Biostratigraphy of Guadalupian (Mid­dle Permian) am­mo­noids from the Olinalá For­ma­tion, southern Mex­i­co

Authors

  • Alberto Alanis Pavón Posgrado en Ciencias del Mar y Limnología, Universidad Nacional Autónoma de México, Ciudad Universitaria, 04510, Alcaldía Coyoacán, México City (México) Author https://orcid.org/0009-0007-0767-3231
  • Martin Guerrero-Suastegui Escuela Superior de Ciencias de la Tierra, Universidad Autónoma de Guerrero, Ex-Hacienda de San Juan Bautista, S/N, Taxco el Viejo, Guerrero (México) Author https://orcid.org/0009-0000-5226-281X
  • Edgar Juárez-Arriaga Instituto de Geociencias, Universidad Nacional Autónoma de México, Querétaro, Qro., 76230 (México) Author https://orcid.org/0000-0002-3010-0788
  • Miguel Angel Torres-Martínez Departamento de Paleontología, Instituto de Geología, Av. Universidad 3000, Circuito de la Investigación Científica, Universidad Nacional Autónoma de México, 04510, Alcaldía Coyoacán, Mexico City (Mexico) Author https://orcid.org/0000-0002-9322-0429
  • Josep Anton Moreno-Bedmar Departamento de Paleontología, Instituto de Geología, Av. Universidad 3000, Circuito de la Investigación Científica, Universidad Nacional Autónoma de México, 04510, Alcaldía Coyoacán, Mexico City (Mexico) Author https://orcid.org/0000-0001-8426-2750

DOI:

https://doi.org/10.2110/

Keywords:

ammonoids, Middle Permian, Guadalupian, Olinalá Formation, biostratigraphy

Abstract

An am­mo­noid biostratigraphic analysis was conducted for the Permian Olinalá For­ma­tion, Guer­rero state, southern Mex­i­co. Bed-by-bed sampling yielded 113 am­mo­noids belonging to 14 dif­fer­ent taxa. The biostratigraphic analysis allowed us to identify two am­mo­noid Zones: Paraceltites ele­gans and Coahuiloceras sp., and one subzone: Pseudagathiceras spinosum. According to the GSSP-de­fined boundaries, these biostratigraphic zones extend from the Roadian-Wordian to the lower Cap­i­ta­ni­an interval. To support the biostratigraphic analysis, several key taxa were reviewed from a taxonomic per­spective. This taxonomic assessment validated the genus Coahuiloceras. A quantitative analysis based on morphometric ratios of the species of the genera Timorites and Coahuiloceras reveals a clear di­ver­gence between both groups. In addition, the biostratigraphic framework of the Olinalá succession is compared with previously published biostratigraphic data from Sonora, Coahuila and Texas, high­light­ing similarities and differences among these areas. The identified fauna in the Olinalá For­ma­tion is main­ly associated with the Amer­i­can Realm.

CG2606

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Published

2026-02-28

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Section

Articles

How to Cite

Biostratigraphy of Guadalupian (Mid­dle Permian) am­mo­noids from the Olinalá For­ma­tion, southern Mex­i­co. (2026). Carnets Geol., 26, 125-150. https://doi.org/10.2110/