<?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>1026-8774</journal-id>
<journal-title><![CDATA[Revista mexicana de ciencias geológicas]]></journal-title>
<abbrev-journal-title><![CDATA[Rev. mex. cienc. geol]]></abbrev-journal-title>
<issn>1026-8774</issn>
<publisher>
<publisher-name><![CDATA[Universidad Nacional Autónoma de México, Instituto de Geología]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S1026-87742025000100031</article-id>
<article-id pub-id-type="doi">10.22201/igc.20072902e.2025.1.1854</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Historia de la vegetación y el clima durante los últimos 3200 años, en la costa sur de Quintana Roo, México]]></article-title>
<article-title xml:lang="en"><![CDATA[Vegetation and climate history over the past 3200 years on the southern coast of Quintana Roo, Mexico]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Rosas]]></surname>
<given-names><![CDATA[Chloe]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Carrillo-Bastos]]></surname>
<given-names><![CDATA[Alicia]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[González-Salvatierra]]></surname>
<given-names><![CDATA[Claudia]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Aragón-Moreno]]></surname>
<given-names><![CDATA[Alejandro Antonio]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Islebe]]></surname>
<given-names><![CDATA[Gerald]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Tecnológico Nacional de México IT de Chetumal ]]></institution>
<addr-line><![CDATA[Chetumal Quintana Roo]]></addr-line>
<country>México</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Tecnológico Nacional de México  IT de Chetumal]]></institution>
<addr-line><![CDATA[Chetumal Quintana Roo]]></addr-line>
<country>México</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,El Colegio de la Frontera Sur  ]]></institution>
<addr-line><![CDATA[Chetumal Quintana Roo]]></addr-line>
<country>Mexico</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>00</month>
<year>2025</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>00</month>
<year>2025</year>
</pub-date>
<volume>42</volume>
<numero>1</numero>
<fpage>31</fpage>
<lpage>43</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1026-87742025000100031&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1026-87742025000100031&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1026-87742025000100031&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen Por medio de análisis de polen y elementos geoquímicos, de un núcleo de sedimento de 1.5 m de profundidad, se identificaron cambios en la historia vegetal y ambiental de los últimos 3200 años de la Laguna Cementerio ubicada en el poblado de Xcalak, Quintana Roo. Los cambios en la composición y abundancia de Rhizophora mangle, Conocarpus erectus, Avicennia germinans y Laguncularia racemosa permitieron inferir cambios en la variabilidad hidrológica. Al inicio de los 3200 años cal AP se presentaron condiciones húmedas, la vegetación dominante era la selva, compuesta principalmente por elementos de Moraceae, Fabaceae, Euphorbiaceae, Rubiaceae y Bursera simaruba. Durante este periodo, los elementos de manglar estaban dominados por Avicennia germinans junto con la presencia de foraminíferos. El primer registro de Zea mays alrededor de 850 a.C (2800 cal AP) permitió identificar la presencia de actividades agrícolas cerca de la zona desde el Preclásico temprano hasta el Clásico tardío. La especie de manglar dominante era C. erectus, lo que sugiere fuertes cambios en la variabilidad hidrológica. Se lograron identificar, por medio de la curva de Ca/&#931; (Ti, Fe, Al), dos periodos de sequía alrededor de 1700 y 850 cal AP, respectivamente. La sequía alrededor de 1700 cal AP podría estar asociada a una intensificación de ENSO y a un cambio en el gradiente de la temperatura superficial del mar y la salinidad que afectan la fuerza de la corriente de chorro del Caribe, provocando una disminución en la cantidad de precipitación para Mesoamérica. Durante ese mismo periodo se registró la mayor reducción de la selva y expansión de la sabana, lo cual permitió el depósito de Pinus sp. La sequía registrada alrededor de 850 cal AP es contemporánea con el periodo Clásico terminal. La comparación con otros registros climáticos de la región y del Circum-Caribe sugieren que las sequías del Clásico terminal estaban alternadas con periodos húmedos. El regreso de las condiciones húmedas alrededor de 700 cal AP permitió la recuperación de la cobertura vegetal. El presente estudio es un registro que aporta nuevas evidencias sobre los cambios en la Laguna Cementerio durante los últimos 3200 años, zona que ha sido poco estudiada desde el punto de vista paleoambiental.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract Changes in vegetation and environmental history for the last 3200 years at Laguna Cementerio, Xcalak, Quintana Roo were identified using fossil pollen and geochemical analyses of a 1.5 m depth sediment core. Changes in abundance and composition of Rhizophora mangle, Conocarpus erectus, Avicennia germinans, and Laguncularia racemosa allowed to infer changes in hydrological variability. At the beginning of the 3200 cal yr BP moist conditions were exhibited. Dominant vegetation was tropical forest, mainly composed of Moraceae, Fabaceae, Euphorbiaceae, Rubiaceae, and Bursera simaruba. During this period, mangroves were dominated by Avicennia germinans along with the presence of foraminifera. The first record of Z. mays around 850 B.C. (2800 cal yr BP) allowed the identification of agricultural activities close to the study area from the Middle Preclassic to the Late Classic. The dominant mangrove species was C. erectus, suggesting strong changes in the hydrological variability. Two drought periods were identified around 1700 and 850 cal yr BP, respectively, with the Ca/&#931; (Ti, Fe, Al) curve. The drought at 1700 cal BP may be associated with changes in sea surface temperatures (SST) and sea surface salinity (SSS) that affect the strength of the Caribbean Low-Level Jet causing a decrease in the amount of rainfall for Mesoamerica. During this same period, the highest reduction of tropical forest was observed, changing the landscape to a more open vegetation that allowed the deposit of Pinus sp. The drought that occurred around 850 cal yr BP corresponds to the Terminal Classic Period. Further comparison with other climate proxy records from the region and Circum-Caribbean area suggests that the Terminal Classic Droughts were alternated with wet periods. Around 700 cal yr BP, moist conditions returned and allowed the recovery of the tropical forest. This study contributes to new evidence of changes experienced in Laguna Cementerio during the last 3200 cal yr BP, an area that has been poorly studied from a paleoenvironmental point of view.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[vegetación]]></kwd>
<kwd lng="es"><![CDATA[manglar]]></kwd>
<kwd lng="es"><![CDATA[paleoambientes]]></kwd>
<kwd lng="es"><![CDATA[polen fósil]]></kwd>
<kwd lng="es"><![CDATA[geoquímica]]></kwd>
<kwd lng="es"><![CDATA[sequía]]></kwd>
<kwd lng="es"><![CDATA[Quintana Roo]]></kwd>
<kwd lng="es"><![CDATA[México]]></kwd>
<kwd lng="en"><![CDATA[vegetation]]></kwd>
<kwd lng="en"><![CDATA[mangrove]]></kwd>
<kwd lng="en"><![CDATA[paleoenvironment]]></kwd>
<kwd lng="en"><![CDATA[fossil pollen]]></kwd>
<kwd lng="en"><![CDATA[geochemistry]]></kwd>
<kwd lng="en"><![CDATA[drought]]></kwd>
<kwd lng="en"><![CDATA[Quintana Roo]]></kwd>
<kwd lng="en"><![CDATA[Mexico]]></kwd>
</kwd-group>
</article-meta>
</front><back>
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