<?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>1659-4266</journal-id>
<journal-title><![CDATA[Cuadernos de Investigación UNED]]></journal-title>
<abbrev-journal-title><![CDATA[Cuadernos de Investigación UNED]]></abbrev-journal-title>
<issn>1659-4266</issn>
<publisher>
<publisher-name><![CDATA[Universidad Estatal a Distancia de Costa Rica]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S1659-42662019000100024</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[Climate change and tropical marine ecosystems: A review with an emphasis on coral reefs]]></article-title>
<article-title xml:lang="es"><![CDATA[El cambio climático y los ecosistemas marinos tropicales: una revisión con énfasis en los arrecifes de coral]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Kleypas]]></surname>
<given-names><![CDATA[Joan A.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,National Center for Atmospheric Research  ]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
<country>USA</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>03</month>
<year>2019</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>03</month>
<year>2019</year>
</pub-date>
<volume>11</volume>
<numero>1</numero>
<fpage>24</fpage>
<lpage>35</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.sa.cr/scielo.php?script=sci_arttext&amp;pid=S1659-42662019000100024&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.sa.cr/scielo.php?script=sci_abstract&amp;pid=S1659-42662019000100024&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.sa.cr/scielo.php?script=sci_pdf&amp;pid=S1659-42662019000100024&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract Climate change is usually associated with warming and weather extremes that impact the human environment and terrestrial systems, but it also has profound effects on the ocean, which is probably the most unique, life-supporting feature of planet Earth. The most direct consequence of rising CO2 concentration in the atmosphere is &#8220;ocean acidification,&#8221; a term that refers to the lowering of seawater pH, but encompasses a suite of chemical changes that affect marine organisms from shell formation, to reproduction, physiology, and behavior. The oceans are also warming in pace with the atmosphere, and in fact store the vast majority of the additional heat generated by rising CO2 and other greenhouse gases in the atmosphere. This warming is causing the more mobile marine species to redistribute poleward and deeper, and is causing high mortality in more sessile species such as those that build and habituate coral reefs. But warming is also leading to a decrease in dissolved oxygen in the oceans. For tropical marine ecosystems, the combination of ocean acidification, warming, and deoxygenation will continue to impact marine ecosystems in the future. The extent of these impacts depends on which energy pathway society follows, and our abilities to reduce other stressors and assist the rate at which species can adapt and migrate to more suitable environments.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen El cambio climático generalmente está asociado con el calentamiento y las condiciones climáticas extremas que impactan el ambiente humano y los sistemas terrestres, pero también tiene profundos efectos en el océano, que es probablemente la característica más importante del planeta Tierra para mantener la vida. La consecuencia más directa del aumento de la concentración de CO2 en la atmósfera es la "acidificación del océano", que se refiere a la disminución del pH del agua de mar, pero abarca un conjunto de cambios químicos que afectan a los organismos marinos desde la formación de conchas hasta la reproducción, fisiología y comportamiento. Los océanos también se están calentando como la atmósfera, y de hecho almacenan la gran mayoría del calor adicional generado por el aumento de CO2 y otros gases de efecto invernadero en la atmósfera. Este calentamiento está causando que las especies marinas más móviles se redistribuyan hacia los polos y a más profundidad, y está causando una alta mortalidad en especies más sésiles, como las que construyen y habitúan los arrecifes de coral. Pero el calentamiento también está conduciendo a una disminución del oxígeno disuelto en los océanos. Para los ecosistemas marinos tropicales, la combinación de acidificación, calentamiento y desoxigenación de los océanos continuará afectando los ecosistemas marinos en el futuro. El alcance de estos impactos depende de la ruta energética que siga la sociedad y de nuestra capacidad para reducir otros factores estresantes y ayudar a la velocidad a la que las especies pueden adaptarse y migrar a entornos más adecuados.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[oceans]]></kwd>
<kwd lng="en"><![CDATA[climate change]]></kwd>
<kwd lng="en"><![CDATA[ocean acidification]]></kwd>
<kwd lng="en"><![CDATA[ocean warming]]></kwd>
<kwd lng="en"><![CDATA[ocean deoxygenation]]></kwd>
<kwd lng="es"><![CDATA[océanos]]></kwd>
<kwd lng="es"><![CDATA[cambio de clima]]></kwd>
<kwd lng="es"><![CDATA[acidificación de océano]]></kwd>
<kwd lng="es"><![CDATA[calentamiento de océano]]></kwd>
<kwd lng="es"><![CDATA[desoxigenación]]></kwd>
</kwd-group>
</article-meta>
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