Gorny Luch farmstead: Rupelian, Russian Federation
collected by Vadim Kitain
List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
Cephalopoda
- Myopsida
- Loliginidae
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Loligo sp.
Schneider 1784
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Gastropoda
- Opisthobranchiata
- Cavoliniidae
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Vaginella sp.
Daudin 1800
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Gastropoda
- Opisthobranchiata
- Limacinidae
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Limacina sp.
Bosc 1817
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Actinopteri
- Clupeiformes
- Clupeoidei
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Rupelia rata
(Daniltshenko 1959)
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= Rupelia rata
Daniltshenko 1959
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Kovalchuk et al. 2020 | |||||||||
Actinopteri
- Scombriformes
- Trichiuridae
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Preserved possibly in tentacles of Loligo | ||||||||||
Actinopteri
- Gadiformes
- Phycidae
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Protobrotula sobijevi
(Daniltshenko 1953)
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Actinopteri
- Gadiformes
- Merlucciidae
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Palaeogadus sp.
Von Rath 1859
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"Palaeogadus spp." | ||||||||||
Echinoidea
- Spatangoida
- Schizasteridae
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Schizaster sp.
Agassiz 1835
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"occasionally found" | ||||||||||
unclassified
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"remains of terrestrial plants" | ||||||||||
see common names |
Geography
Country: | Russian Federation | State/province: | Krasnodar Krai |
Coordinates: | 44.3° North, 39.8° East (view map) | ||
Paleocoordinates: | 38.6° North, 40.9° East (Wright 2013) | ||
Basis of coordinate: | stated in text | ||
Geographic resolution: | hand sample |
Time
Period: | Paleogene | Epoch: | Oligocene |
Stage: | Rupelian | 10 m.y. bin: | Cenozoic 4 |
Key time interval: | Rupelian | Nannofossil zone: | NP 21 |
Age range of interval: | 33.9 - 27.3 m.y. ago |
Stratigraphy
Formation: | Pshekha | Member: | Lower Maikop | ||
Stratigraphic resolution: | group of beds | ||||
Stratigraphy comments: "basal layers of the Lower Maikop deposits (Khadum, Pshekha Formation; Rupelian, nannoplankton zone NP 21)" |
Lithology and environment
Primary lithology: | gray lithified calcareous claystone |
Lithology description: "The lower part of the Pshekha Formation is composed of an alternation of dark grey weakly calcareous clays and light grey clays; the thickness of the interlayers varies from a few millimetres to several centimetres." "The squid was found in a dark grey laminated clay layer (which was formed under anoxic/hypoxic conditions)" | |
Environment: | coastal indet. |
Geology comments: "formed relatively close to the shore in a warm sea basin with alternating anaerobic and aerobic conditions at the bottom. The absence of deep sea fishes at the site of the squid discovery indicates a relatively small thickness of habitable water column
(probably the shelf)" |
Taphonomy
Modes of preservation: | body,soft parts,replaced with pyrite,replaced with carbon |
Size of fossils: | macrofossils |
Collection methods and comments
Collection methods: | observed (not collected) |
Reason for describing collection: | paleoecologic analysis |
Collectors: | Vadim Kitain |
Collection method comments: Borissiak Paleontological Institute of the Russian Academy of Sciences (PIN RAN, Moscow) with collection number PIN 5817 |
Metadata
Database number: | 226844 | ||
Authorizer: | P. Novack-Gottshall | Enterer: | P. Novack-Gottshall |
Created: | 2022-08-03 11:01:16 | Last modified: | 2025-02-22 15:12:02 |
Access level: | the public | Released: | 2022-08-03 11:01:16 |
Creative Commons license: | CC0 |
Reference information
Primary reference:
82322. | A. A. Mironenko, M. S. Boiko, A. F. Bannikov, A. I. Arkhipkin, V. A. Bizikov and M. Košťák. 2021. First discovery of the soft-body imprint of an Oligocene fossil squid indicates its piscivorous diet. Lethaia 54(5):793-805 [P. Novack-Gottshall/P. Novack-Gottshall] |
Secondary references:
82325 | O. Kovalchuk, E. Baykina, E., K. Stefaniak, and A. Nadachowsk. 2020. A systematic revision of herrings (Teleostei, Clupeidae, Clupeinae) from the Oligocene and early Miocene from the Eastern Paratethys and the Carpathian Basin. Journal of Vertebrate Paleontology 40(2):e1778710 [P. Novack-Gottshall/P. Novack-Gottshall] |