<?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>1405-3322</journal-id>
<journal-title><![CDATA[Boletín de la Sociedad Geológica Mexicana]]></journal-title>
<abbrev-journal-title><![CDATA[Bol. Soc. Geol. Mex]]></abbrev-journal-title>
<issn>1405-3322</issn>
<publisher>
<publisher-name><![CDATA[Sociedad Geológica Mexicana A.C.]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S1405-33222024000200108</article-id>
<article-id pub-id-type="doi">10.18268/bsgm2024v76n2a250224</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[Burning effects on the soils of the Mexican Maya Lowlands: Current evidence for understanding past events]]></article-title>
<article-title xml:lang="es"><![CDATA[Efectos de quemas en los suelos de las Tierras Bajas Mayas en México: Evidencias actuales para entender eventos del pasado]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Moreno-Roso]]></surname>
<given-names><![CDATA[Sol]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
<xref ref-type="aff" rid="Aaf"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Solleiro-Rebolledo]]></surname>
<given-names><![CDATA[Elizabeth]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Sedov]]></surname>
<given-names><![CDATA[Sergey]]></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"/>
<xref ref-type="aff" rid="Aaf"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Merino]]></surname>
<given-names><![CDATA[Agustín]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad Nacional Auto&#769;noma de Me&#769;xico Posgrado en Ciencias de la Tierra ]]></institution>
<addr-line><![CDATA[ CDMX]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad Nacional Auto&#769;noma de Me&#769;xico Instituto de Geologi&#769;a Departamento de Ciencias Ambientales y del Suelo]]></institution>
<addr-line><![CDATA[ CDMX]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Laboratorio Nacional de Geoqui&#769;mica y Mineralogi&#769;a  ]]></institution>
<addr-line><![CDATA[ CDMX]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af4">
<institution><![CDATA[,Universidad de Santiago de Compostela Escuela Polite&#769;cnica Superior de Ingenieri&#769;a Departamento de Edafologi&#769;a y Qui&#769;mica Agri&#769;cola]]></institution>
<addr-line><![CDATA[ Lugo]]></addr-line>
<country>Spain</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>00</month>
<year>2024</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>00</month>
<year>2024</year>
</pub-date>
<volume>76</volume>
<numero>2</numero>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1405-33222024000200108&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1405-33222024000200108&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1405-33222024000200108&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT The slash-and-burn cultivation system is a millenarian practice still used in many countries today, with significant environmental impacts. However, identifying evidence of this agricultural method in soil records is challenging due to natural and human factors that can obscure or alter fire signals. This challenge is particularly evident in the Yucatán Peninsula, where the ancient Maya practiced slash-and-burn agriculture in a dynamic tropical karst environment, making it difficult to pinpoint the origins and consequences of this practice. In this study, we use a recent agricultural burning in a karstic landscape in Chiapas as a model to understand alterations in soil properties. We then apply these insights to identify similar features at a Maya site on the Yucatán Peninsula, specifically at Coyote Quarry. For both cases, we conducted micromorphological analysis, soil physical-chemical characterization, thermogravimetry and differential scanning calorimetry analysis, and radiocarbon dating of mollusk shells, soil organic carbon, and charcoal fragments (the latter exclusively at Coyote Quarry). Our findings reveal significant effects on the soils from the Chiapas site post-burning, including changes in grain size distribution, pH, and total organic and inorganic carbon. These results were compared to those obtained from the Coyote Quarry soils and pedosediments. Key findings include micromorphological features, the presence of charcoal and other burned materials, and pyrogenic carbon identified through thermal analyses. The preservation of these burned features was facilitated by the typical karstic vertical soil erosion and redeposition as pedosediments in karstic depressions. The intrinsic association of the fire signals found in these karstic sinkholes and their radiocarbon dates enables us to link this evidence to the initiation of slash-and-burn agriculture by the Maya in the Yucatán Peninsula during the transition between the Archaic and Early Pre-Classic periods.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN La roza-tumba y quema es una práctica agrícola milenaria que tiene un fuerte efecto sobre el medio ambiente. Sin embargo, no es fácil identificar las señales de esta práctica en los registros edáficos debido a factores naturales y antrópicos. Particularmente en la Península de Yucatán, los antiguos mayas utilizaron la roza-tumba y quema en un ambiente kárstico tropical muy dinámico, en donde, reconocer el inicio y las consecuencias de esta práctica, es aún controversial. En esta investigación, utilizamos una quema agrícola reciente en el paisaje kárstico de Chiapas, como modelo para entender las alteraciones de las propiedades del suelo e identificar qué rasgos permanecen en un sitio Maya antiguo de la Península de Yucatán. Para ambos casos, realizamos análisis micromorfológicos, caracterización fisicoquímica de los suelos y pedosedimentos, análisis térmicos de la materia orgánica y dataciones de radiocarbono (exclusivamente en Yucatán). Encontramos efectos intensos en los suelos del sitio de Chiapas después de la quema, con cambios en la distribución granulométrica, en el pH y en el carbono orgánico e inorgánico. Estos resultados se compararon con los obtenidos en los suelos y pedosedimentos de la Cantera Coyote. Los principales hallazgos están relacionados con las características micromorfológicas: presencia de carbón vegetal y otros materiales quemados, así como la identificación de carbono pirogénico en los análisis térmicos. La preservación de estos rasgos de quema se ve favorecida por la erosión vertical del suelo en el karst y la redeposición de estos pedosedimentos en depresiones kársticas. La asociación intrínseca de la señal del uso del fuego encontrada en estas depresiones y sus dataciones nos permiten relacionar esta evidencia con el inicio de la práctica de la roza-tumba y quema por los Mayas en la Península de Yucatán en la transición entre el Arcaico y el Preclásico Temprano.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[Maya]]></kwd>
<kwd lng="en"><![CDATA[slash-and-burn agriculture]]></kwd>
<kwd lng="en"><![CDATA[pyrogenic carbon]]></kwd>
<kwd lng="en"><![CDATA[soil erosion]]></kwd>
<kwd lng="en"><![CDATA[pedosediments]]></kwd>
<kwd lng="en"><![CDATA[karstic pockets]]></kwd>
<kwd lng="es"><![CDATA[Maya]]></kwd>
<kwd lng="es"><![CDATA[agricultura de roza-tumba y quema]]></kwd>
<kwd lng="es"><![CDATA[carbono pirogénico]]></kwd>
<kwd lng="es"><![CDATA[erosión de suelos]]></kwd>
<kwd lng="es"><![CDATA[pedosedimentos]]></kwd>
<kwd lng="es"><![CDATA[bolsas kársticas]]></kwd>
</kwd-group>
</article-meta>
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