<?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>1026-8774</journal-id>
<journal-title><![CDATA[Revista mexicana de ciencias geológicas]]></journal-title>
<abbrev-journal-title><![CDATA[Rev. mex. cienc. geol]]></abbrev-journal-title>
<issn>1026-8774</issn>
<publisher>
<publisher-name><![CDATA[Universidad Nacional Autónoma de México, Instituto de Geología]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S1026-87742018000100093</article-id>
<article-id pub-id-type="doi">10.22201/cgeo.20072902e.2018.1.531</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Estudio palinológico de un perfil sedimentario del Holoceno medio-tardío, oeste del Iberá, Corrientes, Argentina]]></article-title>
<article-title xml:lang="en"><![CDATA[Palynological study of a sedimentary profile from the middle-late Holocene, western Iberá, Corrientes, Argentina]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Fernandez Pacella]]></surname>
<given-names><![CDATA[Lionel]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad Nacional del Nordeste  ]]></institution>
<addr-line><![CDATA[Corrientes ]]></addr-line>
<country>Argentina</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>35</volume>
<numero>1</numero>
<fpage>93</fpage>
<lpage>101</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1026-87742018000100093&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1026-87742018000100093&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1026-87742018000100093&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen: Con la denominación "Iberá", identificamos a uno de los humedales tropicales más importantes de la biósfera en términos de su extensión y de las especies que lo habitan, tanto animales como vegetales. El objetivo de este trabajo es a partir del análisis polínico y litológico de un perfil sedimentario, reconstruir las comunidades vegetales predominantes y sus variaciones, inferir los cambios en las condiciones climáticas que se habrían producido y deducir el ambiente deposicional durante el Holoceno medio y tardío en la región del Iberá. El perfil fue muestreado sobre una barranca ubicada en la zona central de la margen occidental del Sistema Iberá, en la localidad de San Miguel. La dinámica de la vegetación y la relación de los taxones permitieron establecer tres zonas polínicas: La Zona Polínica I (Holoceno medio) presenta una asociación característica de la estepa graminosa. Las litofacies identificadas sugieren un ambiente depositacional de valles anegadizos, que junto a las paleocomunidades vegetales reconocidas, señalarían para el Holoceno medio, condiciones húmedas. Las Zonas Polínicas II y III (Holoceno tardío) registran una asociación característica de estepa herbácea psamófila. El aumento observado en las Brassicaceae, estaría indicando disturbios ambientales, los cuales podrían reflejar la combinación de una intensa acción eólica bajo un clima árido. Las litofacies identificadas señalan un ambiente eólico con derrames fluviales y junto a las comunidades vegetales reconocidas, indicarían para el Holoceno tardío, condiciones áridas a semiáridas.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract: With the denomination "Iberá", we identify one of the most important tropical wetlands of the biosphere in terms of its extension and living species, both animal and vegetal. The objective of this paper is to reconstruct the predominant plant communities and their variations, infer the changes in the climatic conditions that would have occurred and to deduce the depositional environment during the middle and late Holocene in the Iberá region. The profile was sampled in a ravine located in the central zone of the western margin of the Iberá System, in the locality of San Miguel. The dynamics of the vegetation and the relation of the taxa allowed establishing three pollen zones: Pollen Zone I (middle Holocene) presents a characteristic association of steppe grass. The identified lithofacies suggests a depositional environment of waterlogged valleys, which together with the recognized vegetal palaeocommunities, would indicate humid conditions for the middle Holocene. Pollen Zones II and III (late Holocene) show an association characteristic of the herbaceous psammophyte steppe. The observed Brassicaceae increase would indicate environmental disturbances, which could reflect the combination of intense wind action under an arid climate. The identified lithofacies give evidence for an eolian environment with fluvial spills and indicate together with the recognized vegetal communities, arid to semi-arid conditions for the late Holocene.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[alinología]]></kwd>
<kwd lng="es"><![CDATA[Holoceno]]></kwd>
<kwd lng="es"><![CDATA[Iberá]]></kwd>
<kwd lng="es"><![CDATA[reconstrucción]]></kwd>
<kwd lng="es"><![CDATA[ambiente]]></kwd>
<kwd lng="es"><![CDATA[clima]]></kwd>
<kwd lng="es"><![CDATA[Argentina]]></kwd>
<kwd lng="en"><![CDATA[palynology]]></kwd>
<kwd lng="en"><![CDATA[Holocene]]></kwd>
<kwd lng="en"><![CDATA[Iberá]]></kwd>
<kwd lng="en"><![CDATA[reconstruction]]></kwd>
<kwd lng="en"><![CDATA[environment]]></kwd>
<kwd lng="en"><![CDATA[Climate]]></kwd>
<kwd lng="en"><![CDATA[Argentina]]></kwd>
</kwd-group>
</article-meta>
</front><back>
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