34 JOURNAL OF THE [January, 



Dawson, J. W. Origin and History of Life on our Planet. An 

 Address before the Amer. Asso. Adv. Sci. (Detroit meet- 

 ing), vol. xxiv, 1875. Reprint 26 pp., Montreal, 1875. 

 Remark on Eozoon, 



Dawson, J. W. On the Geological Relations and Mode of 

 Preservation of Eozoon canadense. Rep. Brit. Asso., liii, p. 

 494, 1884. 



Dawson, J. W. Notes on Eozoon canadense (abstract of a 

 paper read before the British Association at Southport, 1883). 

 The Canadian Rec. of Sci., vol. i, pp, 58, 59, 1884. 



Dawson (Sir), J. W. Remarks on Eozoon, in his Presidential 

 Address before the British Association for the Advancement 

 of Science, Sept., 1886. The Canadian Rec. Sci., vol. ii, pp. 

 201-228, 1886. 



De Stefani, C. Sulle Serpentine Italiane. Estraite dagli Atti 

 del R. Istituto veneto di scienze, lettere ed arti, vol. ii, ser. vi., 

 (18 pp.), 1884. 



Duncan, P. M. Note on Eozoon canadense. Joum. Roy. 

 Micro. Soc, vol. iii, pp. 615, 616, 1883. 



Gratacap, L. p. The Eozoonal Rock of Manhattan Island. 

 Amer. Joum. Sci., ser. 3, vol. xxxiii, pp. 374-378, 7 wood- 

 cuts, 1887. 



GuMBEL, C. Geognostische Beschreibung des ostbayerisches, 

 Grenzgebirges, 1868. 



Hahn, O. Die Urzelle, nebst dem Beweis dass Granit, Gneiss, 

 Serpentin, Talk, gewisse Sandsteine, auch Basalt, endlich 

 Meteorstein und Meteoreisen aus pflanzen bestehen, 1879. 



Harkness (Prof.), R. '' Eozoon" ha.v'mg been brought under 

 the notice of the Geological Section of the British Associa- 

 tion, held in Birmingham of the year, Prof. R. Hark- 

 ness declared his disbelief in it. " Reader," Sept. 30, 1865. 



Harkness (Prof.), R. On the Metamorphic and Fossiliferous 

 Rocks of the county of Galway. Quart. Joum. Geol. Soc, 

 vol. xxii, pp. 510, 511, 1866. 



With reference to the occurrence of serpentine in connection with the 

 limestones of the metamorphic series of Connemara, this has of late become 

 a matter of some interest, in consequence of the statement that these de- 

 posits afford the Eozoon Canadense. . . . The supposed organic 

 portions of the serpentinous limestones of Connemara do not result from 

 animal structure, but purely from mineral association. Had fossils of 



