Mizur Formation

The Fytyn member represent the older layers of the formation, and depending on the outcrop, it overlies the eroded surface of Paleozoic granites or crystalline schists, or the Sinemurian–lower Pliensbachian volcanosedimentary rocks of the Sadon Formation.{{cite journal |last1=Panov |first1=D.I. |title=Stratigraphy of the Lower and Middle Jurassicrocks in the central North Caucasus (Digor–Ossetia zone) |journal=Byull. Mosk. O-va Ispyt. Prir., Otd. Geol. |date=1997 |volume=72 |issue=5 |pages=46–55}} This member is composed mostly of the product of the regional erosion of older layers — conglomerates, gravelstones, quartz sandstones, and others — that were deposited in a mostly continental setting. It is up to a few dozen meters thick.

In some outcrops the Fytyn Member is absent, as result of a regional uplift, with the sedimentary material transported from this area to central parts of the Greater Caucasus. Such material ended up accumulating on the Kistin Formation (Sinemurian–lower Pliensbachian), a unit that underlies in some sections the Faraskat Member. The Faraskat section began its deposition when the local layers were accompanied by a slow subsidence of the land and sedimentation on the previously denuded area.{{cite book |last1=SSSR |first1=Paleogeografiya |title=Ob"yasnitel'naya zapiska k atlasu li-tologo-paleogeograficheskikh kart SSSR (Paleogeography of the Soviet Union: Explanatory Note to the Atlas of Litho-logic–Paleogeographic Maps of the Soviet Union) |date=1975 |publisher=Nedra |location=Moscow}} The Faraskat sequence represents the first proper coastal deposit in the unit and is composed by a mixture of coarse material, as well as wood fragments and siderite, with some layers being highly bioturbated.

The transition between the Faraskat and Mizur members is gradual, forming a large sedimentary cycle from clayey to sandstone-dominated rocks. This layer represents the last unit of the formation and is dominated by fine-grained sandstone horizons, often low-angle crossbedding and scarce fine ripple marks, in contrast to the abundant large wave ripples. This layers have abundant fragments of terrestrial vegetation in a highly oxidized state. The sedimentation peculiarities of the Mizur layers indicate their accumulation within a relatively wide and shallow shelf. This layer is the only that has provided dinosaur footprints, as well ammonites and other invertebrates.

The Mizur Member contains numerous fragments of plants — stems, wood, and leaves — suggesting a clear influence of nearby emerged settings. The vegetation in the coeval exposures along the Caucasus and adjacent regions were covered by coniferous forests with abundant underliying Bennettitales.{{cite journal |last1=Vakhrameev |first1=V.A. |last2=Vasina |first2=R.A. |title=The Lower Jurassic and Aalenian f lora in the North Caucasus |journal=Paleontol. Zh. |date=1959 |volume=3 |issue=1 |pages=125‒133}} The spores and pollen in the sediments are dominated by bennettitales, which likely grew on nearshore lowlands.{{cite journal |last1=Vakhrameev |first1=V.A. |last2=Krasilov |first2=V.A. |title=The Domerian f lorain the North Caucasus |journal=Paleontol. Zh. |date=1961 |volume=3 |issue=1 |pages=103–108}} The region hosts pollen of several plant groups, notably the Pinaceae, Podocarpaceae, Araucariaceae, with other such as Ginkgoaceae being less common. Beyond trees, the lowlands were covered by thermophilic ferns (Cibitium, Mattonia, Coniopteris), lycophytes (Selaginella), and horsetails (Neocalamites). Invertebrate faunas are linked with the Mediterranean faunal region, with isotope ratios in some specimens (belemnites and brachiopods) yielding estimated average annual temperatures in the North Caucasian–Transcaucasian region of 21.4–23.5 °C; that is, a subtropical humid climate.{{cite journal |last1=Yasamanov |first1=N.A. |title=Temperatures in the habitat of Jurassic–Cretaceous brachiopods, cephalopods, and bivalve mol-luscs in the western Transcaucasian basin |journal=Geokhimiya |date=1973 |volume=5 |issue=2–3 |page=746‒754}}{{cite book |last1=Yasamanov |first1=N.A . |title=Landshaftno-klimaticheskie usloviyayury, mela i paleogena Yuga SSSR (Jurassic, Cretaceous,and Paleogene Landscape-Climate Conditions in theSouthern Soviet Union) |date=1978 |publisher=Nedra |location=Moscow}}

• List of fossiliferous stratigraphic units in Russia
• Sorthat Formation, Denmark
• Neringa Formation, Lithuania
• Pliensbachian formations
• Blanowice Formation, Southern Poland
• Clarens Formation, South Africa
• Fernie Formation, Canada
• Hasle Formation, Denmark
• Kota Formation, India
• Los Molles Formation, Argentina
• Mawson Formation, Antarctica
• Rotzo Formation, Italy
• Whiteaves Formation, British Columbia
• Navajo Sandstone, Utah
• Kandreho Formation, Madagascar
• Kota Formation, India
• Cattamarra Coal Measures, Australia

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Category:Geologic formations of Russia

Category:Jurassic System of Asia

Category:Jurassic Russia

Category:Pliensbachian Stage

Category:Sandstone formations

Category:Coal formations