<?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>0122-9761</journal-id>
<journal-title><![CDATA[Boletín de Investigaciones Marinas y Costeras - INVEMAR]]></journal-title>
<abbrev-journal-title><![CDATA[Bol. Invest. Mar. Cost.]]></abbrev-journal-title>
<issn>0122-9761</issn>
<publisher>
<publisher-name><![CDATA[INSTITUTO DE INVESTIGACIONES MARINAS Y COSTERAS "JOSE BENITO VIVES DE ANDRÉIS" (INVEMAR)    INSTITUTO DE INVESTIGACIONES MARINAS Y COSTERAS -JOSE BENITO VIVES DE ANDRÉIS- (INVEMAR)]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S0122-97612020000300167</article-id>
<article-id pub-id-type="doi">10.25268/bimc.invemar.2020.49.suplesp.1088</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[Dynamics of the benthic community structure on the shallow coral formations of the San Bernardo Archipelago, Colombian Caribbean]]></article-title>
<article-title xml:lang="es"><![CDATA[Dinámica de la estructura de la comunidad bentónica en las formaciones coralinas someras del archipiélago de San Bernardo, Caribe colombiano]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Vega-Sequeda]]></surname>
<given-names><![CDATA[Johanna]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Agudelo-Ramírez]]></surname>
<given-names><![CDATA[Claudia]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Mendoza-Mazzeo]]></surname>
<given-names><![CDATA[Álvaro]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Sanjuan-Muñoz]]></surname>
<given-names><![CDATA[Adolfo]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Investigador independiente  ]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
<country>Colombia</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Sanjuan y Asociados Ltda.  ]]></institution>
<addr-line><![CDATA[Santa Marta Magdalena]]></addr-line>
<country>Colombia</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Hyser Ltda.  ]]></institution>
<addr-line><![CDATA[Barranquilla ]]></addr-line>
<country>Colombia</country>
</aff>
<aff id="Af4">
<institution><![CDATA[,Universidad Jorge Tadeo Lozano  ]]></institution>
<addr-line><![CDATA[Santa Marta El Rodadero]]></addr-line>
<country>Colombia</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>12</month>
<year>2020</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>12</month>
<year>2020</year>
</pub-date>
<volume>49</volume>
<fpage>167</fpage>
<lpage>192</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.co/scielo.php?script=sci_arttext&amp;pid=S0122-97612020000300167&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.co/scielo.php?script=sci_abstract&amp;pid=S0122-97612020000300167&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.co/scielo.php?script=sci_pdf&amp;pid=S0122-97612020000300167&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT Coral reefs have experienced an extensive degradation over the last decades as a result of anthropogenic and natural disturbances. This study presents an historical characterization (1989-2015) of changes in composition of the substrate in coral formations in the San Bernardo Archipelago. In addition, in 2015 coral reef health (presence of deterioration signs) was evaluated, and satellite temperature data were analyzed. In general, coral cover showed a stable trend between 1989 and 2010. The observed differences in the coral reef formations in 2013 and 2015 could have been due to the increase in coverage of species of the genus Orbicella, Porites, Agaricia, Siderastrea and the hydrocoral Millepora complanata. The lower coverage in 1989, 1991 and 2005 was possibly related to massive mortality events of reef species due to diseases and bleaching. Abiotic substrate and algal cover exhibited opposing behavior, and algae became the dominant component of the substrate since 2013. Spatially, there were different trends: stations at Ceycen, Tintipán and Mangle presented better coral development conditions over time, while stations at Cabruna and Palma, closer to urban centers, showed signs of deterioration. In addition, temperatures above the bleaching tolerance threshold (29.4 °C) were recorded since June 2015, which is possibly why corals faced thermal stress and bleached in 18 of the 19 evaluated stations. Management actions on local impacts are essential, accompanied by information provided by monitoring programs, so that coral reefs can recover from the natural and anthropogenic impacts that affect them.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN Los arrecifes de coral han sufrido una extensa degradación en las últimas décadas como resultado de perturbaciones antropogénicas y naturales. Este estudio presenta una caracterización histórica (1989-2015) de los cambios en la composición del sustrato en formaciones coralinas en el archipiélago de San Bernardo. Adicionalmente, en el 2015 se evaluó la salud arrecifal (presencia de signos de deterioro) y se analizaron datos satelitales de temperatura. En general, la cobertura de coral mostró una tendencia estable entre 1989 y 2010. En 2013 y 2015 se registraron diferencias en el ensamblaje coralino las cuales pueden estar asociadas al incremento en la cobertura de las especies de los géneros Orbicella, Porites, Agaricia, Siderastrea y del hidrocoral Millepora complanata. Las menores coberturas observadas en 1989, 1991 y 2005 estuvieron posiblemente relacionados con eventos de mortalidades masivas de especies arrecifales por enfermedades y blanqueamiento. Se registró un comportamiento opuesto entre el sustrato abiótico y las algas, siendo este último grupo el componente dominante del sustrato desde el 2013. Espacialmente se presentaron diferentes tendencias. Las estaciones en Ceycen, Tintipán y Mangle presentaron mejores condiciones de desarrollo coralino en el tiempo, mientras que las estaciones en Cabruna y Palma, lugares más cercanos a los centros urbanos, presentaron indicios de tendencia hacia el deterioro. Adicionalmente, a partir de junio del 2015 se registraron valores de temperatura por encima del umbral de tolerancia al blanqueamiento (29,4 °C), por lo que posiblemente los corales enfrentaron un estrés térmico que causó blanqueamiento en 18 de las 19 estaciones evaluadas. Son esenciales las acciones de gestión sobre los impactos locales, acompañados de la información suministrada por los programas de monitoreo, para que los arrecifes puedan recuperarse de los impactos naturales y antropogénicos que los afectan.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[coral reefs]]></kwd>
<kwd lng="en"><![CDATA[coral monitoring]]></kwd>
<kwd lng="en"><![CDATA[reef cover]]></kwd>
<kwd lng="en"><![CDATA[Corales del Rosario y San Bernardo Natural National Park]]></kwd>
<kwd lng="en"><![CDATA[Colombian Caribbean.]]></kwd>
<kwd lng="es"><![CDATA[arrecifes coralinos]]></kwd>
<kwd lng="es"><![CDATA[monitoreo coralino]]></kwd>
<kwd lng="es"><![CDATA[cobertura arrecifal]]></kwd>
<kwd lng="es"><![CDATA[Parque Nacional Natural Corales del Rosario y San Bernardo]]></kwd>
<kwd lng="es"><![CDATA[Caribe colombiano]]></kwd>
</kwd-group>
</article-meta>
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