Caballero Formation

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Caballero Formation
Stratigraphic range: Tournaisian
TypeFormation
UnderliesLake Valley Limestone
OverliesPercha Shale
Lithology
PrimaryLimestone
OtherShale
Location
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RegionNew Mexico
CountryUnited States
Type section
Named byL.R. Laudon and A.L. Bowsher
Year defined1941

The Caballero Formation is a geologic formation found in the highlands flanking the southern Rio Grande River valley in New Mexico. It preserves fossils dating back to the Tournasian Age of the Carboniferous period.[1]

Description

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The Caballero Formation consists of nodular gray argillaceous limestone, which grades upward into nodular gray marl with shale lenses. It rests conformably on the Percha Shale and is overlain unconformably by the Lake Valley Limestone. The formation likely correlates with the Chouteau Limestone of the upper Mississippi valley.[1]

Fossils

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The formation is locally abundant in fossils of Tournasian age,[1] with more than 200 marine invertebrate species reported.[2] These include the ammonoids Pericyclus blairi, P. Cooperi P. costulatus, and Gattendorfia bransoni as well as Tournasian conodont and brachiopod faunas.[3] The fauna changes significantly from the westernmost to easternmost exposures of the formation.[2]

History of investigation

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The beds forming this unit were originally included in the Devonian Percha Shale, but were separated into their own formation by Laudon and Bowsher in 1941, when it was recognized that they are Mississippian in age.[1]

See also

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References

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