<?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>S1405-33222019000300773</article-id>
<article-id pub-id-type="doi">10.18268/bsgm2019v71n3a9</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[Systematic paleontology and taphonomic studies of Ypresian mollusks at the Kopet-Dagh Basin, NE Iran]]></article-title>
<article-title xml:lang="es"><![CDATA[Paleontología sistemática y estudios tafonómicos de los moluscos del Ypresiano en la Cuenca de Kopet-Dagh, NE Irán]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Salahi]]></surname>
<given-names><![CDATA[Amir]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Ghaderi]]></surname>
<given-names><![CDATA[Abbas]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Ashouri]]></surname>
<given-names><![CDATA[Ali Reza]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Cristín]]></surname>
<given-names><![CDATA[Alejandro]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Senemari]]></surname>
<given-names><![CDATA[Saeedeh]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Ferdowsi University of Mashhad Faculty of Sciences Department of Geology]]></institution>
<addr-line><![CDATA[ Mashhad]]></addr-line>
<country>Iran</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad Nacional Autónoma de México Instituto de Geología ]]></institution>
<addr-line><![CDATA[ CDMX]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Imam Khomeini International University Faculty of Technical &amp; Engineering ]]></institution>
<addr-line><![CDATA[ Qazvin]]></addr-line>
<country>Iran</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>00</month>
<year>2019</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>00</month>
<year>2019</year>
</pub-date>
<volume>71</volume>
<numero>3</numero>
<fpage>773</fpage>
<lpage>804</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1405-33222019000300773&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1405-33222019000300773&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1405-33222019000300773&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract Marine invertebrate fossils have long been considered important tools for age dating and stratigraphic interpretation of the Paleogene deposits of Central Asia, however information has not yet been provided from the Kopet-Dagh Basin (NE Iran). In this research, fossiliferous horizons of the Chehelkaman Formation at the Sheikh and Ghaleh-Zou sections (which have never been recognized previously), both in the Sheikh Syncline area, are discussed. These sedimentary beds overlay the terrestrial siliciclastic Pesteligh Formation and are the first evidence of marine flooding of the Paleogene transgression in the central Kopet-Dagh. Systematic paleontological studies of molluscan fossils in this succession led to the identification of ten genera, twelve species and two subspecies of bivalves and five genera and five species of gastropods. The assemblage belongs to four different fossilif-erous horizons: (1) Turritellidae Dominated Assemblage (TDA), (2) Pycnodonte - Turkostrea horizon, (3) Cordiopsis-Cardium horizon and (4) Globularia shell beds in the Sheikh section and only TDA horizon in the Ghaleh-Zou section. The age of the whole succession, based on Cordiopsis subathooensis - Turritella subathooensis Zone cooccurrence with nannofossil zones NP12 and NP13, is Late Ypresian (early middle Cuisian). The TDA in both sections confirms the abundance of nutrients and their bimodal orientation demonstrates effects of oscillatory waves rather than unidirectional paleo-currents. High rates of bioerosion, encrustation, fragmentation, disarticulation and corrosion of the shells in the Pycnodonte - Turkostrea horizon reveals high volumes of nutrients and energy-rich conditions. This interval, overlain by the Cordiopsis - Cardium horizon in a pavement arrangement, represents the stable conditions after a storm. The Globularia shell beds inter-bedded with marly beds indicate stability and a deepening trend of the environment, terminating to deeper marine shales and marls of the Khangiran Formation.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen Los fósiles de invertebrados marinos se han considerado herramientas importantes para la recolecta de datos por edades y la interpretación estratigráfica de los depósitos de paleógenos de Asia Central, sin embargo, aún no se ha proporcionado información de la cuenca de Kopet-Dagh (NE Irán). En esta investigación, se discuten los horizontes fosilíferos de la Formación Chehelkaman en las secciones Sheikh y Ghaleh-Zou (que nunca antes se habían reconocido), ambos en el área Sheikh Syncline. Estos lechos sedimentarios se superponen a la Formación de Pesteligh siliciclástica terrestre y son la primera evidencia de inundación marina de la transgresión del Paleógeno en el centro de Kopet-Dagh. Los estudios paleontológicos sistemáticos de fósiles de moluscos en esta sucesión condujeron a la identificación de: diez géneros, doce especies, dos subespecies de bivalvos, cinco géneros y cinco especies de gasterópodos. El conjunto pertenece a cuatro horizontes fosilíferos diferentes: (1) Conjunto Dominado por Turritellidae (TDA), (2) Pycnodonte-Turkostrea horizonte, (3) Cordiopsis - Cardium horizonte, (4) Camas de concha Globularia en la sección Sheikh y solo horizonte TDA en la sección de Ghaleh-Zou. La edad de toda la sucesión es Ypresian tardío (Cuisian medio temprano). Ésta edad está basada en Cordiopsis subathooensis - Turritella subathooensis co-ocurrencia de la zona con las zonas de nannofósiles NP12 y NP13. El TDA en ambas secciones confirma la abundancia de nutrientes y su orientación bimodal demuestra los efectos de las ondas oscilatorias en lugar de las paleocorrientes unidireccionales. Las altas tasas de bioerosión, incrustación, fragmentación, desarticulación y corrosión de las conchas en Pycnodonte - Turkostrea horizonte revela altos volúmenes de nutrientes y condiciones ricas en energía. Este intervalo, cubierto por la Cordiopsis - Cardium horizonte en una disposición de pavimento, representa las condiciones estables después de una tormenta. Los lechos de conchas de Globularia intercalados con lechos de marga, indican estabilidad y una tendencia cada vez más profunda del medio ambiente terminando en lutitas y margas más profundas de la Formación Khangiran.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[Taphonomy]]></kwd>
<kwd lng="en"><![CDATA[paleoenvironment]]></kwd>
<kwd lng="en"><![CDATA[Early Eocene]]></kwd>
<kwd lng="en"><![CDATA[Kopet-Dagh Basin]]></kwd>
<kwd lng="en"><![CDATA[Chehelkaman Formation]]></kwd>
<kwd lng="es"><![CDATA[Tafonomía]]></kwd>
<kwd lng="es"><![CDATA[paleo-ambiente]]></kwd>
<kwd lng="es"><![CDATA[Eoceno temprano]]></kwd>
<kwd lng="es"><![CDATA[cuenca de Kopet-Dagh]]></kwd>
<kwd lng="es"><![CDATA[Formación Chehelkaman]]></kwd>
</kwd-group>
</article-meta>
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