Vörös A. szerk.: Fragmenta Mineralogica Et Palaentologica 18. 1996. (Budapest, 1996)

times). Thus, we give the lists of them summarized (details see in the inventory of the original material in the collection of Budapest) (Fig. 1). In the quarry, before and above the (artificial) entrance of the cave, we found also a rich paleontological material, which seem to be contemporaneous with the former collected matter and we designated it as Locality 17, Beremend (B/17). On the basis of all these, TAKÁCSNÉ BOLNER (1985) published a short interpretation of the fauna, according to determinations by D. JÁNOSSY and GY. TOPÁL. She published the main Locality 16 Beremend under the designation "Passage of Bones". We collected the large bones as well as a rich microfauna on the site and we obtained and washed about fifty kilogramm red clay, later picked out for bones too. O 10m Fig. I

. Sketch map of the horizontal plane of the "Crystal Cave" of Beremend at the level of the (artificial) entrance. Asterisks indicate places of paleontological localities of Beremend 16 THE FOSSIL REMAINS In the following I give the list of the fossils, collected in the localities, with some systematical - stratigraphical remarks. Celtis sp.; B/17: one whole and 89 fragments of the kernels of this Mediterranean tree, otherwise widespread in the Lower Pleistocene to present in the VillányMountains, were present among the bones. Celtis sp. is lacking in the Loc.

B/

16. Osteichthyes ("Pisces"); B/16: Fragment of a pharyngeal tooth 5 vertebrae-fragm.; B/17: Fragm. of a pharyngeal tooth and two vertebrae-fragm. The remains originate presumably from Cyprinids.