Schmiedrued-Pfyffrüti (SP) 618: Early/Lower Miocene, Switzerland
List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
Amphibia
- Temnospondyli
- Urodela
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Proteidae indet.
Hogg 1838
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Reptilia
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Amphisbaenidae indet.
(Gray 1865)
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Reptilia
- Lacertidae
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Lacertidae indet.
Bonaparte 1831
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Reptilia
- Anguidae
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Ophisaurus sp.
Daudin 1803
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Anguis sp.
Linnaeus 1758
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Reptilia
- Testudoolithidae
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Testudoolithidae indet.
Hirsch 1996
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Mammalia
- Lipotyphla
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Lipotyphla indet.
Haeckel 1866
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synonym of Eulipotyphla | ||||||||||
Mammalia
- Erinaceidae
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Galerix sp.
Pomel 1848
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Mammalia
- Lagomorpha
- Ochotonidae
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Prolagus oeningensis
(König 1825)
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Mammalia
- Rodentia
- Cricetidae
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Megacricetodon bavaricus
(Fahlbusch 1964)
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Noted to be very abundant (>20 specimens) | ||||||||||
Mammalia
- Rodentia
- Gliridae
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Miodyromys aff. aegercii
Baudelot 1972
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Gastropoda
- Heterostropha
- Limacidae
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Limax sp.
Linnaeus 1758
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Gastropoda
- Heterostropha
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Helicoidea indet.
Rafinesque 1815
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"Helicacea indet." | ||||||||||
Gastropoda
- Heterostropha
- Planorbidae
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Gyraulus sp.
Charpentier 1837
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Gastropoda
- Bithyniidae
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Bithynia sp.
Leach 1818
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unclassified
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Charophyta indet.
Migula 1890
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see common names |
Geography
Country: | Switzerland | State/province: | Aargau | County: | Schmiedrued |
Coordinates: | 47.3° North, 8.1° East (view map) | ||||
Paleocoordinates: | 47.4° North, 6.3° East | ||||
Basis of coordinate: | stated in text | ||||
Geographic resolution: | outcrop |
Time
Period: | Neogene | Epoch: | Miocene |
10 m.y. bin: | Cenozoic 5 | ||
Key time interval: | Early/Lower Miocene | ||
Age range of interval: | 23.03000 - 15.98000 m.y. ago | ||
Age estimate: | 16.2 to 16.1 Ma (paleomagnetic) |
Stratigraphy
Geological group: | Upper Freshwater Molasse | ||||
Stratigraphy comments: "Based on bio- and magnetostratigraphic data, SP 618 is c. 16.1–16.2 m.y. old (late Early Miocene)" |
Lithology and environment
Primary lithology: | fine,medium sandstone | ||
Secondary lithology: | paleosol/pedogenic,gray,green siltstone | ||
Lithology description: The OSM sediments of SP consist of fine to medium-grained sandstones and grey to greenishmottled silts and clays with pedogenetic overprint. | |||
Environment: | fluvial indet. | Tectonic setting: | foreland basin |
Geology comments: Charophytes and freshwater gastropods are very rare and fish remains are completely absent. In contrast, remains of terrestrial vertebrates are abundant and generally well preserved. Thus, the fossil biota clearly indicates that SP 618 represents a terrestrial deposit, most likely a palaeo-soil. Fossorial/subterranean reptiles (Anguis sp., Amphisbaenidae indet.), together with the salamander, suggest that the soil was well oxygenated and well drained, which implies the nearby presence of a river and a humid climate. On the other hand, heliophilic taxa (Ophisaurus sp., Lacertidae indet.) point to open and drier habitats nearby. Their co-occurrence with fossorial/subterranean taxa can perhaps be explained by invoking deposition in raptor pellets, as discussed above for the mammalian tooth sample. The composition of the small-mammal fauna is comparable to those known from lake deposits such as Le Locle Sous le Stand C-13 (MN 7, Kälin et al., 2001) or Mauensee (MN 4b, Reichenbacher et al., 2005). The Upper Freshwater Molasse in general represents a large river system. |
Taphonomy
Modes of preservation: | body |
Size of fossils: | macrofossils,mesofossils |
Collection methods and comments
Reason for describing collection: | general faunal/floral analysis |
Taxonomic list comments:Also reported but given no taxonomic name are "seeds and other remains". |
Metadata
Database number: | 201974 | ||
Authorizer: | T. Cleary | Enterer: | T. Cleary |
Modifier: | T. Cleary | ||
Created: | 2019-06-13 12:22:28 | Last modified: | 2019-06-18 04:16:33 |
Access level: | the public | Released: | 2019-06-13 12:22:28 |
Creative Commons license: | CC BY |
Reference information
Primary reference:
69177. | J. Jost, D. Kälin, S. Börner, D. Vasilyan, D. Lawver and B. Reichenbacher. 2015. Vertebrate microfossils from the Upper Freshwater Molasse in the Swiss Molasse Basin: Implications for the evolution of the North Alpine Foreland Basin during the Miocene Climate Optimum. Palaeogeography, Palaeoclimatology, Palaeoecology 426:22-33 [T. Cleary/T. Cleary] |