<?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>S1026-87742022000100043</article-id>
<article-id pub-id-type="doi">10.22201/cgeo.20072902e.2022.1.1665</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[Diversity of Crinozoa (Echinodermata: Eocrinoidea, Blastoidea, Crinoidea) from the Paleozoic of Mexico.]]></article-title>
<article-title xml:lang="es"><![CDATA[Diversidad de Crinozoa (Echinodermata: Eocrinoidea, Blastoidea, Crinoidea) del Palezoico de México]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Buitrón-Sánchez]]></surname>
<given-names><![CDATA[Blanca Estela]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Cuen-Romero]]></surname>
<given-names><![CDATA[Francisco Javier]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Monreal]]></surname>
<given-names><![CDATA[Rogelio]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Cuadros-Mendoza]]></surname>
<given-names><![CDATA[Iván Manuel]]></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 Departamento de Paleontología]]></institution>
<addr-line><![CDATA[Mexico City ]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad de Sonora Departamento de Geología ]]></institution>
<addr-line><![CDATA[Hermosillo Sonora]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Universidad Nacional Autónoma de México Facultad de Ingeniería ]]></institution>
<addr-line><![CDATA[Mexico City ]]></addr-line>
<country>Mexico</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>00</month>
<year>2022</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>00</month>
<year>2022</year>
</pub-date>
<volume>39</volume>
<numero>1</numero>
<fpage>43</fpage>
<lpage>53</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1026-87742022000100043&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1026-87742022000100043&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1026-87742022000100043&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT Paleozoic outcrops in Mexico containing echinoderms are located to the north, center and south of the country, mainly in the states of Baja California, Sonora, Chihuahua, Tamaulipas, Coahuila, Hidalgo, Puebla, Guerrero, Oaxaca, and Chiapas. These rocks correspond to marine carbonates deposited in warm shallow environments, with an approximate age of 541 to 251 Ma. Also containing a varied and diverse biota made up of phylloid algae, foraminifera (fusulinids), coralline sponges, corals, bryozoans, brachiopods, mollusks, trilobites and echinoderms. In order to know the diversity of Crinozoa from the Paleozoic of Mexico, an analysis of the species documented for the country was carried out, with the objective of contributing to the knowledge of the biostratigraphy and paleogeography of Mexico. The methodology consisted of a detailed analysis of bibliographic sources with information on echinoderms from the Paleozoic of Mexico. Cambrian eocrinoids (Gogia, and Ubaghsicystis) are distributed mainly in Sonora. Crinoid plates from the Carboniferous and Permian, particularly morphospecies of the genera Cyclocaudex, Cyclocrista, Heterostelechus, Lamprosterigma, Mooreanteris, Pentagonopternix, Preptopremnum, and Pentaridica, are widely distributed throughout the country. Analysis of the Mississippian-Permian biota indicates that the cosmopolitan distribution of the fauna studied in this work is due to the connections between the seas of western North America and eastern Asia. The Late Permian benthic fauna of Sonora was widely dispersed in the Tethyan realm, which stretched from western North America to North Africa and Asia. The comprehensive study of Paleozoic marine stratigraphic successions and their biotic content provided information on faunal migrations regarding the Paleozoic carbonate facies. It also contributed to reconstructing the geographical, climatological, and ecological characteristics of the Paleozoic of Mexico.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN Los afloramientos paleozoicos en México con equinodermos se ubican al norte, centro y sur del país, principalmente en los estados de Baja California, Sonora, Chihuahua, Tamaulipas, Coahuila, Hidalgo, Puebla, Guerrero, Oaxaca y Chiapas. Estas rocas carbonatadas marinas fueron depositadas en ambientes cálidos poco profundos, con una edad aproximada de 541 a 251 Ma. También contienen una biota variada y diversa compuesta por algas filoides, foraminíferos (fusulínidos), esponjas coralinas, corales, briozoos, braquiópodos, moluscos, trilobites y equinodermos. Con el objetivo de conocer la diversidad de Crinozoa del Paleozoico de México, se realizó un análisis de las especies documentadas para el país, con el objetivo de contribuir al conocimiento de la bioestratigrafía y paleogeografía de México. La metodología consistió en un análisis detallado de fuentes bibliográficas con información sobre equinodermos del Paleozoico de México. Los eocrinoides cámbricos (Gogia y Ubaghsicystis) se distribuyen principalmente en Sonora. Las placas de crinoideos del Carbonífero y Pérmico, en particular las morfoespecies de los géneros Cyclocaudex, Cyclocrista, Heterostelechus, Lamprosterigma, Mooreanteris, Pentagonopternix, Preptopremnum y Pentaridica, están ampliamente distribuidas por todo el país. El análisis de la biota del Misisípico-Pérmico indica que la distribución cosmopolita de la fauna estudiada en este trabajo se debe a las conexiones entre los mares del oeste de América del Norte y el este de Asia. La fauna bentónica del Pérmico tardío de Sonora estaba muy dispersa en el dominio del Tethys, que se extendía desde el oeste de América del Norte hasta el norte de África y Asia. El estudio exhaustivo de las sucesiones estratigráficas marinas del Paleozoico y su contenido biótico proporcionó información sobre las migraciones de fauna con respecto a las facies carbonatadas del Paleozoico. También contribuyó a reconstruir las características geográficas, climatológicas y ecológicas del Paleozoico de México.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[Paleobiodiversity]]></kwd>
<kwd lng="en"><![CDATA[invertebrates]]></kwd>
<kwd lng="en"><![CDATA[echinoderms]]></kwd>
<kwd lng="en"><![CDATA[paleobiogeo-graphy]]></kwd>
<kwd lng="en"><![CDATA[Paleozoic]]></kwd>
<kwd lng="en"><![CDATA[Mexico]]></kwd>
<kwd lng="es"><![CDATA[paleobiodiversidad]]></kwd>
<kwd lng="es"><![CDATA[invertebrados]]></kwd>
<kwd lng="es"><![CDATA[equinodermos]]></kwd>
<kwd lng="es"><![CDATA[paleobiogeografía]]></kwd>
<kwd lng="es"><![CDATA[Paleozoico]]></kwd>
<kwd lng="es"><![CDATA[México]]></kwd>
</kwd-group>
</article-meta>
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