<?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>S1405-33222018000200397</article-id>
<article-id pub-id-type="doi">10.18268/bsgm2018v70n2a9</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Descripción de las huellas de camélidos y félidos de la localidad Pie de Vaca, Cenozoico Tardío de Puebla, centro de México y algunas consideraciones paleobiológicas]]></article-title>
<article-title xml:lang="en"><![CDATA[Description of camelids and felids of the Pie de Vaca site, Late Cenozoic of Puebla, central Mexico, and some paleobiological considerations]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Cabral-Perdomo]]></surname>
<given-names><![CDATA[Miguel Angel]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Bravo-Cuevas]]></surname>
<given-names><![CDATA[Víctor Manuel]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Pérez-Pérez]]></surname>
<given-names><![CDATA[Alexis]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[García-Cabrera]]></surname>
<given-names><![CDATA[Norberto]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad Autónoma del Estado de Hidalgo Área Académica de Biología ]]></institution>
<addr-line><![CDATA[Mineral de la Reforma Hidalgo]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad Autónoma del Estado de Hidalgo  ]]></institution>
<addr-line><![CDATA[Mineral de la Reforma Hidalgo]]></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>397</fpage>
<lpage>416</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1405-33222018000200397&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1405-33222018000200397&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1405-33222018000200397&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen La localidad Pie de Vaca en el estado de Puebla destaca por su importante abundancia de huellas fósiles pertenecientes a mamíferos, entre las cuales las más representativas han sido referidas a camélidos y félidos. El propósito del presente estudio fue la caracterización formal de este conjunto de huellas y comentar algunos aspectos paleobiológicos relacionados con el tamaño, velocidad y modalidad de progresión de los productores del registro icnofosilífero. La muestra consistió en 233 huellas: 154 pertenecen a nueve rastros producidos por camélidos y 79 a tres rastros por félidos. La caracterización de las huellas se realizó mediante la comparación de su tamaño y morfología con otras producidas por taxones fósiles y recientes. Las impresiones de camélidos, con base en su forma y tamaño, fueron designadas a la icnoespecie Lamaichnum guanicoe, ya que muestran el patrón morfológico típico de este grupo de artiodáctilos. Se sugiere que fueron producidas por algún integrante del género Hemiauchenia, el cual corresponde al camélido más común del Cenozoico tardío de México. Por su parte, las huellas de félidos únicamente fueron referidas a la morfofamilia Felipedidae debido a la mala preservación de sus caracteres icnotaxonómicos; sin embargo, al ser más grandes que huellas de los icnogéneros Felipeda, Pycnodactylopus, Pumaeichnum y Mitsupes, se sugiere que fueron producidas por alguna forma de talla mediana a grande, por ejemplo un macairodontino o un panterino. El modo de progresión de ambos productores corresponde con el de organismos con caminata relativamente rápida que se desplazan a una velocidad inferior a los 4 m/s. La dirección y número de individuos de los rastros de camélidos, son indicativos de un comportamiento gregario, probablemente asociado a cierta organización social. En el caso de los félidos se propone un comportamiento solitario o en pareja.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract The Pie de Vaca locality in the State of Puebla stands out for its important abundance of fossil mammal footprints, among them, the most representatives have been referred to camelids and felids. The purpose of the present study was the formal characterization of this set of footprints and comment on some paleobiological aspects related to their size, speed, and mode of progression of the track-makers. The sample consists of 233 footprints including 154 referable to nine trackways produced by camelids and 79 referable to three trackways produced by felids. The characterization of the tracks was made by comparing their size and morphology with others produced by fossil and recent taxa. The impressions of camelids, based on their shape and size, were designated to the icnospecies Lamaichnum guanicoe because they show the typical morphological pattern of this group of artiodactyls. It is suggested that they were produced by some member of the genus Hemiauchenia, which corresponds to the most common camelid of the Late Cenozoic of Mexico. On the other hand, the tracks of felids were only referred to the morphofamily Felipedidae due to the bad preservation of its ichnotaxonomic characters; however, being larger than traces of the ichnogenera Felipeda, Pycnodactylopus, Pumaeichnum and Mitsupes, it is suggested that they were produced by some form of medium to large size, a machairodontid or a pantherine, for instance. The mode of progression of both producers corresponds to that of relatively fast walking organisms that move at a speed lower than 4 m/s. The direction and number of individuals of camelids trackways, are indicative of gregarious behavior, probably associated with a certain social organization. In the case of felids, solitary or couple behavior is proposed.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[icnita]]></kwd>
<kwd lng="es"><![CDATA[camélidos]]></kwd>
<kwd lng="es"><![CDATA[félidos]]></kwd>
<kwd lng="es"><![CDATA[paso]]></kwd>
<kwd lng="es"><![CDATA[zancada]]></kwd>
<kwd lng="es"><![CDATA[progresión]]></kwd>
<kwd lng="en"><![CDATA[ichnite]]></kwd>
<kwd lng="en"><![CDATA[camelids]]></kwd>
<kwd lng="en"><![CDATA[felids]]></kwd>
<kwd lng="en"><![CDATA[pace]]></kwd>
<kwd lng="en"><![CDATA[stride]]></kwd>
<kwd lng="en"><![CDATA[progression]]></kwd>
</kwd-group>
</article-meta>
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