<?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>0187-5779</journal-id>
<journal-title><![CDATA[Terra Latinoamericana]]></journal-title>
<abbrev-journal-title><![CDATA[Terra Latinoam]]></abbrev-journal-title>
<issn>0187-5779</issn>
<publisher>
<publisher-name><![CDATA[Sociedad Mexicana de la Ciencia del Suelo A.C.]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S0187-57792016000300253</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[Soil respiration in Mexico: Advances and future directions]]></article-title>
<article-title xml:lang="es"><![CDATA[Respiración de suelo en México: Avances y direcciones futuras]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Cueva]]></surname>
<given-names><![CDATA[Alejandro]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Robles Zazueta]]></surname>
<given-names><![CDATA[Carlos A.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Garatuza Payan]]></surname>
<given-names><![CDATA[Jaime]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Yépez]]></surname>
<given-names><![CDATA[Enrico A.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Centro de Investigación Científica y de Educación Superior de Ensenada Departamento de Biología de la Conservación ]]></institution>
<addr-line><![CDATA[Ensenada Baja California]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad de Sonora Departamento de Investigaciones Científicas y Tecnológicas ]]></institution>
<addr-line><![CDATA[Hermosillo Sonora]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Instituto Tecnológico de Sonora Departamento de Ciencias del Agua y Medio Ambiente ]]></institution>
<addr-line><![CDATA[Ciudad Obregón Sonora]]></addr-line>
<country>Mexico</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>09</month>
<year>2016</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>09</month>
<year>2016</year>
</pub-date>
<volume>34</volume>
<numero>3</numero>
<fpage>253</fpage>
<lpage>269</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S0187-57792016000300253&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S0187-57792016000300253&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S0187-57792016000300253&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract: Soil respiration (RS) is a CO2 efflux from the soil to the atmosphere defined as the sum of autotrophic (respiration by roots and mycorrhizae), and heterotrophic (respiration of microorganisms that decompose fractions of organic matter and of soil fauna) respiration. Globally, RS is considered to be the second largest flux of C to the atmosphere. From published literature it is clear that its main controls are soil temperature, soil moisture, photosynthesis, organic matter inputs and soil biota composition. Despite its relevance in C cycle science, there have been only twenty eight studies in Mexico in the last decade where direct measurement of gas exchange was conducted in the field. These studies were held mostly in agricultural and forest ecosystems, in Central and Southern Mexico where mild subtropical conditions prevail. However, arid, semi-arid, tropical and wetland ecosystems may have an important role in Mexico&#8217;s CO2 emissions because of their extent and extensive land use changes. From the twenty eight studies, only two provided continuous measurements of RS with high temporal resolution, highlighting the need for long-term studies to evaluate the complex biophysical controls of this flux and associated processes over different ecological succession stages. We conclude that Mexico represents an important opportunity to understand its complex dynamics, in national and global context, as ecosystems in the country cover a wide range of climatic conditions. This is particularly important because deforestation and degradation of Mexican ecosystems is rapidly increasing along with expected changes in climate.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen: La respiración del suelo (RS) se define como la suma de la respiración autótrofa (raíces y micorrizas) y la respiración heterótrofa (la de los microorganismos del suelo que descomponen materia orgánica y de la fauna del suelo). A nivel global, a RS se le considera el segundo flujo de C más importante hacia la atmósfera. La literatura denota que sus principales controles son la temperatura y humedad del suelo, la fotosíntesis, la disponibilidad de materia orgánica y la composición de la biota del suelo. A pesar de su relevancia en la ciencia del ciclo del C, ha habido solamente 28 estudios publicados en revistas indizadas en México en la última década, en los cuales se llevaron a cabo mediciones directas de intercambio de gases en campo. Estos estudios principalmente representan sistemas agrícolas y bosques en el centro y sur del país. Los ecosistemas áridos y semiáridos, tropicales y los humedales requieren atención debido a su cobertura espacial, su variación de temperatura y humedad, y la amenaza de los cambios de uso de suelo. De los 28 trabajos en la literatura, sólo en dos midieron RS de manera continua, remarcando la necesidad de llevar a cabo estudios a largo plazo para evaluar los complejos controles biofísicos y procesos asociados a este flujo en distintas fases de sucesión ecológica. Concluimos que México representa una oportunidad importante para entender la compleja dinámica de RS, relevante en contextos nacionales e internacionales, debido a la fuerte estacionalidad que gobierna en la mayoría de los ecosistemas mexicanos. Esto es particularmente relevante ya que la deforestación y la degradación en los ecosistemas mexicanos están incrementando rápidamente mientras que se avizoran cambios importantes en la climatología del país.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[biogeosciences]]></kwd>
<kwd lng="en"><![CDATA[carbon cycle]]></kwd>
<kwd lng="en"><![CDATA[soil CO2 efflux]]></kwd>
<kwd lng="en"><![CDATA[soil temperature]]></kwd>
<kwd lng="en"><![CDATA[soil moisture]]></kwd>
<kwd lng="es"><![CDATA[biogeociencias]]></kwd>
<kwd lng="es"><![CDATA[ciclo de carbono]]></kwd>
<kwd lng="es"><![CDATA[flujo de CO2 del suelo]]></kwd>
<kwd lng="es"><![CDATA[temperatura de suelo]]></kwd>
<kwd lng="es"><![CDATA[humedad de suelo]]></kwd>
</kwd-group>
</article-meta>
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