<?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>S1026-87742021000300178</article-id>
<article-id pub-id-type="doi">10.22201/cgeo.20072902e.2021.3.1636</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[Mobile mud layer underneath the desiccated maar lake of Rincón de Parangueo and insights into its microbial fingerprints]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Sánchez-Sánchez]]></surname>
<given-names><![CDATA[Janet]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Cerca]]></surname>
<given-names><![CDATA[Mariano]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Alcántara-Hernández]]></surname>
<given-names><![CDATA[Rocío J]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Aranda-Gómez]]></surname>
<given-names><![CDATA[José Jorge]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Carreón-Freyre]]></surname>
<given-names><![CDATA[Dora]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Lozano-Flores]]></surname>
<given-names><![CDATA[Carlos]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Muñoz-Velasco]]></surname>
<given-names><![CDATA[Israel]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Levresse]]></surname>
<given-names><![CDATA[Gilles]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Varela-Echavarría]]></surname>
<given-names><![CDATA[Alfredo]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad Nacional Auto&#769;noma de Me&#769;xico Centro de Geociencias Posgrado en Ciencias de la Tierra]]></institution>
<addr-line><![CDATA[Juriquilla Quere&#769;taro]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad Nacional Auto&#769;noma de Me&#769;xico Centro de Geociencias ]]></institution>
<addr-line><![CDATA[Juriquilla Quere&#769;taro]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Universidad Nacional Autónoma de México Instituto de Geología ]]></institution>
<addr-line><![CDATA[Mexico City ]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af4">
<institution><![CDATA[,Universidad Nacional Autónoma de México Instituto de Neurobiología Departamento de Biología del Desarrollo y Neurofisiología]]></institution>
<addr-line><![CDATA[Querétaro ]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af5">
<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>3</numero>
<fpage>178</fpage>
<lpage>192</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1026-87742021000300178&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1026-87742021000300178&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1026-87742021000300178&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract We surveyed a subsurface layer of saturated mobile mud and its microbial fingerprints below the desiccated bottom of a maar (sedimentary environmental DNA) lake at Rincón de Parangueo (RP), Mexico. A multiscale approach was followed using geological fieldwork, coring of the sediments, ground penetrating radar survey, physico-chemical characterization including X-ray diffraction and scanning electron microscope, and high-throughput DNA sequencing methods. The mobile mud is an organic-rich silty clay, with high values of alkalinity, volumetric water content and conductivity. Mud mobility has been attributed to overpressure caused by disequilibrium compaction of sediments related to active subsidence and pore overpressure produced by an input of groundwater and gas content in the sediments and resulted in a diverse set of structures related to mud tectonics such as injection domes and fluid seeps through fractures. Extraction and sequencing of sedimentary environmental DNA in the mud layer were performed for Bacteria and Archaea. Despite the small number of samples obtained, the microbial fingerprint from the sedimentary environmental DNA at subsurface shares similarities with the microbial communities identified on the crater surface. Additionally, we identify the DNA of specific methanogenic microorganisms in the mud, such as Bathyarchaeia, Methanomassiliicoccales, and Methanobacteriales, and we speculate on their probable role in gas production and pore overpressure in the mud layer. The underground mud at Rincón de Parangueo represents a geologically dynamic environment with conditions that are favorable for the thriving of microbial communities.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen En este trabajo examinamos una capa subsuperficial de lodo saturado móvil y su huella microbiana por debajo del fondo desecado del lago maar en Rincón de Parangueo (RP), México. Se siguió&#769; un enfoque de múltiples escalas, se integró&#769; trabajo de campo geológico, extracción de núcleos de sedimentos cercanos a la superficie, prospección por radar de penetración terrestre, caracterización fisicoquímica incluida la difracción de rayos X y microscopio electrónico de barrido y métodos de secuenciación de ADN de alto rendimiento. El lodo móvil está compuesto de arcilla limosa rica en materia orgánica total, con altos valores de alcalinidad, contenido volumétrico de agua y conductividad. La movilidad del lodo se atribuye a la sobrepresión causada por la compactación desequilibrada de los sedimentos, relacionada con la subsidencia activa en el cráter, y la sobrepresión de poro producida por una entrada de agua subterránea y gas en los sedimentos, lo que da como resultado un conjunto diverso de estructuras relacionadas con la tectónica de lodo, como domos de inyección de lodo y filtraciones de fluido a travé&#769;s de fracturas. La extracción y secuenciación de ADN ambiental en la capa de lodo se realizó&#769; para Bacteria y Archaea. A pesar de contar con un número pequeño de muestras de sedimentos, la huella microbiana obtenida en el subsuelo comparte similitudes con las secuencias identificadas en la superficie del cráter. Adicionalmente, en el lodo reportamos la presencia de microorganismos metanogénicos, tales como Bathyarchaeia, Methanomassiliicoccales y Methanobacteriales, y especulamos sobre su probable papel en la producción de gas y la sobrepresión del fluido de poro en la capa de lodo. El lodo subterráneo en Rincón de Parangueo representa un ambiente dinámico con condiciones favorables para el crecimiento de comunidades microbianas.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[saturated mud]]></kwd>
<kwd lng="en"><![CDATA[microbiology]]></kwd>
<kwd lng="en"><![CDATA[mud injection domes]]></kwd>
<kwd lng="en"><![CDATA[maar crater]]></kwd>
<kwd lng="en"><![CDATA[lake]]></kwd>
<kwd lng="es"><![CDATA[lodo saturado]]></kwd>
<kwd lng="es"><![CDATA[microbiología]]></kwd>
<kwd lng="es"><![CDATA[domos de inyecció&#769;n de lodo]]></kwd>
<kwd lng="es"><![CDATA[cráter maar]]></kwd>
<kwd lng="es"><![CDATA[lago]]></kwd>
</kwd-group>
</article-meta>
</front><back>
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