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Baruungoyot Formation

Geological formation in Mongolia From Wikipedia, the free encyclopedia

Baruungoyot Formationmap
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The Baruungoyot Formation (also known as Barun Goyot[1]) is a geological formation dating to the Late Cretaceous Period. It is located within and is widely represented in the Gobi Desert Basin, in the Ömnögovi Province of Mongolia.

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Description

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Khulsan in 1970

It was previously known as the Lower Nemegt Beds occurring beneath the Nemegt Formation and above the Djadokhta Formation. It has been suggested that the Djadokhta and Baruungoyot Formations are lower and upper parts, respectively, of the same lithological unit and the boundary between the two does not exist. The stratotype of the Baruungoyot Formation is the Khulsan locality, east of Nemegt. At Nemegt, only the uppermost barungoyotian beds are visible. The Red Beds of Khermeen Tsav are also considered part of the Baruungoyot Formation. It is approximately 110 metres (360 ft) in thickness,[2] and was laid down roughly 72-71 million years ago. Given the new date for the start of the Maastrichtian (72.1 MYA) a basal Maastrichtian age seems probable. The Baruungoyot Formation preserves an environment of sand dunes, created from wind-eroded rocks (aeolian dunes).

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Paleobiota of the Baruungoyot Formation

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Taxon Reclassified taxon Taxon falsely reported as present Dubious taxon or junior synonym Ichnotaxon Ootaxon Morphotaxon
Notes
Uncertain or tentative taxa are in small text; crossed out taxa are discredited.

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Panoramic view of the Hermiin Tsav locality of the Barun Goyot Formation

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