Mississippian-Lower Pennsylvanian foraminifers from the Sierra Nacimiento and San Pedro Mountains, North-Central New Mexico, USA - 31/05/25

Doi : 10.1016/j.geobios.2024.11.009

Karl Krainer ^a,^⁎ , Spencer G. Lucas ^b, Daniel Vachard ^c,^{^{1
Deceased.}}
^a Institute of Geology, University of Innsbruck, Innrain 52, A-6020 Innsbruck, Austria
^b New Mexico Museum of Natural History, 1801 Mountain Road N.W., Albuquerque, NM 87104, USA
^c Collegial and International Research Center of Active Seniors (CIRCAS), 1 rue des Tilleuls, 59152 Gruson, France

^⁎Corresponding author.

Sous presse. Épreuves corrigées par l'auteur. Disponible en ligne depuis le Saturday 31 May 2025
Cet article a été publié dans un numéro de la revue, cliquez ici pour y accéder

Highlights

•	Mississippian rocks in north-central New Mexico, USA, are a thin succession of marine and nonmarine strata.
•	These are rocks of the Arroyo Peñasco and Log Springs formations.
•	The marine strata of the Espiritu Santo Member of the Arroyo Peñasco Formation include age-diagnostic foraminifers of early and late Tournaisian ages.
•	Reworked clasts in the base of the Log Springs Formation contain foraminifers of Visean age.
•	Analysis of thin sections identifies Mississippian depositional environments in north-central New Mexico that ranged from nonmarine fluvial to normal marine settings.

Le texte complet de cet article est disponible en PDF.

Abstract

In the Sierra Nacimiento-San Pedro Mountains-Jemez Mountains of north-central New Mexico (USA), the thin succession of Mississippian sediments is termed the Arroyo Peñasco Formation, overlain by the Log Springs Formation. The Arroyo Peñasco Formation is subdivided into Del Padre Member composed of siliciclastic sediments and the overlying Espiritu Santo Member composed of carbonate sediments. Foraminifers of the Espiritu Santo Member at Lion Spring in the northern San Pedro Mountains indicate a Tournaisian age. The lower Tournaisian (= Hastarian = biozones MFZ1-4 of Poty et al., 2006 [Geological Magazine 143, 829–857]) is locally characterized by Septaglomospiranella ex gr. primaeva, Septabrunsiina minuta and Tournayella sp. The upper Tournaisian (= Ivorian = biozones MFZ5-9 of Poty et al., 2006) is characterized by Spinoendothyra, Inflatoendothyra and Tuberendothyra. In the Sierra Nacimiento-San Pedro Mountains-Jemez Mountains, the sediments of the Arroyo Peñasco Group are unconformably overlain by nonmarine redbeds of the Log Springs Formation (Serpukhovian/upper Chesterian). Some of the carbonate clasts of the basal conglomerate of the Log Springs Formation at Lion Spring contain late early Viséan (biozone MFZ11B of Poty et al., 2006) foraminifers and algae, including Koninckopora and Paraarchaediscus. These carbonate clasts are reworked from the underlying Arroyo Peñasco Formation (Espiritu Santo Member). In north-central New Mexico, a transgression during the Early Pennsylvanian (Morrowan) caused deposition of the shallow marine sediments of the Osha Canyon Formation. The Morrowan age of the Osha Canyon Formation is based on Nigrispiroides nov. gen., Iriclinella, Globivalvulina, and Millerella.