The late pleistocene cave bear fauna of the Torrener Bärenhöhle in the northern alps (Salzburg, Austria)
Research output: Contribution to journal › Article › peer-review
Standard Standard
In: Historical Biology, Vol. 31, No. 4, 11.2021, p. 422-428.
Research output: Contribution to journal › Article › peer-review
HarvardHarvard
APA
CBE
MLA
VancouverVancouver
Author
RIS
TY - JOUR
T1 - The late pleistocene cave bear fauna of the Torrener Bärenhöhle in the northern alps (Salzburg, Austria)
AU - Doppes, Doris
AU - Alberti, Federica
AU - Barlow, Axel
AU - Krutter, Sebastian
AU - FRiedrich, Ronny
AU - Hofreiter, Michael
AU - Lindauer, Susanne
AU - Kavcik-Graumann, Nadja
AU - Rosendahl, Wilfred
AU - Rabeder, Gernot
PY - 2021/11
Y1 - 2021/11
N2 - The Torrener Bärenhöhle (Cave of Torren) is an alpine bear cave in the limestone Alps near Salzburg (Austria). The entrance of this cave is located in the riverbed of a periodically flowing stream that floods the caverns during snowmelt or after heavy rainfall. Due to these flooding events, the fossiliferous layers were repeatedly destroyed and the fossil remains – mainly cave bear bones – were distributed over the cave’s entrance hall. The fossil collections have taken place since 1924. During the last decades, numerous bones scattered over the cave floor have been collected again and again. In this study, we conduct metric and morphological analyses of this fossil material as well as DNA analyses in an attempt to clarify the taxonomic position of the cave bear remains. The chronological status of the bear remains has not yet been clarified, because the few samples that have been analysed so far were beyond the range of 14C dating, indicating they are older than 49,000 cal yr BP. The following taxa are represented in small numbers: Brown bear (Ursus arctos L.), wolf (Canis lupus L.), cave lion (Panthera spelaeus Goldfuss, 1810), European bison (Bison bonasus L.) and beaver (Castor fiber L.).
AB - The Torrener Bärenhöhle (Cave of Torren) is an alpine bear cave in the limestone Alps near Salzburg (Austria). The entrance of this cave is located in the riverbed of a periodically flowing stream that floods the caverns during snowmelt or after heavy rainfall. Due to these flooding events, the fossiliferous layers were repeatedly destroyed and the fossil remains – mainly cave bear bones – were distributed over the cave’s entrance hall. The fossil collections have taken place since 1924. During the last decades, numerous bones scattered over the cave floor have been collected again and again. In this study, we conduct metric and morphological analyses of this fossil material as well as DNA analyses in an attempt to clarify the taxonomic position of the cave bear remains. The chronological status of the bear remains has not yet been clarified, because the few samples that have been analysed so far were beyond the range of 14C dating, indicating they are older than 49,000 cal yr BP. The following taxa are represented in small numbers: Brown bear (Ursus arctos L.), wolf (Canis lupus L.), cave lion (Panthera spelaeus Goldfuss, 1810), European bison (Bison bonasus L.) and beaver (Castor fiber L.).
U2 - 10.1080/08912963.2020.1849175
DO - 10.1080/08912963.2020.1849175
M3 - Article
VL - 31
SP - 422
EP - 428
JO - Historical Biology
JF - Historical Biology
IS - 4
ER -