<?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>S1405-33222018000200351</article-id>
<article-id pub-id-type="doi">10.18268/bsgm2018v70n2a5</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[The Oldest Camel Footprints from Mexico]]></article-title>
<article-title xml:lang="es"><![CDATA[Las huellas de camello más antiguas de México]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Jiménez-Hidalgo]]></surname>
<given-names><![CDATA[Eduardo]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Guerrero-Arenas]]></surname>
<given-names><![CDATA[Rosalía]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad del Mar Instituto de Recursos Laboratorio de Paleobiología]]></institution>
<addr-line><![CDATA[Oaxaca Oaxaca]]></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>2</numero>
<fpage>351</fpage>
<lpage>359</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1405-33222018000200351&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1405-33222018000200351&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1405-33222018000200351&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract Camel footprints have a well preserved record in Neogene strata from North America, including Mexico, however their Paleogene record is much less known. Here, we describe the oldest camel footprints from Mexico, located in the outskirts of Tezoatlán de Segura y Luna, northwestern Oaxaca, southern Mexico. The camel footprints are preserved as concave epirelief in fine-grained tuffaceous sandstone of the late Eocene-early Oligocene Huajuapan Formation. These footprints display the diagnostic features of Lamaichnum guanicoe, such as bidigital tracks with pointed anterior ends and rounded posterior ends, with digit impressions that do not converge anteriorly and footprints that have digit imprints connected. Potential track makers include Paratylopus, Paralabis and Pseudolabis. The concave axial surface and nail imprints of the Oaxacan footprints, indicate that the track makers shared some anatomical foot features with extant camels, suggesting that some characteristics of the peculiar camel foot had already evolved by the late Eocene-early Oligocene.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen En los estratos del Neógeno norteamericano, incluyendo a México, existe un registro de huellas de camélidos bien preservado; sin embargo, el registro del Paleógeno es mucho menos conocido. En este artículo describimos las huellas de camello más antiguas de México, procedentes de los alrededores de Tezoatlán de Segura y Luna, noroeste de Oaxaca, sur de México. Las impresiones de huellas están preservadas como epirelieves cóncavos en areniscas tobáceas del Eoceno tardío-Oligoceno temprano de la Formación Huajuapan. Las huellas se identificaron como Lamaichnum guanicoe, debido a los rasgos que presentan, los cuales incluyen: huellas bidigitígradas con bordes anteriores acuminados y bordes posteriores redondeados, impresiones de dígitos que no convergen anteriormente e impresiones de dígitos conectadas. Los productores potenciales de las huellas incluyen a Paratylopus, Paralabis y Pseudolabis. La superficie axial cóncava y las impresiones de uñas de las huellas oaxaqueñas, indican que los productores compartían algunas características anatómicas podiales con los camellos actuales. Lo anterior, sugiere que algunas características anatómicas del pie de los camellos recientes habían evolucionado ya en el Eoceno tardío-Oligoceno temprano.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[Camelidae]]></kwd>
<kwd lng="en"><![CDATA[Lamaichnum guanicoe]]></kwd>
<kwd lng="en"><![CDATA[EoceneOligocene]]></kwd>
<kwd lng="en"><![CDATA[Tezoatlán]]></kwd>
<kwd lng="en"><![CDATA[Oaxaca]]></kwd>
<kwd lng="en"><![CDATA[Mixteca]]></kwd>
<kwd lng="es"><![CDATA[Camelidae]]></kwd>
<kwd lng="es"><![CDATA[Lamaichnum guanicoe]]></kwd>
<kwd lng="es"><![CDATA[Eoceno-Oligoceno]]></kwd>
<kwd lng="es"><![CDATA[Tezoatlán]]></kwd>
<kwd lng="es"><![CDATA[Oaxaca]]></kwd>
<kwd lng="es"><![CDATA[Mixteca]]></kwd>
</kwd-group>
</article-meta>
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