Betfia 10: Early/Lower Pleistocene, Romania
List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
Mammalia
- Chiroptera
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Chiroptera indet.
Blumenbach 1779
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Mammalia
- Carnivora
- Mustelidae
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Mustela praenivalis
Kormos 1934
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M. praenivalis ? | ||||||||||
Mammalia
- Talpidae
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Talpa fossilis
Petenyi 1864
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T. fosslis sp. | ||||||||||
Talpa minor
Freudenberg 1914
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Mammalia
- Soricidae
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Beremendia fissidens
(Petényi 1864)
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Crocidura sp.
Wagler 1832
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Episoriculus gibberodon
Petenyi 1864
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Petenyia hungarica
Kormos 1934
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Sorex margaritodon
Kormos 1930
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Mammalia
- Lagomorpha
- Leporidae
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Lepus sp.
Linnaeus 1758
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Hypolagus brachygnathus
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Mammalia
- Rodentia
- Cricetidae
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Cricetus cricetus
(Linnaeus 1758)
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C. cricetus nanus | ||||||||||
Allocricetus bursae
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Mimomys pusillus
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Mimomys tornensis
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Microtus pliocaenicus
(Kormos 1932)
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original and current combination Allophaiomys pliocaenicus | ||||||||||
M. (A.) pliocaenicus pliocaenicus | ||||||||||
Ungaromys cf. nanus
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Lagurus arankae
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Pliomys episcopalis
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Mammalia
- Rodentia
- Muridae
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Spalax sp.
Güldenstadt 1770
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Apodemus ex gr. sylvaticus
(Linnaeus 1758)
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original and current combination Mus sylvaticus | ||||||||||
Mammalia
- Rodentia
- Gliridae
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Glirulus pusillus
(Heller 1936)
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original and current combination Amphidyromys pusillus | ||||||||||
Glis sackdillingensis
Heller 1930
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Muscardinus dacicus
Kormos 1930
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Mammalia
- Rodentia
- Sciuridae
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Sciurus sp.
Linnaeus 1758
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Spermophilus primigenius
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see common names |
Geography
Country: | Romania | County: | Bihor |
Coordinates: | 47.0° North, 22.0° East (view map) | ||
Paleocoordinates: | 46.9° North, 22.0° East | ||
Basis of coordinate: | based on nearby landmark |
Time
Period: | Quaternary | Epoch: | Pleistocene |
10 m.y. bin: | Cenozoic 6 | ||
*Period: | Early/Lower Quaternary | *Epoch: | Early/Lower Pleistocene |
*International age/stage: | Early/Lower Waalian | *Local age/stage: | Early/Lower Biharian |
Key time interval: | Early/Lower Pleistocene | ||
Age range of interval: | 2.58000 - 0.77400 m.y. ago | ||
* legacy (obsolete) database fields |
Stratigraphy
Stratigraphy comments: Fewer members of the genus Mimomys, prevalence of arhizodont arvicolids, plus the primitive and homogenous morphology of Microtus has led site to be dated on biostratigraphic grounds to the Lower Waalian (~1.4-~1.3Ma). Abundance of Muridae and the occurence of Glirulus pusillus are in any case evidence of a temperate phase. |
Lithology and environment
Lithology description: Accumulated in a small, entirely silted cave near the village of Betfia, opened by quarrying for Cretaceous limestone. | |
Environment: | cave |
Geology comments: Accumulated in a small, entirely silted cave near the village of Betfia, opened by quarrying for Cretaceous limestone. |
Taphonomy
Size of fossils: | macrofossils,mesofossils |
Disassociated major elements: | many |
Disassociated minor elements: | many |
Collection methods and comments
Collection methods: | bulk,field collection |
Reason for describing collection: | biostratigraphic analysis |
Collection method comments: Caves discovered between 1966 and 1991 and excavated by the Bucharest Speleological Institute and the "Tarii Crisurilor" Museum of Oradea. | |
Taxonomic list comments:Fewer members of the genus Mimomys, prevalence of arhizodont arvicolids, plus the primitive and homogenous morphology of Microtus has led site to be dated on biostratigraphic grounds to the Lower Waalian (~1.4-~1.3Ma). Abundance of Muridae and the occurence of Glirulus pusillus are in any case evidence of a temperate phase. |
Metadata
Also known as: | Betfia X, Somleu Hill | ||
Database number: | 32192 | ||
Authorizer: | A. Behrensmeyer | Enterer: | H. O'Regan |
Modifier: | H. O'Regan | Research group: | PACED |
Created: | 2003-06-10 02:40:41 | Last modified: | 2003-08-12 07:12:23 |
Access level: | the public | Released: | 2003-06-10 02:40:41 |
Creative Commons license: | CC BY |
Reference information
Primary reference:
8655. | E. Terzea. 1996. Biochronology of the Pleistocene deposits at Betfia (Bihor, Romania). Acta Zoologica Cracovensia 39(1):531-540 [A. Behrensmeyer/H. O'Regan/H. O'Regan] |