<?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>1405-0471</journal-id>
<journal-title><![CDATA[Madera y bosques]]></journal-title>
<abbrev-journal-title><![CDATA[Madera bosques]]></abbrev-journal-title>
<issn>1405-0471</issn>
<publisher>
<publisher-name><![CDATA[Instituto de Ecología A.C.]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S1405-04712019000200204</article-id>
<article-id pub-id-type="doi">10.21829/myb.2019.2521804</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Distribución actual y futura del bosque subalpino de Pinus hartwegii Lindl en el Eje Neovolcánico Transversal]]></article-title>
<article-title xml:lang="en"><![CDATA[Current and future distribution of the Pinus hartwegii Lindl subalpine forest in the Tranverse Neovolcanic Belt]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Manzanilla-Quiñones]]></surname>
<given-names><![CDATA[Ulises]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Aguirre-Calderón]]></surname>
<given-names><![CDATA[Óscar Alberto]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Jiménez-Pérez]]></surname>
<given-names><![CDATA[Javier]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Treviño-Garza]]></surname>
<given-names><![CDATA[Eduardo Javier]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Yerena-Yamallel]]></surname>
<given-names><![CDATA[José Israel]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad Autónoma de Nuevo León Facultad de Ciencias Forestales ]]></institution>
<addr-line><![CDATA[Linares Nuevo León]]></addr-line>
<country>Mexico</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>00</month>
<year>2019</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>00</month>
<year>2019</year>
</pub-date>
<volume>25</volume>
<numero>2</numero>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1405-04712019000200204&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1405-04712019000200204&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1405-04712019000200204&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen De acuerdo con las proyecciones del clima a futuro, muchas especies verían reducidas sus áreas de distribución, principalmente, aquellas que habitan en zonas templadas y frías. El objetivo principal del presente fue modelar la distribución actual y bajo escenarios de cambio climático del bosque subalpino de Pinus hartwegii Lindl para 2041-2060 en el Eje Neovolcánico Transversal. Se obtuvieron los registros de Pinus hartwegii Lindl de la plataforma GBIF y campo. Se descargaron las 19 variables bioclimáticas WorldClim para el presente y futuro de los modelos de circulación global CRNMCM5 y HADGEM2_ES con dos forzamientos radiactivos de 4.5 (trayectorias de CO2 constantes) y 8.5 (trayectorias de CO2 altas). Se eliminó la autocorrelación espacial de las variables. Se cargaron las variables y los registros de presencia al programa MaxEnt, utilizando 75% de los datos para entrenar los modelos y 25% para validarlos. Se transfirieron los parámetros del mejor modelo para generar los modelos a futuro. Los modelos presentaron un excelente ajuste estadístico (pruebas de entrenamiento y validación &gt; 0.9) para ambos periodos. Las variables determinantes de ambos periodos analizados fueron temperatura promedio anual (BIO1) y altitud (DEM). Los escenarios de cambio climático predicen un aumento en temperatura promedio anual entre 0.7 °C y 2.1 °C y reducciones entre 11.7% y 26.9% en el nicho subalpino de Pinus hartwegii Lindl., siendo el Nevado de Toluca y el Pico de Orizaba los sitios más susceptibles al cambio climático. Por otra parte, el parque Izta-Popo presentaría un aumento de nicho de 37.4%.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract According to future climate projections, many species will see their ranges reduced, mainly those that live in cold forests. The aim of the present study was to model the current distribution and climate change scenarios of the Pinus hartwegii Lindl subalpine forest for 2041-2060 in the Transverse Neovolcanic Belt. Pinus hartwegii Lindl records were obtained from the Global Biodiversity Information Facility (GBIF) and field. The 19 WorldClim bioclimatic variables for the present and future were downloaded from the CRNMCM5 and HADGEM2_ES Global Circulation Models with two radioactive forcings of 4.5 (CO2 constant pathways) and 8.5 (CO2 high pathways). The spatial autocorrelation of the variables was eliminated. The environmental variables and presence records were uploaded to the MaxEnt program, where 75% of the data was used to train the models and 25% to validate them. The parameters of the best model were transferred to generate future models. The models presented an excellent statistical fit (training and validation tests &gt; 0.9) for both periods. The determining variables of both periods analyzed were mean annual temperature (BIO1) and altitude (DEM). Climate change scenarios predict an increase in average annual temperature between 0.7 °C and 2.1 °C and reductions between 11.7% and 26.9% in the subalpine niche of Pinus hartwegii Lindl. Nevado de Toluca and Pico de Orizaba are the most susceptible sites to climate change. On the other hand, Izta-Popo Park would present a 37.4% niche increase.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[áreas de distribución]]></kwd>
<kwd lng="es"><![CDATA[aumento en temperatura promedio anual]]></kwd>
<kwd lng="es"><![CDATA[bosques de alta montaña]]></kwd>
<kwd lng="es"><![CDATA[escenarios de cambio climático]]></kwd>
<kwd lng="es"><![CDATA[nicho ecológico]]></kwd>
<kwd lng="en"><![CDATA[areas of distribution]]></kwd>
<kwd lng="en"><![CDATA[increase in average anual temperature]]></kwd>
<kwd lng="en"><![CDATA[high mountain forests]]></kwd>
<kwd lng="en"><![CDATA[climate change scenarios]]></kwd>
<kwd lng="en"><![CDATA[ecological niche]]></kwd>
</kwd-group>
</article-meta>
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