<?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>S1405-33222017000100175</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Estratigrafía y Sedimentología del relleno detrítico del estuario del Río Urumea (Donostia-San Sebastián, España)]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Edeso-Fito]]></surname>
<given-names><![CDATA[José Miguel]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
<xref ref-type="aff" rid="Aaf"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Soria-Jáuregui]]></surname>
<given-names><![CDATA[Ángel]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Lopetegi-Galarraga]]></surname>
<given-names><![CDATA[Ane]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Mujika-Alustiza]]></surname>
<given-names><![CDATA[José Antonio]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Ruiz-Alonso]]></surname>
<given-names><![CDATA[Mónica]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad del País Vasco Departamento de Ingeniería Minera y Metalúrgica y Ciencias de los Materiales ]]></institution>
<addr-line><![CDATA[Bilbao ]]></addr-line>
<country>Spain</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad del País Vasco Departamento de Geografía, Prehistoria y Arqueología ]]></institution>
<addr-line><![CDATA[Gasteiz ]]></addr-line>
<country>Spain</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Consejo Superior de Investigaciones Científicas Centro de Ciencias Humanas y Sociales ]]></institution>
<addr-line><![CDATA[Madrid ]]></addr-line>
<country>Spain</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>00</month>
<year>2017</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>00</month>
<year>2017</year>
</pub-date>
<volume>69</volume>
<numero>1</numero>
<fpage>175</fpage>
<lpage>197</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1405-33222017000100175&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1405-33222017000100175&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1405-33222017000100175&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen El análisis y caracterización del relleno sedimentario del estuario del Urumea permite diferenciar 2 sucesiones deposicionales distintas, separadas por un largo período cronológico sin registro sedimentario. La primera de estas sucesiones, de edad Pleistocena (&gt; 43500 BP), está formada por una facies palustre sobre la que se desarrollan facies fluvio-estuarinas, señalando un nivel marino similar o algo más bajo que el actual, lo que permite descartar las fases más frías del Pleistoceno. Sobre esta sucesión se desarrolla otra de edad Holocena que abarca el período comprendido entre el 7040 ± 30 BP (7565-7390 cal. BP) y la época actual. Se reconocen 3 pulsos transgresivos separados o seguidos por fases de estabilización o de regresión. La primera fase transgresiva se inició con anterioridad al 7040 ± 30 BP (7565-7390 cal. BP) y ya había concluido en el 5200 ± 30 BP (5995-5910 cal. BP). Alrededor de esta última fecha tiene lugar una breve pulsación regresiva que sitúa el nivel del mar varios metros por debajo de su posición actual. A partir del 5200 ± 30 BP (5995-5910 cal. BP) se constata un rápido ascenso del nivel del mar, seguido de una fase de estabilización primero y de discreta regresión después, que es aprovechada por grupos humanos para construir 2 rampas de uso desconocido. La cronología de esta fase regresiva se sitúa en torno al 4710 ± 30 BP (4945-4650 cal. BP). Una nueva pulsación transgresiva tiene lugar a partir del 3000 BP prolongándose mediante una suave elevación hasta el 1240 ± 30 BP (1190-1065 cal.BP). La estabilización (y quizás una nueva oscilación en época histórica) del nivel del mar a partir de esta fecha favorece la colmatación del estuario, lo que unido a la formación de un tómbolo en la margen izquierda determina el desarrollo de un estuario semi-cerrado que pervive hasta la actualidad.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract Two different depositional phases can be identified in the Urumea estuarine infill. They were chronologically separated by a long period without sedimentological evidence. The first one, Pleistocene in age (&gt; 43500 BP), is composed of a marsh facies overlaid by fluvio-estuarine facies. This could indicate that the sea level at the time was similar or slightly lower than the present parameter. The later information rules out the coldest stages of the Pleistocene as their origin. On top of the uppermost Pleistocene layer, a Holocene sequence developed which extends from 7040 ± 30 BP (7565-7390 cal. BP) to modern times. In this part of the infill, 3 transgressive pulses can be identified, separated or followed by phases of sea level stabilization or even regression. The first pulse began before 7040 ± 30 BP (7565-7390 cal. BP) and extended to 5200 ± 30 BP (5995-5910 cal. BP). The first regressive pulse took place around the last date, placing the shoreline a few meters below its present position. After 5200 ± 30 BP (5995-5910 cal. BP), a fast sea level rise can be recorded, followed by a stabilisation phase first. Also, a minor regression happened afterwards, which was used by local communities to build two ramps of unknown utility. This regressive pulse was dated 4710 ± 30 BP (4945-4650 cal. BP). A new transgressive pulse took place after 3000 BP extending through a gentle sea level rise to 1240 ± 30 BP (1190-1065 cal. BP). From this date, sea level stabilisation (and maybe a new transgression in historical times) favoured the total infilling of the estuary, which, together with the development of a tombolo on the left bank, induced the formation of a semi-enclosed estuary which can still be observed nowadays.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[Holoceno]]></kwd>
<kwd lng="es"><![CDATA[Pleistoceno]]></kwd>
<kwd lng="es"><![CDATA[transgresión]]></kwd>
<kwd lng="es"><![CDATA[regresión]]></kwd>
<kwd lng="es"><![CDATA[nivel del mar]]></kwd>
<kwd lng="es"><![CDATA[rampas antrópicas]]></kwd>
<kwd lng="en"><![CDATA[Holocene]]></kwd>
<kwd lng="en"><![CDATA[Pleistocene]]></kwd>
<kwd lng="en"><![CDATA[transgression]]></kwd>
<kwd lng="en"><![CDATA[regression]]></kwd>
<kwd lng="en"><![CDATA[sea level]]></kwd>
<kwd lng="en"><![CDATA[anthropic ramps]]></kwd>
</kwd-group>
</article-meta>
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