<?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>S0185-38802017000400217</article-id>
<article-id pub-id-type="doi">10.7773/cm.v43i4.2793</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[Phytoplankton biomass and production off the Baja California Peninsula: 1997-2016]]></article-title>
<article-title xml:lang="es"><![CDATA[Biomasa y producción del fitoplancton frente a la península de Baja California: 1997-2016]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Cruz-Orozco]]></surname>
<given-names><![CDATA[Martín E De la]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Gómez-Ocampo]]></surname>
<given-names><![CDATA[Eliana]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Miranda-Bojórquez]]></surname>
<given-names><![CDATA[Luis E]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Cepeda-Morales]]></surname>
<given-names><![CDATA[Jushiro]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Durazo]]></surname>
<given-names><![CDATA[Reginaldo]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Lavaniegos]]></surname>
<given-names><![CDATA[Bertha E]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Espinosa-Carreón]]></surname>
<given-names><![CDATA[Teresa L]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Sosa-Ávalos]]></surname>
<given-names><![CDATA[Ramón]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Aguirre-Hernández]]></surname>
<given-names><![CDATA[Elsa]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Gaxiola-Castro]]></surname>
<given-names><![CDATA[Gilberto]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Michel-Villalobos]]></surname>
<given-names><![CDATA[Claudia]]></given-names>
</name>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Centro de Investigación Científica y de Educación Superior de Ensenada División de Oceanología ]]></institution>
<addr-line><![CDATA[Ensenada Baja California]]></addr-line>
<country>México</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad Autónoma de Nayarit  ]]></institution>
<addr-line><![CDATA[Tepic Nayarit]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Universidad Autónoma de Baja California Facultad de Ciencias Marinas ]]></institution>
<addr-line><![CDATA[ Baja California]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af4">
<institution><![CDATA[,Instituto Politécnico Nacional Centro Interdisciplinario de Investigación para el Desarrollo Integral Regional ]]></institution>
<addr-line><![CDATA[Guasave Sinaloa]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af5">
<institution><![CDATA[,Universidad de Colima Facultad de Ciencias Marinas ]]></institution>
<addr-line><![CDATA[Manzanillo Colima]]></addr-line>
<country>Mexico</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>43</volume>
<numero>4</numero>
<fpage>217</fpage>
<lpage>228</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S0185-38802017000400217&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S0185-38802017000400217&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S0185-38802017000400217&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract Between 1997 and 2016, the Investigaciones Mexicanas de la Corriente de California (IMECOCAL, Mexican Investigations of the California Current) program conducted measurements of chlorophyll a and phytoplankton production off Baja California. Here, we summarize the main results obtained during the survey period. Long-term means indicated that high productivity occurred along the coastal zone where upwelling occurs, and in a semi-permanent cyclonic gyre off Punta Eugenia. At the seasonal scale, the variability of integrated primary production showed differences with respect to integrated chlorophyll a variability. Integrated chlorophyll a exhibited maximum values during the coastal upwelling season in spring and summer, while minimum values occurred during the inflow of tropical-subtropical waters south of Punta Eugenia in autumn and winter. In contrast, the highest values of integrated primary production occurred in spring and summer to the north of Punta Eugenia, whereas to the south of this location, the highest values occurred in winter and autumn. This seasonal variability was associated with phytoplankton size and maximum photosynthetic rates. At the interannual scale, low productivity was associated with increased stratification during the subarctic water intrusion events and the &#8220;Blob&#8221; and El Niño events in 2015-2016. Productivity time-series were in agreement with the seasonal variability of the north Pacific Gyre Oscillation index. Given that phytoplankton is the first level of the marine food web, this study contributes to the understanding of regional variations in higher trophic levels at the seasonal and interannual scales.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen Entre 1997 y 2016, en el programa de Investigaciones Mexicanas de la Corriente de California (IMECOCAL) se realizaron mediciones de clorofila a y producción del fitoplancton frente a la península de Baja California. En este trabajo se resumen los resultados del periodo de observaciones. Se encontró que la productividad promedio fue alta en zonas de surgencias costeras, y en el giro ciclónico semipermanente frente a punta Eugenia. A escala estacional, la variación de la producción primaria fue diferente a la de la clorofila a integrada. La clorofila a integrada presentó máximos durante la época de surgencias costeras en primavera y verano, y mínimos durante la influencia de agua cálida de origen tropical-subtropical en la zona al sur de punta Eugenia en otoño e invierno. Los mayores valores de producción primaria integrada ocurrieron en primavera y verano al norte de punta Eugenia y en invierno y otoño al sur de esta localidad. Esta variabilidad se relacionó con la presencia de fitoplancton de ciertos tamaños y sus tasas fotosintéticas máximas características. A escala interanual, la menor productividad estuvo asociada con la mayor estratificación durante los eventos de intrusión de agua subártica, y los eventos el &#8220;Blob&#8221; y El Niño entre 2015 y 2016. Los cambios en la productividad observados concuerdan con la variación temporal del índice de la Oscilación del Giro del Pacifico Norte. La variabilidad observada en ambas escalas contribuye a entender la variación regional en niveles tróficos superiores, dado que el fitoplancton es el principal componente de la cadena trófica marina.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[integrated chlorophyll a]]></kwd>
<kwd lng="en"><![CDATA[integrated primary production]]></kwd>
<kwd lng="en"><![CDATA[California Current]]></kwd>
<kwd lng="en"><![CDATA[climatic variations]]></kwd>
<kwd lng="en"><![CDATA[North Pacific Gyre Oscillation]]></kwd>
<kwd lng="es"><![CDATA[clorofila a integrada]]></kwd>
<kwd lng="es"><![CDATA[producción primaria integrada]]></kwd>
<kwd lng="es"><![CDATA[corriente de California]]></kwd>
<kwd lng="es"><![CDATA[variabilidad climática]]></kwd>
<kwd lng="es"><![CDATA[Oscilación del Giro del Pacifico Norte]]></kwd>
</kwd-group>
</article-meta>
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