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W. BOYD DAWKINS ON TIIE MAMMAL-FAUNA 



W5 ^ -^_ 



been confirmed since by repeated visits, are shared by Prof. Hughes, 

 whose opinions on a matter of this kind are entitled to the greatest 

 weight. At present he holds that it is postglacial. 



The second reputed case of the discovery of Pleistocene mamma- 

 lia in Glacial or Interglacial deposits is offered by those in the caves 

 of Cefn explored and described by Dr. Falconer, Mrs. AYilliam 

 Wynn, Prof. Hughes, the Rev. D. R, Thomas, and myself, and lately 

 correlated (Quart. Journ. Geol. Soc. xxxii. p. 94) by Mx. Mackin- 

 tosh with the Glacial strata of the surrounding district. Here, 



