<?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>S0185-38802023000100101</article-id>
<article-id pub-id-type="doi">10.7773/cm.y2023.3370</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[Influence of a cyclonic gyre and a thermohaline front on the population structure of Centropages furcatus in Bay of La Paz, Gulf of California]]></article-title>
<article-title xml:lang="es"><![CDATA[Influencia de un giro ciclónico y un frente termohalino en la estructura poblacional de Centropages furcatus en la bahía de La Paz, golfo de California]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Mojica-Ramírez]]></surname>
<given-names><![CDATA[Erika]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Monreal-Gómez]]></surname>
<given-names><![CDATA[María Adela]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Hernández-Trujillo]]></surname>
<given-names><![CDATA[Sergio]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Salas-de-León]]></surname>
<given-names><![CDATA[David Alberto]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad Nacional Autónoma de México  ]]></institution>
<addr-line><![CDATA[Mexico City ]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad Nacional Autónoma de México Instituto de Ciencias del Mar y Limnología Unidad Académica de Ecología y Biodiversidad Acuática]]></institution>
<addr-line><![CDATA[Mexico City ]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Instituto Politécnico Nacional Centro Interdisciplinario de Ciencias Marinas ]]></institution>
<addr-line><![CDATA[La Paz Baja California Sur]]></addr-line>
<country>Mexico</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>12</month>
<year>2023</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>12</month>
<year>2023</year>
</pub-date>
<volume>49</volume>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S0185-38802023000100101&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S0185-38802023000100101&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S0185-38802023000100101&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract. The population structure of Centropages furcatus associated with hydrographic structures in late spring 2004 was analyzed. The distribution of the different copepodite stages of C. furcatus was analyzed from zooplankton samples obtained with a bongo net. The hydrography and geostrophic velocity in Bay of La Paz relative to the bottom depth revealed the presence of a cyclonic gyre in the Alfonso basin area and a thermohaline front near Boca Grande. The distribution of vertically integrated chlorophyll a concentration showed maximum values at the center of the gyre and in the region of the front, making evident that both hydrographic structures stimulated biological productivity because of the flux of nutrients into the euphotic layer in the gyre and the nutrient accumulation in the thermohaline front. The results showed that the spatial variation of C. furcatus was influenced by both hydrographic structures. The differential distribution of the copepodite stages was noticeable in the cyclonic gyre, with the highest density for the first copepodite stages at the center of the gyre because of the high chlorophyll a concentration due to the nutrient enrichment in the euphotic layer, as a result of Ekman pumping. Copepod density was higher in the thermohaline front than inside the cyclonic gyre because the front serves as a reproductive spot for the species, maintaining a stable adult population density inside the bay and in the Gulf of California.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen. Se analizó la estructura poblacional de Centropages furcatus asociada a estructuras hidrográficas a finales de la primavera de 2004. La distribución de los diferentes estadios de copepoditos de C. furcatus fue analizada a partir de las muestras de zooplancton obtenidas con una red bongo. En la bahía de La Paz, la hidrografía y la velocidad geostrófica relativa al fondo revelaron la presencia de un giro ciclónico en la cuenca Alfonso y un frente termohalino cerca de Boca Grande. La distribución de la concentración de clorofila a integrada verticalmente mostró valores máximos en el centro del giro y en la región del frente, lo que evidenció que ambas estructuras hidrográficas favorecen la productividad biológica debido al flujo de nutrientes hacia la capa eufótica en el giro y a la acumulación de nutrientes en el frente termohalino. Los resultados mostraron que la variación espacial de C. furcatus estuvo influenciada por ambas estructuras hidrográficas. En el giro ciclónico se observó una distribución diferencial por etapa de desarrollo, con mayor densidad poblacional de los primeros estadios de copepoditos en el centro del giro, como consecuencia de la alta concentración de clorofila a por el enriquecimiento de nutrientes en la capa eufótica, debido al bombeo de Ekman. La densidad poblacional de copépodos fue mayor en el frente termohalino que en el interior del giro ciclónico, debido a que el frente actúa como una zona reproductiva de la especie que mantiene una densidad poblacional estable para los adultos de la bahía y del golfo de California.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[copepodites]]></kwd>
<kwd lng="en"><![CDATA[Centropages furcatus]]></kwd>
<kwd lng="en"><![CDATA[community structure]]></kwd>
<kwd lng="en"><![CDATA[thermohaline front]]></kwd>
<kwd lng="en"><![CDATA[Bay of La Paz]]></kwd>
<kwd lng="es"><![CDATA[copepoditos]]></kwd>
<kwd lng="es"><![CDATA[Centropages furcatus]]></kwd>
<kwd lng="es"><![CDATA[estructura de la comunidad]]></kwd>
<kwd lng="es"><![CDATA[frente termohalino]]></kwd>
<kwd lng="es"><![CDATA[bahía de La Paz]]></kwd>
</kwd-group>
</article-meta>
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