Late Pleistocene voles (Arvicolinae, Rodentia) from the Baranica Cave (Serbia)
Samo za registrovane korisnike
2012
Članak u časopisu (Objavljena verzija)
Metapodaci
Prikaz svih podataka o dokumentuApstrakt
Baranica is a cave system situated in the south-eastern part of Serbia, four kilometers south to Knjazevac, on the right bank of the Trgoviski Timok. The investigations in Baranica were conducted from 1994 to 1997 by the Faculty of Philosophy from Belgrade and the National Museum of Knjazevac. Four geological layers of Quaternary age were recovered. The abundance of remains of both large and small mammals was noticed in the early phase of the research. In this paper, the remains of eight vole species are described: Arvicola terrestris (Linnaeus, 1758), Chionomys nivalis (Martins, 1842), Microtus (Microtus) arvalis (Pallas, 1778) and Microtus (Microtus) agrestis (Linnaeus, 1761), Microtus (Stenocranius) gregalis (Pallas, 1779), Microtus (Terricola) subterraneus (de Selys-Longchamps, 1836), Clethrionomys glareolus (Schreber, 1780) and Lagurus lagurus (Pallas, 1773). Among them, steppe and open area inhabitants prevail. Based on the evolutionary level and dimensions of the Arvicola terres...tris molars, as well as the overall characteristics of the fauna, it was concluded that the deposits were formed in the last glacial period of the Late Pleistocene. These conclusions are rather consistent with the absolute dating of large mammal bones (23.520 +/- 110 B. P. for Layer 2 and 35.780 +/- 320 B.P. for Layer 4).
Ključne reči:
Serbia / rodents / Quaternary / Late Pleistocene / Balkans / arvicolidsIzvor:
Geologica Carpathica, 2012, 63, 1, 83-94Izdavač:
- Slovak Acad Sciences Geological Inst, Bratislava
Finansiranje / projekti:
- Geodiverzitet, litostratigrafija i geološka evolucija basena centralnog Balkanskog poluostrva i susednih oblasti (RS-MESTD-Basic Research (BR or ON)-176015)
- Kulturne promene i populaciona kretanja u ranoj praistoriji centralnog Balkana (RS-MESTD-Basic Research (BR or ON)-177023)
DOI: 10.2478/v10096-012-0006-6
ISSN: 1335-0552
WoS: 000301748900006
Scopus: 2-s2.0-84858690404
Institucija/grupa
Arheologija / ArchaeologyTY - JOUR AU - Bogićević, Katarina AU - Nenadić, Draženko AU - Mihailović, Dušan PY - 2012 UR - http://reff.f.bg.ac.rs/handle/123456789/1357 AB - Baranica is a cave system situated in the south-eastern part of Serbia, four kilometers south to Knjazevac, on the right bank of the Trgoviski Timok. The investigations in Baranica were conducted from 1994 to 1997 by the Faculty of Philosophy from Belgrade and the National Museum of Knjazevac. Four geological layers of Quaternary age were recovered. The abundance of remains of both large and small mammals was noticed in the early phase of the research. In this paper, the remains of eight vole species are described: Arvicola terrestris (Linnaeus, 1758), Chionomys nivalis (Martins, 1842), Microtus (Microtus) arvalis (Pallas, 1778) and Microtus (Microtus) agrestis (Linnaeus, 1761), Microtus (Stenocranius) gregalis (Pallas, 1779), Microtus (Terricola) subterraneus (de Selys-Longchamps, 1836), Clethrionomys glareolus (Schreber, 1780) and Lagurus lagurus (Pallas, 1773). Among them, steppe and open area inhabitants prevail. Based on the evolutionary level and dimensions of the Arvicola terrestris molars, as well as the overall characteristics of the fauna, it was concluded that the deposits were formed in the last glacial period of the Late Pleistocene. These conclusions are rather consistent with the absolute dating of large mammal bones (23.520 +/- 110 B. P. for Layer 2 and 35.780 +/- 320 B.P. for Layer 4). PB - Slovak Acad Sciences Geological Inst, Bratislava T2 - Geologica Carpathica T1 - Late Pleistocene voles (Arvicolinae, Rodentia) from the Baranica Cave (Serbia) EP - 94 IS - 1 SP - 83 VL - 63 DO - 10.2478/v10096-012-0006-6 ER -
@article{ author = "Bogićević, Katarina and Nenadić, Draženko and Mihailović, Dušan", year = "2012", abstract = "Baranica is a cave system situated in the south-eastern part of Serbia, four kilometers south to Knjazevac, on the right bank of the Trgoviski Timok. The investigations in Baranica were conducted from 1994 to 1997 by the Faculty of Philosophy from Belgrade and the National Museum of Knjazevac. Four geological layers of Quaternary age were recovered. The abundance of remains of both large and small mammals was noticed in the early phase of the research. In this paper, the remains of eight vole species are described: Arvicola terrestris (Linnaeus, 1758), Chionomys nivalis (Martins, 1842), Microtus (Microtus) arvalis (Pallas, 1778) and Microtus (Microtus) agrestis (Linnaeus, 1761), Microtus (Stenocranius) gregalis (Pallas, 1779), Microtus (Terricola) subterraneus (de Selys-Longchamps, 1836), Clethrionomys glareolus (Schreber, 1780) and Lagurus lagurus (Pallas, 1773). Among them, steppe and open area inhabitants prevail. Based on the evolutionary level and dimensions of the Arvicola terrestris molars, as well as the overall characteristics of the fauna, it was concluded that the deposits were formed in the last glacial period of the Late Pleistocene. These conclusions are rather consistent with the absolute dating of large mammal bones (23.520 +/- 110 B. P. for Layer 2 and 35.780 +/- 320 B.P. for Layer 4).", publisher = "Slovak Acad Sciences Geological Inst, Bratislava", journal = "Geologica Carpathica", title = "Late Pleistocene voles (Arvicolinae, Rodentia) from the Baranica Cave (Serbia)", pages = "94-83", number = "1", volume = "63", doi = "10.2478/v10096-012-0006-6" }
Bogićević, K., Nenadić, D.,& Mihailović, D.. (2012). Late Pleistocene voles (Arvicolinae, Rodentia) from the Baranica Cave (Serbia). in Geologica Carpathica Slovak Acad Sciences Geological Inst, Bratislava., 63(1), 83-94. https://doi.org/10.2478/v10096-012-0006-6
Bogićević K, Nenadić D, Mihailović D. Late Pleistocene voles (Arvicolinae, Rodentia) from the Baranica Cave (Serbia). in Geologica Carpathica. 2012;63(1):83-94. doi:10.2478/v10096-012-0006-6 .
Bogićević, Katarina, Nenadić, Draženko, Mihailović, Dušan, "Late Pleistocene voles (Arvicolinae, Rodentia) from the Baranica Cave (Serbia)" in Geologica Carpathica, 63, no. 1 (2012):83-94, https://doi.org/10.2478/v10096-012-0006-6 . .