<?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>S1405-33222021000100005</article-id>
<article-id pub-id-type="doi">10.18268/bsgm2021v73n1a171220</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[Environmental variability during the last three millennia in the rain shadows of central Mexico]]></article-title>
<article-title xml:lang="es"><![CDATA[Variabilidad ambiental durante los últimos tres milenios en las sombras de lluvia de México central]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Olivares-Casillas]]></surname>
<given-names><![CDATA[Gustavo]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Correa-Metrio]]></surname>
<given-names><![CDATA[Alex]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Zawisza]]></surname>
<given-names><![CDATA[Edyta]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Wojewódka-Przyby&#322;]]></surname>
<given-names><![CDATA[Marta]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Blaauw]]></surname>
<given-names><![CDATA[Maarten]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Romero]]></surname>
<given-names><![CDATA[Francisco]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad Nacional Autónoma de México Posgrado en Ciencias del Mar y Limnología ]]></institution>
<addr-line><![CDATA[CD-MX ]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad Nacional Autónoma de México Instituto de Geología ]]></institution>
<addr-line><![CDATA[CDMX ]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Research Centre in Warzaw Polish Academy of Sciences Institute of Geological Sciences]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
<country>Poland</country>
</aff>
<aff id="Af4">
<institution><![CDATA[,Queen's University Belfast School of Natural and Built Environment ]]></institution>
<addr-line><![CDATA[Belfast ]]></addr-line>
<country>United Kingdom</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>00</month>
<year>2021</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>00</month>
<year>2021</year>
</pub-date>
<volume>73</volume>
<numero>1</numero>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1405-33222021000100005&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1405-33222021000100005&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1405-33222021000100005&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT The last three millennia have been characterized by global temperature oscillations of around one Celsius degree, and high frequency variability on precipitation. Two main temperature anomalies have been reported worldwide, the Medieval Warm Period (ÏVIWP) and the Little Ice Age (LIA), characterized by higher and lower than average temperatures, respectively. Precipitation variability has been mostly associated with El Niño anomalies in the Equatorial Pacific. These global variability modes have been modulated by regional factors such as sea surface temperatures and their interaction with continental landmasses. Understanding regional responses to these anomalies would shed light on ecosystem response to environmental variability, a paramount tool for conservation purposes on the light of modern climate change. Here we present a 3,000-year sedimentary record from Lake Metztitlán, located in a Biosphere Reserve under the rain shadow of the Sierra Madre Oriental. Cladoceran and geo-chemical analyses were used to reconstruct lacustrine dynamics through the time period encompassed by the record. Our record points to highly dynamic lacustrine systems, coupled with global and regional climatic variability. In Metztitlán, the MWP was associated with low lake levels and a high torrentiality of the precipitation reflected in high-frequency peaks of detrital material. The LIA was associated with an enlarged water body, probably as a result of lower evapotranspiration. Overall, global climatic variability resulted in high variability of regional precipitation and detrital input in the Metztitlán region, in turn associated with changes in lake morphometry and depth. Our record highlights the vulnerability of the area to changes in sea surface temperature of the Gulf of Mexico, and to changes in the frequency of El Niño events. Although the effects of global climate change in the region are inescapable, our results emphasize the importance of controlling anthropogenic activities as an additional source of pressure on the regional ecosystems.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN Los últimos tres milenios se han caracterizado por oscilaciones en la temperatura global alrededor de un grado Celsius, y una variabilidad de alta frecuencia de la precipitación. Dos principales anomalias de temperatura han sido reportadas mundialmente, el Periodo Cálido Medieval (PCM) y la Pequeña Edad de Hielo (PER), caracterizadas por temperaturas más cálidas y más frías que el promedio, respectivamente. La variabilidad de la precipitación ha estado estrechamente relacionada con las anomalías de El Niño en el Pacifico Ecuatorial. A nivel regional, estos modos de variabilidad han sido modulados por factores como la temperatura superficial de los océanos y .su interacción con las masas continentales. El entendimiento de las respuestas regionales a estas anomalias ayuda a comprender la respuesta de los ecosistemas a la variabilidad global, un elemento critico para la conservación en vista del cambio climático moderno. En este trabajo se presenta un registro sedimentario de 3000 años del lago Metztitlán, ubicado en la Reserva de la Biosfera en la Sierra Aladre Oriental. Se empleo un análisis geoquimico y cladócero para reconstruir dinámicas lacustre en el periodo de tiempo que abarca el informe. Nuestro registro apunta a sistemas dinámicos lacustres, asociados con la variabilidad climática global y regional. En Metztitlán, el PCM estuvo asociado con bajos niveles lacustres y una alta torrencialidad de la lluvia, reflejada en picos de alta frecuencia en los indicadores de aporte detritico. La PEH estuvo asociada con un cuerpo lacustre más extenso, probablemente resultado de una menor evapotranspiración. En general, los efectos de la variabilidad climática global se reflejaron en una alta variabilidad de la precipitación y entrada de detriticos (detrital input) en la región de Metztitlán, a su vez asociada con cambios en la morfometria y la profundidad del lago. En nuestro registro resalta la vulnerabilidad del área a cambios en la temperatura superficial de mar en el Golfo de México, y a cambios en la frecuencia de los eventos El Niño. Aunque los efectos del cambio climático en el área son inevitables, nuestros resultados enfatizan la importancia de controlar las actividades antropogénicas como una fuente adicional de presión sobre los ecosistemas regionales.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[Medieval Warm Period]]></kwd>
<kwd lng="en"><![CDATA[Little Ice Age]]></kwd>
<kwd lng="en"><![CDATA[Cladocera]]></kwd>
<kwd lng="en"><![CDATA[late Holocene]]></kwd>
<kwd lng="en"><![CDATA[rain shadow]]></kwd>
<kwd lng="en"><![CDATA[Barranca de Metztitlán Biosphere Reserve]]></kwd>
<kwd lng="es"><![CDATA[Periodo cálido medieval]]></kwd>
<kwd lng="es"><![CDATA[pequeña edad de hielo]]></kwd>
<kwd lng="es"><![CDATA[cladóceros]]></kwd>
<kwd lng="es"><![CDATA[Holoceno tardío]]></kwd>
<kwd lng="es"><![CDATA[sombra de lluvia]]></kwd>
<kwd lng="es"><![CDATA[Reserva de la Biósfera Barranca de Metztitlán]]></kwd>
</kwd-group>
</article-meta>
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