<?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>0185-3880</journal-id>
<journal-title><![CDATA[Ciencias marinas]]></journal-title>
<abbrev-journal-title><![CDATA[Cienc. mar]]></abbrev-journal-title>
<issn>0185-3880</issn>
<publisher>
<publisher-name><![CDATA[Universidad Autónoma de Baja California, Instituto de Investigaciones Oceanológicas]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S0185-38802018000300203</article-id>
<article-id pub-id-type="doi">10.7773/cm.v44i3.2833</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[The carbonate system in coastal waters off the northern region of the Baja California Peninsula under La Niña conditions]]></article-title>
<article-title xml:lang="es"><![CDATA[El sistema de carbonatos en aguas costeras del norte de la península de Baja California bajo condiciones de La Niña]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Oliva-Méndez]]></surname>
<given-names><![CDATA[Norma]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
<xref ref-type="aff" rid="Aaf"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Delgadillo-Hinojosa]]></surname>
<given-names><![CDATA[Francisco]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Pérez-Brunius]]></surname>
<given-names><![CDATA[Paula]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Valencia-Gasti]]></surname>
<given-names><![CDATA[Augusto]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Huerta-Diaz]]></surname>
<given-names><![CDATA[Miguel A]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Palacios-Coria]]></surname>
<given-names><![CDATA[Eduardo]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Hernández-Ayón]]></surname>
<given-names><![CDATA[J Martín]]></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 de Baja California Instituto de Investigaciones Oceanológicas ]]></institution>
<addr-line><![CDATA[Ensenada Baja California]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Centro de Investigación Científica y de Educación Superior de Ensenada Departamento de Oceanografía Biológica ]]></institution>
<addr-line><![CDATA[Ensenada Baja California]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af4">
<institution><![CDATA[,Estación de Investigación Oceanográfica  ]]></institution>
<addr-line><![CDATA[Ensenada Baja California]]></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>44</volume>
<numero>3</numero>
<fpage>203</fpage>
<lpage>220</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S0185-38802018000300203&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S0185-38802018000300203&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S0185-38802018000300203&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract In the North Pacific, variations in isopycnal depth influence the biogeochemical characteristics of the water column and the aragonite saturation horizon (Z&#937;a) during interannual events. The objective of this study was to assess the effect of the 2011 La Niña conditions on Z&#937;a in Todos Santos Bay (Baja California, Mexico) and surrounding waters. The results showed that Z&#937;a variability was modulated by the intensity of interannual conditions and by the water masses that were present in the region. Subarctic Water predominated in the upper 200 m with anomalous characteristics, such as low temperature and low salinity. Also, isopycnals shoaled toward the coast and Z&#937;a was thus ~30 m in the nearshore area, in contrast with the oceanic region, where Z&#937;a was ~150 m. Prior to this study, there were no records of Z&#937;a in Todos Santos Bay, nor were there any records of its shallowness.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen En el Pacífico Norte se presentan variaciones en la profundidad de las isopicnas durante eventos interanuales que influyen en las características biogeoquímicas de la columna de agua y en el horizonte de saturación del aragonita (Z&#8486;a). El objetivo de este trabajo fue evaluar el efecto de las condiciones de La Niña de 2011 sobre el Z&#8486;a en la bahía de Todos Santos (Baja California, México) y aguas adyacentes. Los resultados mostraron que la variabilidad del Z&#8486;a estuvo modulada por la intensidad de las condiciones interanuales y por las masas de agua que se presentaron en la región. En los primeros 200 m superficiales predominó el Agua del Subártico con características anómalas de baja temperatura y baja salinidad. Asimismo, se observó un ascenso de las isopicnas con dirección a la costa y, por tanto, el Z&#8486;a fue de ~30 m en la zona más cercana a la costa, en contraste con la región más oceánica, donde el Z&#8486;a fue de ~150 m. Antes del presente estudio, no se tenían registros del Z&#8486;a para la zona dentro de la bahía de Todos Santos, tampoco de que pudiera ser somero.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[upwelling]]></kwd>
<kwd lng="en"><![CDATA[aragonite saturation horizon]]></kwd>
<kwd lng="en"><![CDATA[Todos Santos Bay]]></kwd>
<kwd lng="en"><![CDATA[ocean acidification]]></kwd>
<kwd lng="es"><![CDATA[surgencia]]></kwd>
<kwd lng="es"><![CDATA[horizonte de saturación del aragonita]]></kwd>
<kwd lng="es"><![CDATA[bahía de Todos Santos]]></kwd>
<kwd lng="es"><![CDATA[acidificación del océano]]></kwd>
</kwd-group>
</article-meta>
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