<?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>0258-5936</journal-id>
<journal-title><![CDATA[Cultivos Tropicales]]></journal-title>
<abbrev-journal-title><![CDATA[cultrop]]></abbrev-journal-title>
<issn>0258-5936</issn>
<publisher>
<publisher-name><![CDATA[Ediciones INCA]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S0258-59362024000200009</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Influencia compleja del relieve en la erosión de los suelos Ferralíticos Rojos a escala local]]></article-title>
<article-title xml:lang="en"><![CDATA[Complex influence of relief on the erosion of Red Ferrallitic soils at a local scale]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Febles González]]></surname>
<given-names><![CDATA[José Manuel]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Febles Díaz]]></surname>
<given-names><![CDATA[José Miguel]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Maura Santiago]]></surname>
<given-names><![CDATA[Ana Victoria]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Tolón Becerra]]></surname>
<given-names><![CDATA[Alfredo]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Brasil do Amaral Sobrinho]]></surname>
<given-names><![CDATA[Nelson Moura]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Zonta]]></surname>
<given-names><![CDATA[Everaldo]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad de La Habana Centro de Investigaciones Marinas ]]></institution>
<addr-line><![CDATA[Miramar La Habana]]></addr-line>
<country>Cuba</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad de La Habana Facultad de Contabilidad y Finanzas ]]></institution>
<addr-line><![CDATA[Municipio Plaza de la Revolución La Habana]]></addr-line>
<country>Cuba</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Universidad de Almería  ]]></institution>
<addr-line><![CDATA[ Almería]]></addr-line>
<country>España</country>
</aff>
<aff id="Af4">
<institution><![CDATA[,Universidad Federal Rural de Rio de Janeiro  ]]></institution>
<addr-line><![CDATA[ Rio de Janeiro]]></addr-line>
<country>Brazil</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>06</month>
<year>2024</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>06</month>
<year>2024</year>
</pub-date>
<volume>45</volume>
<numero>2</numero>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://scielo.sld.cu/scielo.php?script=sci_arttext&amp;pid=S0258-59362024000200009&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://scielo.sld.cu/scielo.php?script=sci_abstract&amp;pid=S0258-59362024000200009&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://scielo.sld.cu/scielo.php?script=sci_pdf&amp;pid=S0258-59362024000200009&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN Estudiar el relieve a través del análisis morfológico permite tipificar formas, elementos y estructuras del relieve kárstico que auxilian en el entendimiento de la génesis, evolución y dinámica que asume la erosión de los suelos Ferralíticos Rojos, circunstancia particularmente importante en la Llanura Kárstica Meridional Habana - Matanzas, para comprender cómo y porqué cierta información es preservada y otra se pierde conforme la investigación se ejecuta de una escala a otra, lo que ha propiciado ciertos mitos e incertidumbres sobre los procesos de degradación de estos suelos. El presente trabajo tiene como objetivo analizar la influencia compleja del relieve y la escala geográfica en la comprensión de los procesos kárstico - erosivos en las áreas de influencia de las depresiones kársticas, a partir de una línea base de más de tres décadas, que demuestra el avance unidireccional de la dinámica kárstico - erosiva, en conformidad con las condiciones de uso y manejo a que han estado sometidos. Se concluye que el reconocimiento y evolución espacio - temporal de las formas de erosión solo es posible realizarla a escala local y no a partir de un re-escalamiento simple de las variables a grandes áreas, para así evitar diferentes interpretaciones en los mapas de erosión de los suelos Ferralíticos Rojos en Cuba.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT Studying the relief through morphological analysis allows typifying forms, elements and structures of the karst relief that help in the understanding of the genesis, evolution and dynamics assumed by the erosion of the Red Ferrallitic soils. It is a particularly important circumstance in the Southern karst Plain Havana-Matanzas, to understand how and why certain information is preserved and others are lost as the research is carried out from one scale to another, which has led to certain myths and uncertainties about the degradation processes of these soils. The present work aims to analyze the complex influence of relief and geographic scale on the understanding of karst-erosive processes in the areas of influence of karst depressions from a baseline of more than three decades, which demonstrates the unidirectional advance of karst-erosive dynamics in accordance with the conditions of use and management to which they have been subjected. It is concluded that the recognition and spatio-temporal evolution of erosion forms is only possible at a local scale and not from a simple rescaling of the variables to large areas, in order to avoid different interpretations in the erosion maps of the Red Ferralitic soils in Cuba.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[degradación]]></kwd>
<kwd lng="es"><![CDATA[karst]]></kwd>
<kwd lng="es"><![CDATA[relieve]]></kwd>
<kwd lng="en"><![CDATA[degradation]]></kwd>
<kwd lng="en"><![CDATA[karst]]></kwd>
<kwd lng="en"><![CDATA[relief]]></kwd>
</kwd-group>
</article-meta>
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