<?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>S1405-33222016000300537</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Paleoecología y cronoestratigrafía de las diatomeas del Miembro Los Indios en la Mesa La Misión, del Mioceno de Baja California, México]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Salinas Márquez]]></surname>
<given-names><![CDATA[Fernando Manuel]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Flores Trujillo]]></surname>
<given-names><![CDATA[Juan Gabriel]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Helenes]]></surname>
<given-names><![CDATA[Javier]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Téllez Duarte]]></surname>
<given-names><![CDATA[Miguel Agustín]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Aranda Manteca]]></surname>
<given-names><![CDATA[Francisco Javier]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad Autónoma de Baja California Facultad de Ciencias Marinas ]]></institution>
<addr-line><![CDATA[Ensenada Baja California]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad Autónoma del Carmen Dependencia Académica de Ingeniería y Tecnología ]]></institution>
<addr-line><![CDATA[Ciudad del Carmen Campeche]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Centro de Investigación Científica y Estudios Superiores de Ensenada División de Ciencias de la Tierra ]]></institution>
<addr-line><![CDATA[Ensenada B.C.]]></addr-line>
<country>México</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>12</month>
<year>2016</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>12</month>
<year>2016</year>
</pub-date>
<volume>68</volume>
<numero>3</numero>
<fpage>537</fpage>
<lpage>552</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1405-33222016000300537&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1405-33222016000300537&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1405-33222016000300537&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen: El presente trabajo tiene como objetivo identificar y analizar los aspectos paleoambientales y bioestratigráficos de las especies de diatomeas presentes en los sedimentos en la Mesa La Misión.La Mesa La Misión, es un afloramiento del Miembro Los Indios de la formación Rosarito Beach en Baja California. Es una secuencia de rocas volcanoclásticas que contiene una abundante y diversa fauna. Se tomaron muestras de sedimentos a lo largo de la secuencia estratigráfica, y se encontraron 15 especies de diatomeas. La asociación de diatomeas indica que el depósito de sedimentos en el Miembro Los Indios ocurrió en una plataforma progradacional. Las diatomeas bentónicas son más abundantes en la base de la secuencia y se observa una disminución de estas en las capas superiores. La mayoría de las especies de diatomeas encontradas son de temperaturas templadas, sin embargo se observan algunas diatomeas tropicales y otras de aguas frías, lo que sugiere una mezcla de masas de agua. La mezcla de diatomeas de diferentes masas de agua y la disminución de las diatomeas bentónicas sugiere una elevación del nivel del mar, que se asocia al evento del Máximo Climático del Mioceno Medio y puede corresponder al ciclo global TM2.2. La presencia de la especie Actynocyclus ingens var. nodus asigna una edad de Mioceno medio, más específico entre los 13.0 y 15.6 Ma (Langhiano medio) al Miembro Los Indios de la Formación Rosarito Beach. Esta edad coincide con las fechas obtenidas de los basaltos subyacentes y sobreyacentes que dan 16.1 ± 2.1 y 14.3 ± 2.6 millones de años respectivamente.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract: The aim of the present study is to identify and analyze the paleoenvironmental and biostratigraphic aspects of the diatoms, in the sediments of the Mesa La Misión outcrop. The Mesa La Misión in Baja California is an outcrop of the Member Los Indios, part of the Rosarito Beach Formation. This formation consists of a volcanoclastic sequence with abundant and diverse vertebrate fauna named "La Misión Local Fauna". The presence of 15 different diatom species were found in samples taken from four stratigraphic levels of the Mesa La Misión outcrop. Deposition of the Los Indios Member occurred in a marine progradational platform. Benthic diatoms are abundant in the lower part of the sequence and become less abundant at higher stratigraphic levels. Most of the diatom species found indicate temperate waters. However, mixing of water may have been present due to some tropical and cold water specimens that were found. An increase of the deposition depth towards the top of the section was found. This was due to the occurrence of diatoms from different temperature gradients, combined with the reduction of benthic diatoms towards the top of the section. This sea level can be associated with the Middle Miocene Climatic Optimum. It may correspond to the global cycle TM 2.2. In addition, the presence of Actynocyclus ingens var. nodus , a biostratigraphical taxon, places the deposition of the sediments during the middle Miocene. More specifically, between 15.6 and 13.0 million years (middle Langhian). This age correlates with the radiometric dating of the underlaying and overlaying basalts dated 16.1 ± 2.1 and 14.3 ± 2.6, respectively.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[diatomeas]]></kwd>
<kwd lng="es"><![CDATA[La Misión]]></kwd>
<kwd lng="es"><![CDATA[Paleoecología]]></kwd>
<kwd lng="es"><![CDATA[Bioestratigrafía]]></kwd>
<kwd lng="es"><![CDATA[Rosarito Beach]]></kwd>
<kwd lng="en"><![CDATA[diatoms]]></kwd>
<kwd lng="en"><![CDATA[La Misión]]></kwd>
<kwd lng="en"><![CDATA[Paleoecology]]></kwd>
<kwd lng="en"><![CDATA[Biostratigraphy]]></kwd>
<kwd lng="en"><![CDATA[Rosarito Beach]]></kwd>
</kwd-group>
</article-meta>
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