<?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>0016-7169</journal-id>
<journal-title><![CDATA[Geofísica internacional]]></journal-title>
<abbrev-journal-title><![CDATA[Geofís. Intl]]></abbrev-journal-title>
<issn>0016-7169</issn>
<publisher>
<publisher-name><![CDATA[Universidad Nacional Autónoma de México, Instituto de Geofísica]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S0016-71692025000101479</article-id>
<article-id pub-id-type="doi">10.22201/igeof.2954436xe.2025.64.1.1768</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[Bioweathering of lava flows: the case of Xitle volcano in Mexico City]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Martínez Báez-Téllez]]></surname>
<given-names><![CDATA[M. F.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Ortega-Larrocea]]></surname>
<given-names><![CDATA[M. P.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad Nacional Autónoma de México Posgrado en Ciencias Biológicas ]]></institution>
<addr-line><![CDATA[Ciudad de México ]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad Nacional Autónoma de México Instituto de Geología Laboratorio Microcosmos Bioedáfico, Departamento de Ciencias Ambientales y del Suelo]]></institution>
<addr-line><![CDATA[Ciudad de México ]]></addr-line>
<country>Mexico</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>03</month>
<year>2025</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>03</month>
<year>2025</year>
</pub-date>
<volume>64</volume>
<numero>1</numero>
<fpage>1479</fpage>
<lpage>1491</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S0016-71692025000101479&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S0016-71692025000101479&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S0016-71692025000101479&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract This contribution describes biological weathering features produced by microbial communities growing on rock surfaces denominated biological rock crusts. We provide arguments related to the importance of recognizing rocks as an ecological niche and a review of main recognized bio-weathering processes in basaltic bedrock. We particularly address the features found in the lava flow of the monogenetic volcano Xitle, which is located in the volcanic field of the Sierra del Chichinautzin in the south of Mexico City. We found that the diversity and distribution of organisms within the rock crusts varies depending on the superficial texture and porosity of the lavas. Mosses have a preference for vesicles and crevices, while lichens can establish in smoother and more exposed areas. The predominant biological weathering features we have found associated with these crusts are incrustation, penetration, vesicle infilling, endolithic colonization, fractures, and particle entrapment. It is worth noting that bioweathering features are related to specific biological groups: lichens exert all of the features found, while mosses are mostly associated with particle entrapment and vesicle infilling, and biofilms are related to penetration and endolithic colonization. Therefore, this article discusses the importance of geoheritage conservation in relation to the biodiversity these lavas harbor.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen En esta contribución se describen los rasgos de intemperismo biológico producidos por comunidades microbianas que crecen sobre superficies rocosas denominadas costras saxícolas. Se presentan argumentos relacionados con la importancia de reconocer a las rocas volcánicas como un nicho ecológico, se hace una revisión de los principales procesos de intemperismo biológico reconocidos en lechos rocosos basálticos, abordando en particular los rasgos encontrados en el flujo de lava del volcán monogénico Xitle, ubicado en el campo volcánico de la Sierra del Chichinautzin al sur de la Ciudad de México. Se encontró que la diversidad y distribución de organismos dentro de las costras varía dependiendo de la textura superficial y la porosidad de las lavas. Los musgos tienen preferencia por vesículas y grietas, mientras que los líquenes pueden establecerse en áreas más lisas y expuestas. Las características de biointemperismo predominantes que hemos encontrado asociadas con estas costras son incrustación, penetración, relleno de vesículas, colonización endolítica, fracturas y atrapamiento de partículas. Las características de biointemperismo están relacionadas con grupos biológicos específicos: los líquenes están asociados con todos los rasgos encontrados; los musgos están más asociados con el atrapamiento de partículas y el relleno de vesículas, mientras que los biofilms se relacionan con la penetración y la colonización endolítica. Se analiza la importancia de la conservación del patrimonio geológico en relación con la biodiversidad que albergan estas lavas.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[Biological rock crusts]]></kwd>
<kwd lng="en"><![CDATA[bioreceptivity]]></kwd>
<kwd lng="en"><![CDATA[andesitic basalt]]></kwd>
<kwd lng="en"><![CDATA[biofilms]]></kwd>
<kwd lng="en"><![CDATA[monogenetic volcanoes]]></kwd>
<kwd lng="es"><![CDATA[Costras saxícolas]]></kwd>
<kwd lng="es"><![CDATA[biorreceptividad]]></kwd>
<kwd lng="es"><![CDATA[basalto andesítico]]></kwd>
<kwd lng="es"><![CDATA[biofilms]]></kwd>
<kwd lng="es"><![CDATA[volcanes monogenéticos]]></kwd>
</kwd-group>
</article-meta>
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