<?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>1870-3453</journal-id>
<journal-title><![CDATA[Revista mexicana de biodiversidad]]></journal-title>
<abbrev-journal-title><![CDATA[Rev. Mex. Biodiv.]]></abbrev-journal-title>
<issn>1870-3453</issn>
<publisher>
<publisher-name><![CDATA[Instituto de Biología]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S1870-34532020000100306</article-id>
<article-id pub-id-type="doi">10.22201/ib.20078706e.2020.91.3117</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Sensibilidad climática en anchuras de anillos de crecimiento de Pinus hartwegii: una especie alpina mexicana con potencial dendroclimático]]></article-title>
<article-title xml:lang="en"><![CDATA[Climate sensitivity in tree-ring widths of Pinus hartwegii: a Mexican alpine species with dendroclimatic potential]]></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[Villanueva-Díaz]]></surname>
<given-names><![CDATA[José]]></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>
<aff id="Af2">
<institution><![CDATA[,Instituto Nacional de Investigaciones Forestales, Agrícolas y Pecuarias  ]]></institution>
<addr-line><![CDATA[Gómez Palacio Durango]]></addr-line>
<country>Mexico</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>00</month>
<year>2020</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>00</month>
<year>2020</year>
</pub-date>
<volume>91</volume>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1870-34532020000100306&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1870-34532020000100306&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1870-34532020000100306&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen Este estudio analizó la respuesta climática, potencial dendrocronológico e influencia de fenómenos océano-atmosféricos en anillos de crecimiento de Pinus hartwegii Lindl. en 3 sitios de la Faja Volcánica Transmexicana. Se recolectaron de 36 a 40 núcleos de crecimiento por sitio. Las muestras se analizaron y fecharon mediante técnicas dendrocronológicas. La anchura de anillo total se midió en un micrómetro. La verificación del fechado se efectuó mediante análisis de correlación. Se descargaron los registros de estaciones meteorológicas cercanas a los sitios de estudio de la base de datos CLICOM, se identificaron periodos de respuesta clima-crecimiento radial y se realizaron correlaciones entre las cronologías de arstan y los índices de ENOS, ODP y OMA, con el fin evaluar la influencia de dichos fenómenos en el crecimiento radial. El análisis de los parámetros dendrocronológicos indicó un potencial dendrocronológico de P. hartwegii de intermedio a alto. La sensibilidad climática mayor de la especie se registró en el Nevado de Colima. La precipitación invierno-primavera fue la variable que influyó más sobre el crecimiento, mientras que la temperatura máxima promedio afectó negativamente el crecimiento. ENOS y OMA no influyeron el crecimiento. Sin embargo, en el Nevado de Colima, ODP influyó positiva y significativamente en el crecimiento.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract This study analyzed the climatic response, dendrochronological potential, and influence of oceanic-atmospheric phenomena in tree-rings of Pinus hartwegii Lindl. in 3 sites in the Trans-Mexican Volcanic Belt. From 36 to 40 growth nuclei per site were sampled. The samples were analyzed and dated using dendrochronological techniques. The total ring width was measured with a micrometer. Verification of the dating was carried out by correlation analysis. The records of weather stations near the study sites were downloaded from the CLICOM database, radial weather-growth response periods were identified, and correlations among ARSTAN chronologies and ENOS, ODP and OMA indices were developed to evaluate the influence of these phenomena on radial-growth. The analysis of dendrochronological parameters showed that the dendrochronological potential for P. hartwegii was from intermediate to high. The highest climatic sensitivity for the species was recorded in Nevado de Colima. The winter-spring precipitation was the variable that influenced more the growth, while the average maximum temperature negatively affected the growth of the trees. ENOS and OMA did not influence the radial growth. However, in Nevado de Colima ODP had a positive and significant influence on growth.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[Bosque de alta montaña]]></kwd>
<kwd lng="es"><![CDATA[Clima-crecimiento]]></kwd>
<kwd lng="es"><![CDATA[Dendrocronología]]></kwd>
<kwd lng="es"><![CDATA[Fenómenos océano-atmosféricos]]></kwd>
<kwd lng="es"><![CDATA[Precipitación invierno-primavera]]></kwd>
<kwd lng="en"><![CDATA[High mountain forest]]></kwd>
<kwd lng="en"><![CDATA[Climate-growth]]></kwd>
<kwd lng="en"><![CDATA[Dendrochronology]]></kwd>
<kwd lng="en"><![CDATA[Ocean-atmospheric phenomena]]></kwd>
<kwd lng="en"><![CDATA[Winter-spring precipitation]]></kwd>
</kwd-group>
</article-meta>
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