Khatyspyt Formation Explained

Khatyspyt Formation
Age:Neoproterozoic
Type:Geological formation
Unitof:Olenëk Uplift
Underlies:Turkut Formation
Overlies:Mastakh Formation
Location:Siberia

The Khatyspyt Formation is a Neoproterozoic formation exposed in the Olenëk Uplift of north central Siberia,which contains the only known instance of the Ediacara biota preserved in a limestone bed. The Khatyspyt Formation forms one of the major parts of the Khorbusuonka Group; underlying the Khatyspyt are dolomites of the Mastakh Formation and their overlying red beds; the Turkut Formation overlies the Khatyspyt. The Khatyspyt and part of the overlying Turkut comprise a major shallowing upward marine carbonate sequence. [1] Khatyspytia is named after this formation.[2]

Notes and References

  1. Knoll. Andrew H.. John P. Grotzinger . Alan J. Kaufman . Petr Kolosov . Integrated approaches to terminal Proterozoic stratigraphy: an example from the Olenek Uplift, northeastern Siberia. Precambrian Research. 1995. 73. 1–4 . 251–270. 10.1016/0301-9268(94)00081-2. 11539551 . 1995PreR...73..251K .
  2. Grazhdankin, Dima . 2004 . Patterns of distribution in the Ediacaran biotas: facies versus biogeography and evolution . 30 . 2 . 203–221 . 10.1666/0094-8373(2004)030<0203:PODITE>2.0.CO;2 . 0094-8373 . Paleobiology . 129376371 .