<?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>S1026-87742021000100065</article-id>
<article-id pub-id-type="doi">10.22201/cgeo.20072902e.2021.1.1598</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[Biostratigraphy and paleoenvironment of Maastrichtian foraminiferal assemblages from a succession located NW of Tuxtla Gutiérrez, Chiapas (SE Mexico)]]></article-title>
<article-title xml:lang="es"><![CDATA[Bioestratigrafía y paleoambiente de conjuntos foraminiferales de una sucesión ubicada al NW de Tuxtla Gutiérrez, Chiapas (SE de México)]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Omaña]]></surname>
<given-names><![CDATA[Lourdes]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Pons]]></surname>
<given-names><![CDATA[Jose Maria]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Cruz]]></surname>
<given-names><![CDATA[Rubén]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad Nacional Autónoma de México Instituto de Geología ]]></institution>
<addr-line><![CDATA[Mexico City ]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universitat Autònoma de Barcelona Departament de Geologia ]]></institution>
<addr-line><![CDATA[Bellaterra ]]></addr-line>
<country>Spain</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Universidad Nacional Autónoma de México Facultad de Ciencias ]]></institution>
<addr-line><![CDATA[Mexico City ]]></addr-line>
<country>Mexico</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>00</month>
<year>2021</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>00</month>
<year>2021</year>
</pub-date>
<volume>38</volume>
<numero>1</numero>
<fpage>65</fpage>
<lpage>81</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1026-87742021000100065&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1026-87742021000100065&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1026-87742021000100065&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT During the Maastrichtian, two lithostratigraphic units were deposited in the central Chiapas region; the Ocozocoautla and Angostura formations. The first unit crops out northwest of the city of Tuxtla Gutiérrez in central Chiapas. It is a complex lithological unit mainly composed of siliciclastic rocks interbedded with limestone. Overlying it, the Angostura limestone is recognized. This study focuses on a taxonomic study of the larger benthic and planktic foraminifera from both formations in order to assign age and to infer the paleoenviroment. The Ocozocoautla Formation includes an association of benthic as well as significant planktic foraminifera. Based on the microfossils stratigraphic distribution, two biozones were defined: the Pseudorbitoides rutteni-Ayalaina rutteni Assemblage Zone of earliest Maastrichtian and the upper part of the Gansserina gansseri Interval Zone of early Maastrichtian. The Angostura Formation contains dasycladacean algae and larger foraminifera considered as important age markers in shallow-water environments. Two foraminiferal interval zones were defined, Praechubbina breviclaustra Interval Zone of early late Maastrichtian and Chubbina jamaicensis Total Range Zone of late to latest Maastrichian age. The microfacies (grainstone, wackestone-packstone, wackestone) as well as the foraminiferal assemblage enable the paleoenvironment to be reconstructed, suggesting a deposit that developed in an open-water marine setting with moderate to high energy, characterized by benthic and planktic foraminifera in the Ocozocoautla Formation, while in the Angostura Formation a shallow-water marine protected environment is inferred. The paleobiogeographical distribution of the assemblage from both the Ocozocoautla and Angostura formations mostly contains endemic benthic foraminifera of the Caribbean Province and other few Tethysian forms of the Angostura Formation.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN Durante el Maastrichtiano se depositaron dos unidades litológicas en el centro de Chiapas, las formaciones Ocozocoautla y Angostura. La primera unidad está aflorando al noroeste de la ciudad de Tuxtla Gutiérrez, en el centro de Chiapas. Es una unidad litológica compleja compuesta principalmente de rocas siliciclásticas interestratificadas con caliza. Sobreyaciendo a esta unidad se reconoce a la caliza Angostura. Esta investigación se ha centrado en el estudio taxonómico de los macroforaminíferos de ambas formaciones y en la presencia de foraminíferos planctónicos del componente calcáreo de la unidad Ocozocoautla. La Formación Ocozocoautla incluye una asociación de foraminíferos bentónicos, así como importantes foraminíferos planctónicos, con base en la distribución estratigráfica de estos microfósiles fueron definidas dos zonas Zona de Conjunto Pseudorbitoides rutteni-Ayalaina rutteni del Maastrichtiano más temprano y la parte superior de la Zona de Intervalo Gansserina gansseri del Maastrichtiano temprano. Por otro lado, la Formación Angostura contiene macroforaminíferos, los cuales son considerados importantes marcadores de edad en ambientes someros: dos zonas fueron definidas la Zona de Intervalo Praechubbina breviclaustra del Maastrichtiano tardío temprano y la Zona de Alcance Total Chubbina jamaicensis del Maastrichtiano tardío a más tardío. Las microfacies (grainstone, wackestone-packstone,wackestone), así como el conjunto foraminiferal permiten reconstruir el paleoambiente, sugiriendo un depósito que se desarrolló en un entorno marino de aguas abiertas con energía moderada a alta, caracterizado por foraminíferos planctónicos para la Formación Ocozocooautla mientras que en la Formación Angostura se infiere un ambiente protegido de aguas poco profundas. La distribución paleobiogeográfica del conjunto foraminiferal de las formaciones Ocozocoautla y Angostura contienen principalmente formas endémicas de la Provincia del Caribe, así como otras pocas formas Tethysianas en la Formación Angostura.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[Foraminifera]]></kwd>
<kwd lng="en"><![CDATA[early-late Maastrichtian]]></kwd>
<kwd lng="en"><![CDATA[Chiapas]]></kwd>
<kwd lng="en"><![CDATA[SE Mexico]]></kwd>
<kwd lng="es"><![CDATA[Foraminíferos]]></kwd>
<kwd lng="es"><![CDATA[Maastrichtiano temprano-tardío]]></kwd>
<kwd lng="es"><![CDATA[Chiapas]]></kwd>
<kwd lng="es"><![CDATA[SE de México]]></kwd>
</kwd-group>
</article-meta>
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