Jump to content

Muleros Formation

From Wikipedia, the free encyclopedia

This is an old revision of this page, as edited by Kent G. Budge (talk | contribs) at 02:03, 21 October 2020 (Descriptiom: sp). The present address (URL) is a permanent link to this revision, which may differ significantly from the current revision.

Muleros Formation
Stratigraphic range: Albian
TypeFormation
UnderliesMesilla Valley Formation
OverliesSmeltertown Formation
Thickness106 feet (32 m)
Location
Coordinates31°47′39″N 106°32′35″W / 31.7940792°N 106.5430513°W / 31.7940792; -106.5430513
RegionNew Mexico
CountryUnited States
Type section
Named forCerro de Muleros (now Cerro de Cristo Rey)
Named byW.S. Strain
Year defined1976
Muleros Formation is located in the United States
Muleros Formation
Muleros Formation (the United States)
Muleros Formation is located in New Mexico
Muleros Formation
Muleros Formation (New Mexico)

The Muleros Formation is a geologic formation in New Mexico.[1] It preserves fossils dating back to the early Cretaceous period.[2]

Descriptiom

The formation consists of highly fossiliferous nodular argillaceous limestone at its base and in its upper portion, with shale dominating the middle section and interbedding with the limestone towards the top of the formation. Total thickness is 106 feet (32 m). The formation conformably overlies the Smeltertown Formation and grades into the overlying Mesilla Valley Formation.[2]

The formation is interpreted as an outer shelf formation that later experienced shallowing and deposition of limestone in an inner shelf environment subject to storm influence, then deepened again to deposit shale with some storm layers.[3]

Fossils

The formation contains at least 20 genera and 23 species of fossils. These include the molluscs Lima wacoensis Roemer, Lima mexicana Bose, Pecten texanus var. elongatus Bose, Pecten subalpinus Bose, Plicatula incongrua Conrad, Ostrea quadriplicata (Shumard), Texigryphaea washitaensis. Trigonia emery Conrad, Helicocryptus mexicanus Bose, and Turritella granulata Sowerby var. cenomanensis d'Orbigny and the echinoderm Heteraster bravoensis (Bose). These are characteristic of the Albian age.[1] The formation is highly fossiliferous, with some beds consisting almost entirely of fossils of the oyster Texigryphaea washitaensis.[2]

History of investigation

The beds making up the formation were first described by E. Bose in 1906 as subdivision 5 of his stratigraphic section.[1] W.S. Strain assigned the name Muleros Formation to this subdivision in 1976.[2]

See also

Footnotes

  1. ^ a b c Bose 1906
  2. ^ a b c d Strain 1976
  3. ^ Lucas et al. 2010

References

  • Bose, E. (1906). "Excursion au Cerro de Muleros". International Geological Congress 10, Guide for Excursion. 20.
  • Lucas, Spencer; Krainer, Karl; Spielmann, Justin; Durney, Kevin (2010). "Cretaceous stratigraphy, paleontology, petrography, depositional environments, and cycle stratigraphy at Cerro de Cristo Rey, Doña Ana County, New Mexico". New Mexico Geology. 32: 103–130. Retrieved August 5, 2020.
  • Strain, W.S. (1976). "New formation names in the Cretaceous at Cerro de Cristo Rey, Dona Ana County, New Mexico; Appendix 2" (PDF). New Mexico Bureau of Mines and Mineral Resources Memoir. 31: 77–82. Retrieved August 5, 2020.