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Cadernos Lab. Xeolóxico de Laxe Coruña. 2001. Vol. 26, pp. 447-455 ISSN: 0213-4497 The updated record of cave bear and other members of the genus Ursus on the territory of Czech Republic Registro actualizado de Oso de las Cavernas y otras especies del género Ursus en la República Checa A B S T R A C T WAGNER, J. During the 2nd half of 20th century, a succession of new Pleistocene localities was discovered and some classical paleontological sites were revised. From many of those places also bear remains were recorded. Nine localities provided large material of bear remains in good stratified layers. Bear record from Moravian localities were studied in details by Prof. R. MUSIL from Brno. This paper presents a review of updated knowledge on this localities - especially about their stratigrafical position (based on micromammalian evidence) and basic information on bear remains studied. Key words: Pleistocene, U r s u s, cave bear, brown bear, Czech Republick, Bohemian karst, Moravian Karst Charles University. Faculty of Sciences. Department of Palaeontolog. Albertova 6.12843 Praha 2. CZECH REPUBLIC
448 WAGNER, J. CAD. LAB. XEOL. LAXE 26 (2001) INTRODUCTION Palaeontological investigation of fossil cenozoic mammals has a tradition in the territory of the Czech Republic. Already from the begining of this investigations remains of bears were among the most frequent finds. The first phase research started in area of Moravian karst in the 1 st half of the 19 th century (e. g. WANKEL made in 1850 first skeleton of cave bear in the Austria-Ungarn from bones founded in Vupustek cave). From the 2 nd half of 19 th century lot of data about bear finds from Moravia (WANKEL. 1867; MASKA, 1884, 1886; KNIES, 1891, 1893 etc.) and from Bohemia (KREJCI, 1865; LAUBE, 1874; WOLDRICH, 1890, 1893, etc.) has been recorded. At the end of 19 th and during the 1 st half of 20 th century first lists of vertebrates fossils finds (incl. bears) were given from the area of Bohemia (WOLDRICH, 1897; KAFKA, 1901; B AYER, 1905) and Moravia (KNIES, 1929; STEHLIK, 1929; SKUTIL & STEHLIK, 1932). The old authors determined their finds mostly as U. spelaeus or Ursus arctos/priscus. Some of these finds are but lost, the most of remaining is not revised and without stratigraphical level or correct localization. Till in 2 nd half of 20 st century began modern palaeontological research. New and revised old localities are discovered, with emphasis to stratigraphical signification. The most important researchers of this period are FEJFAR in Bohemia (FEJFAR, 1956, 1961, 1993, etc.) and MUSIL (MUSIL, 1959, 1962, 1965, 1968, etc.) in Moravia. The papers of the last author brougt detailed studies of cave and brown bear. The most important informations are given by new discovered sites with both large and small mammals together, which allows morphometric studies of bears combined with their exact stratification. The most importent are as follows: 1) Holstejn (Moravian karst) Stratigraphy: zona B of Early Biharian 1 (FEJFAR & HORACEK, 1990) Stratigraphicaly significant taxa from this locality: Microtus (Allophaimys) pliocae - n i c u s KORMOS, Mimomys pusilus (MÉHELY), Pliomys episcopalis MÉHELY, P. lenki (HELLER), Hypolagus beremendensis (PETENYI) (according MUSIL, 1966). The others species of carnivores from this locality: P a n t h e r a cf. g o b a s z o e g e n s i s (KRETZOI), Putorius cf. stromeri KOR- MOS, Meles meles (LINNAEUS) (according MUSIL, 1966). Locality was discovered in 1965 during limestone-mining. It was a chimney cave infilled with terra rossa deposits. Fauna was published by MUSIL (1966). The locality provided about 30 items of bears, all identified as Ursus sp. by MUSIL who compared them to the bears of Biharian age (U. deningeri, U. mediterra - neus, U. e. ? d. gombaszoegensis) but did not coidentified the Holstejn bears with anyone of them. The form was very near to U. e. ? d. gombaszoegensis but exhibited some more primitive features. The following items were published: fragment of mandible with M 2 and M 3 , free C, fragment of mandible with C, and a lot of fragments of long bones, hand and food bones and ribs. 2) Stranska Skala (Brno) Stratigraphy: Late Biharian 2 (FEJ- FAR & HORACEK, 1990)
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