology, Stratigraphic; Paleontology; Geology, Economic; Géologie; Géologie stratigraphique; Paléontologie; Géologie économique. 244 THE CARBONIFEROUS SYSTEM. .li. Pala3opteris Ilarttii, Dawson, Coal Creek, Gran J Lake. Lepidodendron Pictoeiise, Dawson, „ Newcastle lliver, Grand Lake. Lepidostrobus scjuamosus, Dawson, „ „ „ Cordaites , Corda, C. simplex, Dawson, Cardiocarpum bisectatum, Dawson, „ Bale de Cbaleur. Newcastle Itiver, Fig. 73.—NaggeratUiix diapar. Ual/nat. Nceggeratliia dispar (Fig. 73), Dawson, Baie de Chaleur. Halonia? sp. ? Dawson, Coal Creek. {b) Lower Coal Formation—{Horizon of the Albert shales, etc.). Cyclopteris Acadica, Dawson, Norton Creek. Lepidodendron corrugatum, * ,, „ Cordaites borassifulia Corda, Albert shales. (Figured iu Jackson's Report.) FOSSIL ANIMALS. Mr Hartt mentions (Appendix to Bailey's Report) that the only animal fossils he has found in the Coal measures are Spirorbis carbon- arius, attached to plants, and coprolites of fishes. In the Lower Car- boniferous Limestones he has observed fossils of most of the genera to be noticed in subsequent pages as occurring in these beds in Nova Scotia; but they have not been examined as to species, which, however, in so far as my observation extends, are identical with those of Nova Scotia. Dr Jackson has named and figured three species of Palceo- niscus from the Albert shales. One of these is represented in Fig. 62 above; and I have seen another specimen which appears to belong to a second of this species, but the figures and descriptions are not suf- ficient for their certain determination. * See Figa. 74, 75, and 76 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 wo
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Keywords: ., boo, bookcentury1800, booksubjectgeology, booksubjectpaleontology
