Alai Beds Stratigraphic range: Ypresian (Bumbanian) ~ | |
---|---|
Type | Geological formation |
Overlies | Paleozoic rocks |
Thickness | More than 25 m (82 ft) |
Lithology | |
Primary | Siltstone, conglomerate |
Other | Limestone |
Location | |
Coordinates | 39°54′N69°30′E / 39.9°N 69.5°E Coordinates: 39°54′N69°30′E / 39.9°N 69.5°E |
Approximate paleocoordinates | 40°42′N69°42′E / 40.7°N 69.7°E |
Region | Osh |
Country | Kyrgyzstan |
Extent | Aktash Range |
The Alai Beds is an Early Eocene (Ypresian, or Bumbanian in the ALMA classification) geologic formation in the Osh Region of southwestern Kyrgyzstan. The formation has provided many fossils of mammals, lizards, turtles and snakes. [1]
The Paleogene Alai Beds have a limited distribution, and are restricted to the northern slope of Aktash Range, formed by Paleozoic rocks, which is one of the foothills of the Turkestan Range. The Paleogene deposits on the Aktash Range are badly exposed, they can be observed only in three outcrops, separated by short distances about 1 to 2 kilometres (0.62 to 1.24 mi). Despite of their close position, the Paleogene deposits in these outcrops are varied greatly in composition and thickness of layers. [2]
The lower Alai Beds contain 5 metres (16 ft) of silts and siltstones, and the upper part comprises oyster-bearing limestones of which 2 to 3 metres (6 ft 7 in to 9 ft 10 in) 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 25 metres (82 ft) of visible thickness) with some horizons of oyster-bearing conglomerates. [3]
The formation has provided the following fossils: [1]
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