1 I 



304 



Ari'ENDlX 





i 



structures of Eozoon, and shown its resemblance to 

 modern forms, places Eozoon as a generalized type 

 between the Nummuline and Rotaline groups of 

 Foraminifera. It resembles the former in its fine 

 and complicated tubulations, and some of the 

 larger sessile forms of the latter in its habit of 

 growth. More especially, this is near to that of 

 the genera Carpenteria and Polytrema. In the 

 former, more especially, there are a number of 

 somewhat flattened calcareous cells with perforated 

 walls, and built up in a conical form arout.d a 

 central pipe or funnel into which the apertures of 

 the cells open. A specimen of Carpenteria, enlarged 



ill 



structure and aflfinities of Eozoon Canadense, Quart. Journ. 

 Geol. Soc, Lond. Vol. xxii., pp. 219-228, 1866. Notes on 

 the structures and afifinities of Eozoon Canadense. Canad. 

 Nat.^ new sen, vol. ii., pp. 111-119, wood-cut, 1865. A reprint 

 from Quart. Journ. Gcol. Soc, Lond., 1865. Further obser- 

 vations on the structure and affinities of Eozoon Canadense. 

 In a letter to the President. Pfoc. Roy. Soc, Lond., vol. xxv., 

 pp. 503-508, 1867. New observations on Eozoon Canadense. 

 Ann. and Mag. Nat. Hist., ser. 4, vol. xiii., pp. 456-470, one 

 plate, 1874. Final note on Eozoon Canadense. Ann. and 

 Mag. Nat. Hist., ser. 4, vol. xiv., pp. 371-372, 1874. Remarks 

 on Mr. H. J. Carter's letter to Prof. King on the structure of 

 the so-called Eozoon Canadense. Ann. and Mag. Nat. Hist., 

 ser. 4, vol. xiii., pp. 277-284, with two engravings, 1874. 



