<?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>S0187-57792016000100001</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Almacén y dinámica del carbono orgánico del suelo en bosques templados de México]]></article-title>
<article-title xml:lang="en"><![CDATA[Stocks and dynamics of soil organic carbon in temperate forests of Mexico]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Galicia]]></surname>
<given-names><![CDATA[Leopoldo]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Gamboa Cáceres]]></surname>
<given-names><![CDATA[Ana María]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Cram]]></surname>
<given-names><![CDATA[Silke]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Chávez Vergara]]></surname>
<given-names><![CDATA[Bruno]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Peña Ramírez]]></surname>
<given-names><![CDATA[Víctor]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Saynes]]></surname>
<given-names><![CDATA[Vinisa]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Siebe]]></surname>
<given-names><![CDATA[Christina]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad Nacional Autónoma de México Instituto de Geografía ]]></institution>
<addr-line><![CDATA[ D. F.]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad Nacional Autónoma de México Instituto de Geología ]]></institution>
<addr-line><![CDATA[ D. F.]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Colegio de Postgraduados Campus Montecillo ]]></institution>
<addr-line><![CDATA[ Estado de México]]></addr-line>
<country>Mexico</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>03</month>
<year>2016</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>03</month>
<year>2016</year>
</pub-date>
<volume>34</volume>
<numero>1</numero>
<fpage>1</fpage>
<lpage>29</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S0187-57792016000100001&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S0187-57792016000100001&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S0187-57792016000100001&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen: Los bosques templados se establecen sobre diversos tipos de suelo, sin embargo la información sobre las características físicas, químicas y biológicas de estos suelos y su influencia en el ciclo del carbono es escasa. El objetivo de la presente revisión fue conocer el almacenamiento de carbono en suelos cubiertos por bosques templados. Estos bosques se distribuyen sobre 23 tipos de suelo, principalmente Leptosoles, Regosoles, Luvisoles, Phaeozems, Cambisoles, Umbrisoles y Andosoles formados a partir de materiales volcánicos en el centro del país, sedimentarios en la Sierra Madre Oriental y una variedad amplia de sustratos en la Sierra Madre Occidental. La información sobre el potencial de captura de carbono en los bosques templados está sesgada a la biomasa aérea; y existe menos información sobre los almacenes de carbono edáficos y un escaso entendimiento de los procesos de su estabilización. El almacenamiento de carbono del suelo varió con el tipo de suelo, la composición de especies y el relieve. Los Andosoles, a pesar de su escasa abundancia, son los suelos con la mayor capacidad de almacenar carbono debido a sus características mineralógicas. Los cambios en el carbono orgánico del suelo y los flujos de carbono en los bosques templados en México son el resultado de cambios locales, generados por las actividades humanas como el cambio de uso, el manejo forestal, los incendios, la regeneración y la sustitución de especies. El cambio de uso de suelo es uno de los principales factores que explican los flujos de carbono en estos ecosistemas, sin embargo, aún no existe evidencia clara de que sea en sentido negativo. Esta revisión resume la información existente y propone investigaciones futuras que permitan conocer mejor los procesos de estabilización de la materia orgánica en los suelos de bosques templados.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract: Temperate forests are distributed on several soil types; however information on the physical, chemical and biological properties of these soils and their influence on the carbon cycle are scarce. The objective of this review was to determine the soil carbon stocks in soils covered by temperate forests. These forests are distributed over 23 types of soil, mainly Leptosols, Regosols, Luvisols, Phaeozems, Cambisols, Umbrisols and Andosols formed from volcanic materials in Central Mexico, sedimentary rocks in the Sierra Madre Oriental and a wide variety of substrates in the Sierra Madre Occidental. Information on the potential for soil carbon sequestration in temperate forests is skewed to the aboveground biomass; and there is less information on soil carbon stocks and little understanding of the stabilization processes. The soil carbon storage varied with soil type, species composition and relief. Andosols, despite their low abundance, are the soils with the greatest capacity to store carbon due to their mineralogical characteristics. Soil organic carbon and carbon flux changes in temperate forests in Mexico are a result of human activities such land use change, forest management, fires, regeneration and replacement of species. The land use change is one of the main factors behind the carbon flux in these ecosystems; however, there is still no clear evidence that it is negative. In this review, existing information was synthesized to propose future research to improve our understanding of the stabilization processes of soil organic carbon of temperate forests.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[andosoles]]></kwd>
<kwd lng="es"><![CDATA[encinos]]></kwd>
<kwd lng="es"><![CDATA[materia orgánica del suelo]]></kwd>
<kwd lng="es"><![CDATA[pino]]></kwd>
<kwd lng="es"><![CDATA[relación planta-suelo]]></kwd>
<kwd lng="en"><![CDATA[Andosols]]></kwd>
<kwd lng="en"><![CDATA[oak]]></kwd>
<kwd lng="en"><![CDATA[soil organic matter]]></kwd>
<kwd lng="en"><![CDATA[pine]]></kwd>
<kwd lng="en"><![CDATA[plant-soil relationship]]></kwd>
</kwd-group>
</article-meta>
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