INTRODUCTION, XXI 



structure, but purely from mineral association. Had fossils of 

 any kind presented themselves in this district, they ought to 

 have occurred in that portion of the limestone which has been 

 least affected by metamorphic action." 



Mr. W, Warington Smyth, in his Anniversary Address 1867, 

 Q. J. G. S. vol. xxiii. p. Ixiv) as President of the Geological 

 Society, noticing the announcement made by Dr. Dawson of " the 

 occurrence of Eozoon preserved simply in carbonate of lime/' 

 declared that this ' ' discovery of Eozoon preserved in carbonate 

 of lime pure and simple would appear to close the discussion," 



Further Observations on the Structure and Affinities of Eozoon 1867. 

 Canadense. Dr. W. B. Carpenter, A letter to the Presi- 

 dent of the Royal Society. Proc. R. S. vol. xv. pp. 545-549. 

 The writer, who had previously made a similar acknowledg- 

 ment in his " Notes" (A.D. 1866), declares : " Yet the very 

 exact correspondence in age and mode of aggregation between 

 the serpentine granules of the Connemara marble and those of 

 the ' acervuline portion ' of the Canadian was sufficient to 

 justify in behalf of the one the claim which has been freely 

 conceded in regard to the other." 



On new Specimens of Eozoon. Sir W. E. Logan. Q. J. G. S. 1867. 

 vol. xxiii. pp. 253-257, 



Notes on Fossils recently obtained from the Laurentian Kocks 1867. 

 of Canada, and on Objections to the Organic Nature of 

 Eozoon. Dr. J. W. Dawson. Q. J. G. S. vol. xxiii. pp. 257- 

 264. 



The paper is in a great measure taken up with a description 

 of a specimen of ' ' Eozoon " from Tudor (the one noticed by 

 Carpenter A.D* 1866, Warington Smyth A.D. 1867, and Logan 

 as above), stated to consist ( ' simply of carbonate of lime." 



Esquisse Geologique du Canada. ? Prepared by the Officers of 1867. 



the " Commission Geologique du Canada." 

 Notices the Tudor and other specimens of " Eozoon." 



