28:
386:
293:
Shishkin, M.A.; Ochev, V.G.; Lozovskii, V.R.; Novikov, I.V. (2000). "Tetrapod biostratigraphy of the
Triassic of Eastern Europe". In Benton, M.J.; Shishkin, M.A.; Unwin, D.M.; Kurochkin, E.N. (eds.).
430:
214:), though there is some controversy over how the stratigraphy of the area should be defined. Thin exposures of Yarenskian units are also known further north in the
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91:). Others prefer to consider the Fedorovskian and Gamskian to be subgorizonts or members of the Yarenskian. Vertebrate
75:. Some paleontologists elevate the Yarenskian to a supergorizont and subdivide it into two smaller units: the older
320:"Differentiation of Tetrapod Communities and Some Aspects of Biotic Events in the Early Triassic of Eastern Europe"
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Tverdokhlebov, Valentin P.; Tverdokhlebova, Galina I.; Surkov, Mikhail V.; Benton, Michael J. (2003).
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Ochev, V.G.; Shishkin, M.A.; Kukhtinov, D.A.; Tverdokhlebov, V.P.; Makarova, I.S. (2004).
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includes coastal sediments equivalent to the
Yarenskian (such as the Bogdo or
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are more common in southern exposures while procolophonids and putative "
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Shishkin, M.A.; Sennikov, A.G.; Novikov, I.V.; Ilyina, N.V. (2006).
249:"Tetrapod localities from the Triassic of the SE of European Russia"
359:"Some Unsolved Problems of Triassic Stratigraphy in Eastern Europe"
319:
186:), a Fedorovskian-age assemblage in the Cis-Ural region (near the
142:, respectively. The Yarenskian as a whole is characterized by the
159:. A few geographical influence on the faunas can be observed;
297:. Cambridge: Cambridge University Press. pp. 140–159.
174:
The
Yarenskian encompasses several svitas (equivalent to
404:
124:. In the Gamskian, these index fossils are replaced by
178:). The most fossiliferous and best-exposed is the
194:). Another productive unit is the Gamskian-age
59:-age terrestrial sediments. It lies above the
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295:The Age of Dinosaurs in Russia and Mongolia
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363:Stratigraphy and Geological Correlation
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36:, an index fossil of the Yarenskian.
403:. You can help Knowledge (XXG) by
47:("Yarenskian Horizon") is a major
25:
480:European geologic formation stubs
152:, and has also been known as the
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171:" are more common in the north.
95:of the Fedorovskian include the
67:, and is located below a short
392:This article about a specific
1:
450:Geologic formations of Russia
265:10.1016/S0012-8252(02)00076-4
475:Geography of Orenburg Oblast
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379:
198:, which is found near the
455:Triassic System of Europe
336:10.1134/S0031030106010011
324:Paleontological Journal
184:Petropavlovka Formation
65:Vetlugian Supergorizont
55:corresponding to Upper
470:Paleontology in Russia
180:Petropavlovskaya Svita
37:
18:Petropavlovskaya Svita
253:Earth-Science Reviews
176:geological formations
77:Fedorovskian Gorizont
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196:Lipovskaya Formation
81:Fedorovkian Horizon
208:Caspian Depression
83:) and the younger
61:Ustmylian Gorizont
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212:Bogdinskaya Svita
85:Gamskian Gorizont
16:(Redirected from
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204:Volgograd Oblast
71:overlain by the
49:biostratigraphic
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465:Olenekian Stage
460:Triassic Russia
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399:in Europe is a
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192:Orenburg Oblast
182:(anglicized as
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133:Trematosaurus
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117:procolophonid
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155:Parotosuchus
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149:Parotosuchus
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109:
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69:unconformity
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33:Parotosuchus
31:
330:(1): 1–10.
259:(1): 1–66.
169:rauisuchids
101:Gnathorhiza
42:Yarenskian
444:Categories
234:References
188:Ural River
146:amphibian
144:capitosaur
397:formation
344:129895753
273:0012-8252
230:basins.
200:Don River
127:Ceratodus
121:Burtensia
57:Olenekian
220:Vychegda
115:and the
97:lungfish
51:unit in
44:Gorizont
228:Pechora
63:of the
342:
301:
271:
226:, and
216:Vyatka
206:. The
136:, and
53:Russia
340:S2CID
157:fauna
139:Kapes
401:stub
299:ISBN
269:ISSN
224:Luza
163:and
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332:doi
261:doi
202:in
190:in
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Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.
