Geology of Sierra de la Pena and paleontology of the Indidura formation Coahuila, Mexico

Jones, Theodore S.

doi:10.1130/gsab-49-69

Cited by 31 publications

(31 citation statements)

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“…En Estados Unidos de Norteamérica esta especie ha sido reportada en el Albiano de Texas (Adkins, 1920;Cooke, 1953). En México, Heteraster texanus proviene del Aptiano (Adkins, 1928) y Albiano (Buitrón, 1973) de Colima, Chihuahua (Stanton, 1896;Böse, 1910;Böse y Cavins, 1927;Burckhardt, 1930;Durango (Kellum, 1956) (Kellum, 1956), el Cenomaniano inferior de Coahuila (Cotteau, 1890;Stanton, 1896;Böse, 1906;Cooke, 1955), Jalisco (Böse, 1906;Cooke, 1946), Chihuahua (Jones, 1938) (Kellum, 1956). et al, 1983, 2007) , Santoniano (Gallemi et al, 1983(Gallemi et al, , 2007, Campaniano (Gallemi et al, 1983) (Cooke, 1953).…”

Section: Discussionunclassified

“…Los primeros reportes sobre equinoideos fósiles en México fueron realizados por Schluter (1887), Böse (1913), Burckhardt (1930) y Jones (1938), Dumble (1895), quienes describen asociaciones fósiles de este grupo provenientes de rocas del Cretácico tardío de diferentes localidades de Coahuila y Chihuahua. Posteriormente, Maldonado-Koerdell (1953) reporta un cuadro de distribución estratigráfica y describe 25 especies de este grupo para el Aptiano de Puebla.…”

Section: Introductionunclassified

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Equinoideos del Cretácico Tardío del Norte de Coahuila, México

Silva-Martínez¹,

Blanco-Piñón²,

León-González³

2014

BSGM

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ResumenEn el presente trabajo se describen diez especies de equinodermos fósiles que han sido colectados en varios afloramientos de la Formación Austin (Cretácico Superior) localizados en los arroyos El Freno y El Tecolote, dentro del municipio de Jiménez, norte de Coahuila. La presencia de los ammonites Scaphites hippocrepis y Delawarella delawarensis en las secciones estudiadas permite asignar a estas capas una edad de Campaniano inferior. Algunos taxa aquí reportados como Cidaris texanus Clark, Salenia mexicana Schluter, Holectypus sp., Heteraster texanus Röemer y Diplodetus sp. son conocidos en varias localidades de México. Por otra parte, Cidaris splendens Morton, Diplopodia hilli Clark, Orthopsis casanovai Cooke, Micraster uddeni Cooke, Mecaster batnensis (Coquand), y Diplodetus sp. se reportan por primera vez para México en este trabajo, por lo que se amplía su rango de distribución en la parte oeste del Océano Proto-Atlántico. Por otra parte, la presencia de las especies Cidaris texanus, Cidaris splendens, Selenia mexicana y Heteraster texanus en capas de la Formación Austin amplía el rango de distribución temporal de estas especies dentro del Campaniano inferior en México, lo que podría contribuir en futuras interpretaciones bioestratigráficas de todo el Sistema Cretácico basadas en equinoideos.Palabras clave: Cretácico Superior, Campaniano inferior, Grupo Austin, equinoideos fósiles, noreste de México. Abstract Ten species of fossil echinoids are herein described from different outcrops of the Austin Formation (Upper Cretaceous) in the El

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Section: Discussionunclassified

Section: Introductionunclassified

Equinoideos del Cretácico Tardío del Norte de Coahuila, México

Silva-Martínez¹,

Blanco-Piñón²,

León-González³

2014

BSGM

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“…found unusual and exotic ammonites known until then only in the Western Interior: Prionocyclus novimexicanus (Marcou, 1858) in the Upper Turonian of Central Tunisia (Amédro in Robaszynski et al 1990), Acanthoceras amphibolum Morrow, 1935 and Paraconlinoceras aff. barcusi (Jones, 1938) in the Middle Cenomanian of Central Tunisia (Amédro in Robaszynski et al 1994), Metengonoceras teigenense Cobban and Kennedy, 1989 in the Lower Cenomanian of Normandy, France (Amé-dro et al 2002) and, lastly, the association being the subject of the present paper, with Romaniceras mexicanum Jones, 1938, Prionocyclus hyatti (Stanton, 1894) and Coilopoceras cf. springeri Hyatt, 1903, in the late Middle Turonian of south-east France (Amé-dro and Devalque in Robaszynski et al 2014).…”

mentioning

confidence: 61%

“…springeri Hyatt, 1903, from S Peyras, UL 4, Tm4, Romaniceras mexicanum Zone. C, D -Romaniceras (Romaniceras) mexicanum Jones, 1938, from SE Peyras, UL 4, Tm4, Romaniceras mexicanum Zone (scale bar = 2 cm).…”

Section: Platementioning

confidence: 99%

A North American ammonite fauna from the late Middle Turonian of Vaucluse and Gard, southern France: the Romaniceras mexicanum, Prionocyclus hyatti and Coilopoceras cf. springeri association

Amédro¹,

Robaszynski²,

Matrion³

et al. 2016

Acta Geologica Polonica

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An unusual, exotic, ammonite fauna including Romaniceras mexicanum Jones, 1938, Prionocyclus hyatti (Stanton, 1894) and Coilopoceras cf. springeri Hyatt, 1903 is recorded from the late Middle Turonian of Vaucluse and Gard, southern France. It is the first record of this ammonite association outside the Gulf Coast region and the Western Interior of the United States of North America. Up to present, these species were considered as endemic to the Western Interior sea-way. The migration of numerous ammonites from North America to western Europe during the late Middle Turonian suggests it is linked to a transgressive event or to a short sea-level high.

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“…One of the most interesting elements of the faunas was the recognition of Romaniceras (R.) mexicanum Jones, 1938, andCoilopoceras springeri Hyatt, 1903, in the Middle Turonian. These species were originally described from Coahuila Province in northern Mexico and New Mexico in the United States respectively, and remained unknown outside North America until Robaszynski et al (2014) documented their presence in the Uchaux Massif in Vaucluse, and interpreted this occurrence as a result of a transgressive event or sea level high at that time (as discussed elsewhere in this volume: Amédro et al 2016).…”

Section: Introductionmentioning

confidence: 99%

Coilopoceras inflatum Cobban and Hook, 1980, a United States Western Interior ammonite from the Upper Turonian of the southern Corbières, Aude, France

Melchior

Bilotte

Kennedy

2017

Acta Geologica Polonica

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A newly discovered ammonite faunule from the Padern region of the southern Corbières in southern France includes representatives of typical northwest European Upper Turonian species Subprionocyclus cf. neptuni (Geinitz, 1850) and Lewesiceras cf. woodi Wright 1979, tethyan/ northwestern Pacific species Phyllopachyceras cf. ezoense (Yokoyama, 1890), Anagaudryceras involvulum (Stoliczka, 1865) and, Desmoceras (Pseudouhligella) sp., together with Coilopoceras inflatum Cobban and Hook, 1980, a species previously known only from New Mexico in the United States, where it is regarded as Middle Turonian. The faunule occurs above one with Romaniceras (R.) mexicanum Jones, 1938 and Coilopoceras springeri Hyatt, 1903, also originally described from New Mexico and northern Mexico, and recently described from the Uchaux massif in Vaucluse in southern France. The records suggest that the base of the Upper Turonian may be drawn at different, higher level in the United States Western Interior than in Europe. The coming together of these mixed faunal elements may be a result of high sea levels, and changing oceanic circulation patterns.

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Geology of Sierra de la Pena and paleontology of the Indidura formation Coahuila, Mexico

Cited by 31 publications

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Equinoideos del Cretácico Tardío del Norte de Coahuila, México

Equinoideos del Cretácico Tardío del Norte de Coahuila, México

A North American ammonite fauna from the late Middle Turonian of Vaucluse and Gard, southern France: the Romaniceras mexicanum, Prionocyclus hyatti and Coilopoceras cf. springeri association

Coilopoceras inflatum Cobban and Hook, 1980, a United States Western Interior ammonite from the Upper Turonian of the southern Corbières, Aude, France

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