<?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>S1026-87742020000100009</article-id>
<article-id pub-id-type="doi">10.22201/cgeo.20072902e.2020.1.1095</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[Revisiting the Cupidito unit (Cupido Formation) along peritidal carbonates from northeastern Mexico]]></article-title>
<article-title xml:lang="es"><![CDATA[Carbonatos perimareales a lo largo de la Plataforma Cupido del Cretácico: noreste de México]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Torres de la Cruz]]></surname>
<given-names><![CDATA[Felipe de Jesús]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Chacón-Baca]]></surname>
<given-names><![CDATA[Elizabeth]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Chávez-Cabello]]></surname>
<given-names><![CDATA[Gabriel]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Hernández-Ocaña]]></surname>
<given-names><![CDATA[María Isabel]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad Autónoma de Nuevo León Posgrado de la Facultad de Ciencias de la Tierra ]]></institution>
<addr-line><![CDATA[Linares N.L.]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad Autónoma de Nuevo León Facultad de Ciencias de la Tierra ]]></institution>
<addr-line><![CDATA[Linares N.L.]]></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>9</fpage>
<lpage>25</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1026-87742020000100009&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1026-87742020000100009&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1026-87742020000100009&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT Depositional episodes are readily identified along representative localities of the Lower Cretaceous Cupido platform in northeastern Mexico. The basal part of the Cupido Formation exhibits a progradational reef platform that, at the upper limit, is truncated by a sequence boundary defined by a breccia. This breccia marks the development of a peculiar sedimentary facies informally known as the Cupidito unit, a distinctive stratigraphical unit in northeastern Mexico that remained uninterpreted for decades. Through the analysis of facies, microfacies and stable isotope comparisons from representative localities (Potrero Chico, Potrero de García, La Huasteca, La Muralla and Puerto Mexico) and from other previously reported outcrops, this work describes six diagnostic features for Cupidito and an improved stratigraphic model is proposed. The depositional sequence suggests a broad flat-topped platform with a general low organic productivity and restricted conditions followed by recurrent inundations of lagoon waters. Before drowning, this carbonate platform remained under equilibrium conditions interrupted by short pulses of relative higher-temperatures (48.3 °C and 39.2 °C). Coral-rudist-stromatoporoid patch-reefs with inferred inter-tropical temperatures between 31.5 °C and 32.2 °C originated as a progradational response to the instauration of a new Sequence Boundary at the base of Cupidito.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN Se identificaron episodios de depósito a lo largo de localidades representativas de la plataforma Cupido del Cretácico Temprano en el noreste de México. La parte basal de la Formación Cupido se compone de una facies arrecifal progradante que, en su límite superior, se trunca por un límite de secuencia identificada mediante una brecha. Esta brecha marca el desarrollo de una facies sedimentaria muy distintiva conocida como unidad Cupidito, una unidad estratigráfica reconocida en el noreste de México y que ha sido interpretada como un Tracto Sistema Transgresivo. A través del análisis de facies, microfacies y de la comparación de isótopos estables de localidades representativas (Potrero Chico, Potrero de García, La Huasteca, La Muralla y Puerto México) y de otros afloramientos previamente reportados, este trabajo describe seis características diagnósticas para la unidad Cupidito y propone un modelo de facies mejorado basado en los datos derivados de este trabajo y literatura disponible. El depósito de la Formación Cupido sugiere una plataforma amplia y plana con una productividad orgánica relativamente baja y ocasionalmente con condiciones muy restringidas, seguidas de episodios de inundaciones recurrentes de aguas de origen lagunar. Antes del episodio de ahogamiento, esta plataforma carbonatada se mantuvo en condiciones de equilibrio interrumpido por pulsos cortos de temperaturas relativamente altas (entre 48.3 °C y 39.2 °C). Las paleotemperaturas inferidas para los parches arrecifales de corales-rudistas-estromatopóridos intertropicales oscilan entre 31.5 °C y 32.2 °C; dichos parches probablemente se originaron como una respuesta progradante a la instauración del Límite de Secuencia en la base de Cupidito.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[Peritidal carbonates]]></kwd>
<kwd lng="en"><![CDATA[drowning platform]]></kwd>
<kwd lng="en"><![CDATA[deposition model]]></kwd>
<kwd lng="en"><![CDATA[sequence boundary]]></kwd>
<kwd lng="en"><![CDATA[stratiform microbial mats]]></kwd>
<kwd lng="en"><![CDATA[paleotemperature]]></kwd>
<kwd lng="es"><![CDATA[Carbonatos perimareales]]></kwd>
<kwd lng="es"><![CDATA[plataforma ahogada]]></kwd>
<kwd lng="es"><![CDATA[modelo de depósito]]></kwd>
<kwd lng="es"><![CDATA[límite de secuencia]]></kwd>
<kwd lng="es"><![CDATA[tapetes microbianos estratiformes]]></kwd>
<kwd lng="es"><![CDATA[paleotemperatura]]></kwd>
</kwd-group>
</article-meta>
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