Alai Beds
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The Alai Beds is an
Early Eocene In the geologic timescale the Ypresian is the oldest age or lowest stratigraphic stage of the Eocene. It spans the time between , is preceded by the Thanetian Age (part of the Paleocene) and is followed by the Eocene Lutetian Age. The Ypresian i ...
(
Ypresian In the geologic timescale the Ypresian is the oldest age (geology), age or lowest stage (stratigraphy), stratigraphic stage of the Eocene. It spans the time between , is preceded by the Thanetian Age (part of the Paleocene) and is followed by th ...
, or
Bumbanian The Bumbanian is an Asian Land Mammal Age (ALMA), a large biozone which corresponds to ages between 55.8–46.8 Ma for finds of fossil mammals in Asia. This zone lies within the Ypresian stage of the Eocene The Eocene ( ) Epoch is a geological ...
in the ALMA classification)
geologic formation A geological formation, or simply formation, is a body of rock having a consistent set of physical characteristics ( lithology) that distinguishes it from adjacent bodies of rock, and which occupies a particular position in the layers of rock exp ...
in the
Osh Region Osh Region ( ky, Ош облусу, translit=Osh oblusu; russian: Ошская область, Oshskaya oblast) is a region (''oblast'') of Kyrgyzstan. Its capital is Osh, which is not part of the region. It is bounded by (clockwise) Jalal-Abad Re ...
of southwestern
Kyrgyzstan Kyrgyzstan,, pronounced or the Kyrgyz Republic, is a landlocked country in Central Asia. Kyrgyzstan is bordered by Kazakhstan to the north, Uzbekistan to the west, Tajikistan to the south, and the People's Republic of China to the east. ...
. The formation has provided many
fossil A fossil (from Classical Latin , ) is any preserved remains, impression, or trace of any once-living thing from a past geological age. Examples include bones, shells, exoskeletons, stone imprints of animals or microbes, objects preserved ...
s of
mammal Mammals () are a group of vertebrate animals constituting the class Mammalia (), characterized by the presence of mammary glands which in females produce milk for feeding (nursing) their young, a neocortex (a region of the brain), fur or ...
s,
lizard Lizards are a widespread group of squamate reptiles, with over 7,000 species, ranging across all continents except Antarctica, as well as most oceanic island chains. The group is paraphyletic since it excludes the snakes and Amphisbaenia alt ...
s,
turtle Turtles are an order of reptiles known as Testudines, characterized by a special shell developed mainly from their ribs. Modern turtles are divided into two major groups, the Pleurodira (side necked turtles) and Cryptodira (hidden necked tu ...
s and
snake Snakes are elongated, Limbless vertebrate, limbless, carnivore, carnivorous reptiles of the suborder Serpentes . Like all other Squamata, squamates, snakes are ectothermic, amniote vertebrates covered in overlapping Scale (zoology), scales. Ma ...
s.Alai Beds
at
Fossilworks Fossilworks is a portal which provides query, download, and analysis tools to facilitate access to the Paleobiology Database The Paleobiology Database is an online resource for information on the distribution and classification of fossil animals ...
.org


Description

The Paleogene Alai Beds have a limited distribution, and are restricted to the northern slope of Aktash Range, formed by
Paleozoic The Paleozoic (or Palaeozoic) Era is the earliest of three geologic eras of the Phanerozoic Eon. The name ''Paleozoic'' ( ;) was coined by the British geologist Adam Sedgwick in 1838 by combining the Greek words ''palaiós'' (, "old") and ' ...
rocks, which is one of the foothills of the
Turkestan Range One of the northern extensions of the Pamir-Alay system, the Turkestan Range (russian: Туркестанский хребет; ky, Түркстан кырка тоосу; uz, Туркистон тизмаси, Turkiston tizmasi; tg, Қатор ...
. The Paleogene deposits on the Aktash Range are badly exposed, they can be observed only in three
outcrop An outcrop or rocky outcrop is a visible exposure of bedrock or ancient superficial deposits on the surface of the Earth. Features Outcrops do not cover the majority of the Earth's land surface because in most places the bedrock or superficial ...
s, separated by short distances about . Despite their close position, the Paleogene deposits in these outcrops are varied greatly in composition and thickness of layers.Averianov, 1994a, p.399 The lower Alai Beds contain of silts and siltstones, and the upper part comprises
oyster Oyster is the common name for a number of different families of salt-water bivalve molluscs that live in marine or brackish habitats. In some species, the valves are highly calcified, and many are somewhat irregular in shape. Many, but not al ...
-bearing
limestone Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms whe ...
s of which are exposed. At the base of the Upper Alai Beds there is a layer of conglomerate which produces a number of marine vertebrates, but a few terrestrial vertebrates including mammals. The section I1 is more complete and has a greater thickness, but produces a few shark teeth only. The third Paleogene section, where the mammal bearing locality Andarak 2 is located, has a much greater thickness of sands of the lower Alai Beds (more than of visible thickness) with some horizons of oyster-bearing conglomerates.Averianov, 1994a, p.400


Fossil content

The formation has provided the following fossils:


Mammals

;Artiodactyls * '' Eolantianius russelli'' * '' Diacodexis sp.'' * Diacodexeidae indet. ;Cimolesta * '' Metasarcodon udovichenkoi''Averianov, 1994b * '' Nuryctes alayensis''Lopatin & Averianov, 2004 * Palaeoryctidae indet.Lopatin, 2006 ;Hyaenodonta * '' Isphanatherium ferganensis''Lavrov & Averianov, 1998 * '' Neoparapterodon sp.'' ;Lipotyphla * '' Protogalericius averianovi'' ;Perissodactyls * '' Eoletes tianshanicus'' * '' Pataecops minutissimus''Averianov, 1994b * '' Sharamynodon kirghisensis'' * '' Teleolophus medius'' ;Rodents * '' Aktashmys montealbus''Averianov, 1994a, p.406Averianov & Lopatin, 2005 * '' Alaymys ctenodactylus''Averianov, 1994a, p.401 * '' Anatolimys rozhdestvenskii''Averianov, 1994a, p.402 * '' Gobiolagus hekkeri''Lopatin & Averianov, 2006 * '' Khodzhentia vinogradovi'' * '' Advenimus cf. burkei'' * '' Petrokozlovia cf. notos'' * '' Saykanomys cf. bohlini'' * '' ?Adolomys sp.'' * Ctenodactyloidea indet.Averianov & Danilov, 1996a


Reptiles

;Lizards * '' ?Saniwa sp.''Averianov & Danilov, 1997 * Agamidae indet.Averianov & Danilov, 1996b * Uromastycinae indet. ;Snakes * '' Calamagras turkestanicus''Danilov & Averianov, 1999 * '' Palaeophis ferganicus'' * Boidae indet. ;Turtles * '' Hadrianus vialovi''Averianov & Godinot, 2005Danilov & Averianov, 1999 * Cheloniinae indet.Averianov, 2002


See also

* Ypresian formations **
Ieper Group The Ieper Group ( nl, Ieper Groep; french: Groupe d'Ypres) is a group of rock strata in the subsurface of northwest Belgium. The group is subdivided into three marine formations, all formed during the Ypresian, a single age of the geologic timesc ...
of Belgium **
Fur Formation The Fur Formation is a marine geological formation of Ypresian (Lower Eocene Epoch, c. 56.0-54.5 Ma) age which crops out in the Limfjord region of Denmark from Silstrup via Mors and Fur to Ertebølle, and can be seen in many cliffs and quarries in ...
of Denmark **
London Clay Formation The London Clay Formation is a marine geological formation of Ypresian (early Eocene Epoch, c. 56–49 million years ago) age which crops out in the southeast of England. The London Clay is well known for its fossil content. The fossils from th ...
of England ** Silveirinha Formation of Portugal * Wasatchian formations **
Nanjemoy Formation The Nanjemoy Formation is a geologic formation pertaining to both the Wilcox Group and the Pamunkey Group of the eastern United States, stretching across the states of Virginia, Maryland, and District of Columbia. The formation crops out east of ...
of the eastern United States **
Wasatch Formation The Wasatch Formation (Tw)Shroba & Scott, 2001, p.3 is an extensive highly fossiliferous geologic formation stretching across several basins in Idaho, Montana Wyoming, Utah and western Colorado.Itaboraian formations **
Itaboraí Formation The Itaboraí Formation ( pt, Formação Itaboraí) is a highly list of fossiliferous stratigraphic units in Brazil, fossiliferous geologic Formation (geology), formation and LagerstätteKellner & Campos, 1999, p.399 of the Itaboraí Basin in Rio ...
of Brazil **
Laguna del Hunco Formation The Laguna del Hunco Formation or Laguna del Hunco Tuff ( es, Formación Laguna del Hunco, Tufolitas Laguna del Hunco) is a localized Early Eocene (Itaboraian in the SALMA classification) fossiliferous geological formation of the Cañadón Asfalto ...
of Argentina


References


Bibliography

* * * * * * * * * * * * * * * {{cite journal , last=Averianov , first=A. O , year=1994b , title=A new species of ''Sarcodon'' (Mammalia, Palaeoryctoidea) from the Lower Eocene of Kirgizia , journal=
Geobios Geobios is an academic journal published bimonthly by the publishing house Elsevier. Geobios is an international journal of paleontology, focusing on the areas of palaeobiology, palaeoecology, palaeobiogeography, stratigraphy and biogeochemistry ...
, volume=27 , pages=255-258 Geologic formations of Kyrgyzstan Paleogene System of Asia Ypresian Stage Conglomerate formations Siltstone formations Shallow marine deposits Fossiliferous stratigraphic units of Asia Paleontology in Kyrgyzstan Formations