PhotosLocation


donguz+gorizont Latitude and Longitude:

51°30′N 55°12′E / 51.5°N 55.2°E / 51.5; 55.2
From Wikipedia, the free encyclopedia
(Redirected from Donguz Gorizont)
Donguz Formation
Stratigraphic range: Anisian
~247–242  Ma
O
S
D
C
P
T
J
K
N
Eryosuchus, an index fossil of the Donguz
Type Stratigraphic Formation
Underlies Bukobay Svita [1]
Overlies Petropavlovskaya Svita ( Yarenskian Gorizont)
Lithology
Primary Sandstone
Other Claystone, conglomerate
Location
Coordinates 51°30′N 55°12′E / 51.5°N 55.2°E / 51.5; 55.2
Approximate paleocoordinates 33°36′N 43°12′E / 33.6°N 43.2°E / 33.6; 43.2
Region Bashkortostan
Orenburg Oblast
CountryRussia
Type section
Named for Donguz River
Donguz Formation is located in Russia
Donguz Formation
Donguz Formation (Russia)

The Donguz Formation, Donguz Svita, or Donguz Rocks ( Russian: Донгузские скалы) is a Middle Triassic geological formation that crops out on the right bank of Donguz River in Orenburg Oblast, Russia, across the settlement of Pervomaisky. The formation is equivalent to a biostratigraphic unit, the Donguz Gorizont. It is famous for its rich collection of the fossils of Middle Triassic tetrapods. [2] [1] [3]

It is a nature monument (особо охраняемых природных территорий (ООПТ)). [4]

Fossil content

The following fossils have been found in the Donguz Formation: [1]

See also

References

  1. ^ a b c Lucas, Spencer G (1 November 1998). "Global Triassic tetrapod biostratigraphy and biochronology". Palaeogeography, Palaeoclimatology, Palaeoecology. 143 (4): 347–384. Bibcode: 1998PPP...143..347L. CiteSeerX  10.1.1.572.872. doi: 10.1016/S0031-0182(98)00117-5.
  2. ^ Sennikov, A.G. (29 February 1996). "Evolution of the Permian and Triassic tetrapod communities of Eastern Europe". Palaeogeography, Palaeoclimatology, Palaeoecology. 120 (3–4): 331–351. Bibcode: 1996PPP...120..331S. doi: 10.1016/0031-0182(95)00041-0.
  3. ^ область&objregion=Оренбургский район
  4. ^ Uraloved.ru

donguz+gorizont Latitude and Longitude:

51°30′N 55°12′E / 51.5°N 55.2°E / 51.5; 55.2
From Wikipedia, the free encyclopedia
(Redirected from Donguz Gorizont)
Donguz Formation
Stratigraphic range: Anisian
~247–242  Ma
O
S
D
C
P
T
J
K
N
Eryosuchus, an index fossil of the Donguz
Type Stratigraphic Formation
Underlies Bukobay Svita [1]
Overlies Petropavlovskaya Svita ( Yarenskian Gorizont)
Lithology
Primary Sandstone
Other Claystone, conglomerate
Location
Coordinates 51°30′N 55°12′E / 51.5°N 55.2°E / 51.5; 55.2
Approximate paleocoordinates 33°36′N 43°12′E / 33.6°N 43.2°E / 33.6; 43.2
Region Bashkortostan
Orenburg Oblast
CountryRussia
Type section
Named for Donguz River
Donguz Formation is located in Russia
Donguz Formation
Donguz Formation (Russia)

The Donguz Formation, Donguz Svita, or Donguz Rocks ( Russian: Донгузские скалы) is a Middle Triassic geological formation that crops out on the right bank of Donguz River in Orenburg Oblast, Russia, across the settlement of Pervomaisky. The formation is equivalent to a biostratigraphic unit, the Donguz Gorizont. It is famous for its rich collection of the fossils of Middle Triassic tetrapods. [2] [1] [3]

It is a nature monument (особо охраняемых природных территорий (ООПТ)). [4]

Fossil content

The following fossils have been found in the Donguz Formation: [1]

See also

References

  1. ^ a b c Lucas, Spencer G (1 November 1998). "Global Triassic tetrapod biostratigraphy and biochronology". Palaeogeography, Palaeoclimatology, Palaeoecology. 143 (4): 347–384. Bibcode: 1998PPP...143..347L. CiteSeerX  10.1.1.572.872. doi: 10.1016/S0031-0182(98)00117-5.
  2. ^ Sennikov, A.G. (29 February 1996). "Evolution of the Permian and Triassic tetrapod communities of Eastern Europe". Palaeogeography, Palaeoclimatology, Palaeoecology. 120 (3–4): 331–351. Bibcode: 1996PPP...120..331S. doi: 10.1016/0031-0182(95)00041-0.
  3. ^ область&objregion=Оренбургский район
  4. ^ Uraloved.ru

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