V. Contributions to the Fossil Quarternary Flora of Cyprus. 



When ridiiiir through tlie Kyrenia-pass on tlie 2nd of June, 1905, I had the fortune of discovering- 

 great deposits of calcareous tufa, containing numerous excellent impressions of fossil plants. At that season 



Fig. 63. The Tufa-ljiiuk at Kazan seen from the Upitu.sitf side ut' the Valley. 



I could not spare any time from the study of the living vegetation, but in the month of September I 

 returned to the place, examined the profll and made collections of fossils in the various levels. The fossils 

 I have afterwards determined in the botanical Institute of the University at Vienna under the conduct of 



