<?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>1405-3322</journal-id>
<journal-title><![CDATA[Boletín de la Sociedad Geológica Mexicana]]></journal-title>
<abbrev-journal-title><![CDATA[Bol. Soc. Geol. Mex]]></abbrev-journal-title>
<issn>1405-3322</issn>
<publisher>
<publisher-name><![CDATA[Sociedad Geológica Mexicana A.C.]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S1405-33222018000300797</article-id>
<article-id pub-id-type="doi">10.18268/bsgm2018v70n3a12</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Presencia de Plagiobrissus grandis (Gmelin, 1788) (Echinoidea: Spatangoida) en la Formación Tuxpan, Mioceno (Langhiano) del norte del Estado de Veracruz, México. Consideraciones Biogeográficas]]></article-title>
<article-title xml:lang="en"><![CDATA[Occurrence of Plagiobrissus grandis (Gmelin, 1788) (Echinoidea: Spatagoida) in the Tuxpan Formation, Miocene (Langhian) in northem Veracruz state, Mexico. Biogeographic considerations]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Sour-Tovar]]></surname>
<given-names><![CDATA[Francisco]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Quiroz-Barroso]]></surname>
<given-names><![CDATA[Sara Alicia]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Torres-Martínez]]></surname>
<given-names><![CDATA[Miguel Ángel]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad Nacional Autónoma de México Facultad de Ciencias Departamento de Biología Evolutiva]]></institution>
<addr-line><![CDATA[CDMX ]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad Nacional Autónoma de México Instituto de Geología Departamento de Paleontología]]></institution>
<addr-line><![CDATA[CDMX ]]></addr-line>
<country>Mexico</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>00</month>
<year>2018</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>00</month>
<year>2018</year>
</pub-date>
<volume>70</volume>
<numero>3</numero>
<fpage>797</fpage>
<lpage>807</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1405-33222018000300797&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1405-33222018000300797&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1405-33222018000300797&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen Se reporta la presencia de Plagiobrissus grandis en una localidad del Mioceno medio (Langhiano) de la Formación Tuxpan en la región de Papantla-Martínez de la Torre, norte de Veracruz. Tal hallazgo permite analizar el patrón de distribución espacio-temporal del género, corrobora su origen durante el Eoceno en el Caribe y su posterior dispersión en el Mioceno que le permitió aumentar su rango de distribución hasta Carolina del Norte en los Estados Unidos y las costas de Venezuela y Brasil. La formación del Istmo de Panamá, y con ello el cierre de la conexión con el Pacífico durante el Mioceno-Plioceno, desencadenó grandes cambios en las corrientes del Atlántico Norte, favoreciendo, entre el Mioceno tardío y el presente, la dispersión del género hacia el Mediterráneo y las costas del Norte de África, hasta el Golfo de Guinea. La evidencia de Plagiobrissus grandis en el Mioceno medio y su existencia en el Reciente, da un ejemplo de la longevidad que presentan diversas especies de equinoideos.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract The presence of Plagiobrissus grandis is reported in a locality of the middle Miocene (Langhiano) of the Tuxpan Formation in the Papantla-Martínez de la Torre region, North of Veracruz. The finding allows to analyze the space-time distribution of the genus, and corroborates its origin in the Caribbean during Eocene times, as well as its later dispersion during the Miocene to North Carolina in the United States and the coasts of Venezuela and Brazil. The division of the Pacific and the Atlantic oceans during the Miocene-Pliocene, by the emergence of the Panama Isthmus, triggered great changes in the marine currents of the North Atlantic; that event favored the dispersion of the genus from the Miocene to the Recent towards the Mediterranean and the coasts of North Africa, to the Gulf of Guinea. The finding of Plagiobrissus grandis in the middle Miocene and its survival until the present provides an example of the longevity of several echinoid species.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[Mioceno]]></kwd>
<kwd lng="es"><![CDATA[Plagiobrissus grandis]]></kwd>
<kwd lng="es"><![CDATA[Spatangoida]]></kwd>
<kwd lng="es"><![CDATA[Formación Tuxpan]]></kwd>
<kwd lng="es"><![CDATA[Veracruz]]></kwd>
<kwd lng="es"><![CDATA[México]]></kwd>
<kwd lng="en"><![CDATA[Miocene]]></kwd>
<kwd lng="en"><![CDATA[Plagiobrissus grandis]]></kwd>
<kwd lng="en"><![CDATA[Spatangoida]]></kwd>
<kwd lng="en"><![CDATA[Tuxpan Formation]]></kwd>
<kwd lng="en"><![CDATA[Veracruz]]></kwd>
<kwd lng="en"><![CDATA[Mexico]]></kwd>
</kwd-group>
</article-meta>
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