<?xml version="1.0" encoding="ISO-8859-1"?><article xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance">
<front>
<journal-meta>
<journal-id>1026-8774</journal-id>
<journal-title><![CDATA[Revista mexicana de ciencias geológicas]]></journal-title>
<abbrev-journal-title><![CDATA[Rev. mex. cienc. geol]]></abbrev-journal-title>
<issn>1026-8774</issn>
<publisher>
<publisher-name><![CDATA[Universidad Nacional Autónoma de México, Instituto de Geología]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S1026-87742020000100040</article-id>
<article-id pub-id-type="doi">10.22201/cgeo.20072902e.2020.1.1421</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Fauna de tiburones y rayas de la Formación Tirabuzón (Plioceno) en el Cañón El Álamo, sierras de La Reforma - El Aguajito, Baja California Sur, México]]></article-title>
<article-title xml:lang="en"><![CDATA[Shark and ray fauna of the Tirabuzón Formation (Pliocene) in El Álamo Canyon, Sierra de Reforma - Aguajito, Baja California Sur, Mexico]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Lira-Beltrán]]></surname>
<given-names><![CDATA[R. Marcela]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[González-Barba]]></surname>
<given-names><![CDATA[Gerardo]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Macías]]></surname>
<given-names><![CDATA[José Luis]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Solis-Añorve]]></surname>
<given-names><![CDATA[Azucena]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[García-Tenorio]]></surname>
<given-names><![CDATA[Felipe]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[García-Sánchez]]></surname>
<given-names><![CDATA[Laura]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Osorio-Ocampo]]></surname>
<given-names><![CDATA[Susana]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad Nacional Autónoma de México ENES Morelia Posgrado en Ciencias de la Tierra]]></institution>
<addr-line><![CDATA[Morelia Michoacán]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad Autónoma de Baja California Sur Museo de Historia Natural ]]></institution>
<addr-line><![CDATA[La Paz B.C.S.]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Universidad Nacional Autónoma de México Instituto de Geofísica ]]></institution>
<addr-line><![CDATA[Morelia Michoacán]]></addr-line>
<country>Mexico</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>00</month>
<year>2020</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>00</month>
<year>2020</year>
</pub-date>
<volume>37</volume>
<numero>1</numero>
<fpage>40</fpage>
<lpage>63</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1026-87742020000100040&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1026-87742020000100040&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1026-87742020000100040&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN En el presente trabajo presentamos los resultados de un estudio estratigráfico y paleontológico de nuevas localidades fosilíferas encontradas en el sustrato de las calderas La Reforma y El Aguajito, ubicadas aproximadamente a 30 km al norte de la población de Santa Rosalía, Baja California Sur, México. La sucesión sedimentaria estudiada se correlaciona con la Formación Tirabuzón del Plioceno de la cuenca de Santa Rosalía y forma parte del sustrato sedimentario de las calderas pleistocénicas. Una de las secciones más completas se encuentra expuesta en el cañón El Álamo y consiste en una sucesión de arenisca limosa de color naranja, conglomerado con abundantes fósiles de dientes de tiburón y rayas, un depósito volcánico basal y limolita de color amarillo ocre, las cuales en este trabajo se agruparon en tres unidades: 1) arenisca-limolita naranja, 2) depósito volcánico basal y 3) limolita Cimarrón. El material fósil estudiado consiste en 500 ejemplares de dientes individuales de elasmobranquios (macrodientes) que se extrajeron in situ. Para la localidad de El Álamo reportamos 19 taxa de tiburones y siete de rayas, siendo así el primer reporte de una fauna de Batoideos para la Formación Tirabuzón. La misma sucesión litológica y fósil fue encontrada en otras cinco localidades: Corkscrew Hill, Santa María, Cueva Amarilla, El Morro Prieto y El Gringo, en donde reportamos la presencia de Hemipristis Serra, así como Otodus megalodon y Parotodus benedeni para la localidad de Corkscrew Hill. Sobreyaciendo discordantemente a la unidad limolita Cimarrón se encuentra la ignimbrita Cueva Amarilla de la Formación Infierno fechada en 2.4 Ma. Estas nuevas localidades son una herramienta para poder correlacionar la Formación Tirabuzón hasta la porción noroccidental de la Caldera El Aguajito. El ensamblaje faunístico reportado corresponde a un ambiente marino somero de plataforma continental de aguas tropicales de edad Plioceno medio-superior.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT In this paper we present the results of a stratigraphic and paleontological study of new fossil localities found in the La Reforma and El Aguajito Calderas, Baja California Sur, Mexico, approximately 30 km north of the town of Santa Rosalía. The studied sedimentary succession is part of the substrate of the Pleistocene Calderas and is related to the Tirabuzón Formation (Pliocene) of the Santa Rosalía basin. During the Pliocene-Pleistocene the boundary of the Santa Rosalía basin extended beyond these volcanic structures and therefore the El Álamo canyon site recorded stratigraphic and paleontological evidences of the Tirabuzon Formation with abundant shark teeth and ray fossils and interbedded volcanic deposits. Shark fauna had previously been reported for the Tirabuzón Formation, to the south of the study area, but not at the El Álamo canyon. The same lithology and fossil assemblage was found in other locations: Corkscrew Hill, Santa María, Cueva Amarilla, El Morro Prieto and El Gringo. The studied material consists of 500 individual specimens of elasmobranch fossil teeth (macroteeth). We report 17 species and two genera of sharks, one species, and six genera of rays and, for the first time, a Batoid fauna for the Tirabuzón Formation. Discordantly on top of the Cimarrón siltstone appears the 2.4 Ma Cueva Amarilla ignimbrite of the Inferno Formation. The faunal assembly corresponds to a shallow and warm marine environment, similar to the current fauna of the Eastern Tropical Pacific.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[Neógeno]]></kwd>
<kwd lng="es"><![CDATA[Elasmobranquios]]></kwd>
<kwd lng="es"><![CDATA[Formación Tirabuzón]]></kwd>
<kwd lng="es"><![CDATA[cuenca de Santa Rosalía]]></kwd>
<kwd lng="es"><![CDATA[Baja California Sur]]></kwd>
<kwd lng="es"><![CDATA[México]]></kwd>
<kwd lng="en"><![CDATA[Neogene]]></kwd>
<kwd lng="en"><![CDATA[Elasmobranch]]></kwd>
<kwd lng="en"><![CDATA[Tirabuzón Formation]]></kwd>
<kwd lng="en"><![CDATA[Santa Rosalia basin]]></kwd>
<kwd lng="en"><![CDATA[Baja California Sur]]></kwd>
<kwd lng="en"><![CDATA[Mexico]]></kwd>
</kwd-group>
</article-meta>
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