Folia archeologica 35.
HUNTED MAMMALS IN THE ISTÁLLÓSKC5 CAVE 21 Layer V 1 : dry-cold climate, but without the characteristic arctic-alpine species of the Würm III cold maximum. Cave bear is already missing. The occurrence of willow grouse (33,00 %) culminates in this layer while the ratio of black grouse (0,76 %) here is the lowermost. Steppe species are dominant among the micro- and meso-size animals. C M DETERMINATIONS The specific assemblages of the Pleistocene sediments of the Istállóskő Cave belong to the Utrecht faunal wave. I., The fauna of Layer I — Au. I belongs to the Szeleta faunal phase (W I/Il — Hengelo Interstadial) Layer I —"LCL", A u. I the exact position of the samples is unknown. 1, 3 Preliminary Groningen dates 3 4 from bones: 3 5 lower level: Gro 44 300± 1 900 BP upper level: Gro 39 800± 900 BP II., The faunas of Layers II, III and IV belong to the Istállóskő faunal phase (W II/III — Stillfried В Interstadial) Layer III "U С L", Ли. I I middle level: Block VII, depth 80—100 cms, from charcoal got from the hearth Gro—1935 30 710 ±600 BP 3« Gro—1935 30 900 ± 600 BP 37 lower level: Block X, depth 140—150 cms, from charcoal got from the hearth Gro—1501 30 670 ± 670 BP 3 8 III., The terminus ante quen of the faunas of Layers V and VI is the Pilisszántó faunal phase (Upper layer of the Pilisszántó Rock shelter № I). 3: 1 L. Vértes tells only that that they derived from the bottom and top of Au I. (light brown clay) layer: Geyh , AÍ. A. —Schweitzer, F. et al., loc. cit. The bone remains derive from the socalled "carrion-pit" places in parts between 170—200 cm of Blocks I, III and VI —VII. As regard bone remains the lower part of Layer I was sterile. Charcoal remains were only in level 200—220/ 230 cm of Blocks VII —VIII and in level 250—260 cm of Block IX. See: excavation reports footnote N° 8. ,1 4 Geyh, AI. A. —Schweitzer, F. et al., loc. cit. Gábori-Gsdnk, V., Acta Arch. Hung. 22(1970) 9—, 1, 6 Vértes, L.— Vries, H., Arch. Ért. 86(1959) 195. and footnote N" 3. For excavation documentation see in footnote № 8. 3 7 Kretzoi, M. Vértes, L., Acta Geol. 9(1965) 139.; Geyh, M. A.—Schweitzer, F. et al., loc. cit. 3 8 Erroneously determined as Au I.: Vértes , V., Arch. Ért. 84(1957) 222.; Vértes, L. — Vries, H., op. cit. (1959) 195.; footnote N" 3., Excavation documentation see in footnote N° 8.