<?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>S1405-33222019000200519</article-id>
<article-id pub-id-type="doi">10.18268/bsgm2019v71n2a17</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[Late Holocene human activities and their impacts on the soils and sediments at La Playa, Sonora, Mexico]]></article-title>
<article-title xml:lang="es"><![CDATA[Actividades humanas durante el Holoceno tardío y su impacto en los suelos y sedimentos en La Playa, Sonora]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Cruz-y-Cruz]]></surname>
<given-names><![CDATA[Tamara]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Sánchez]]></surname>
<given-names><![CDATA[Guadalupe]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Carpenter]]></surname>
<given-names><![CDATA[John]]></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[Solleiro-Rebolledo]]></surname>
<given-names><![CDATA[Elizabeth]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Barceinas-Cruz]]></surname>
<given-names><![CDATA[Hermenegildo]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad Nacional Autónoma de México  ]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Instituto Nacional de Antropología e Historia  ]]></institution>
<addr-line><![CDATA[Hermosillo Sonora]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Universidad Nacional Autónoma de México Instituto de Geología ]]></institution>
<addr-line><![CDATA[CDMX ]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af4">
<institution><![CDATA[,Universidad Nacional Autónoma de México  ]]></institution>
<addr-line><![CDATA[CDMX ]]></addr-line>
<country>Mexico</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>00</month>
<year>2019</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>00</month>
<year>2019</year>
</pub-date>
<volume>71</volume>
<numero>2</numero>
<fpage>519</fpage>
<lpage>541</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1405-33222019000200519&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1405-33222019000200519&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1405-33222019000200519&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract The activities carried out by preindustrial agricultural societies are not usually considered as important factors of soil degradation. Nonetheless, repetitive human daily activities for hundreds of years can substantially transform the natural properties of the soils. At the site of La Playa, Mexico, the activities of early farmers modified the landscape and had an important role in the physical transformations of the natural soil features. This paper depicts the characteristics of La Playa paleosols, which were the living surface of the Early Agriculture Period community (4000 - 1800 cal BP) and we discuss the influence of daily subsistence activities on the soil. The soil features (structuring, differentiation of horizons, texture-in field and laboratory, color, porosity, stoniness, magnetic properties, organic carbon content, carbonation, presence of cutans, nodules and/or concretions, among other pedological features) of three profiles with pedosediments (paleosols interbedded with sediments) formed during late Holocene are discussed. Our study suggests that La Playa Fluvisols are poorly developed and were formed with alluvial deposits (largely composed of reworked soils). The pedogenic properties indicate that overlapping developed during short time periods of stability, under arid conditions of the last 4000 years. The uniformity of the features in all the studied profiles indicate similar pedogenetic conditions across the site. The micromorphological and magnetic properties clearly show that the soil was deeply disturbed by human activities, mainly by roasting features to process food, crematories and grave digging to bury the dead, and removing soil for several agricultural activities.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen Las actividades realizadas por las sociedades agrícolas prehispánicas poco complejas, no son usualmente consideradas como factores importantes de degradación del suelo. Sin embargo, la repetición de actividades cotidianas durante cientos de años puede afectar sustancialmente sus características. En el sitio de La Playa, las modificaciones del paisaje producidas por las actividades cotidianas, tales como la construcción de hornos de tierra para cocer alimentos, campos de maíz con un complejo sistema de canales de riego, y la práctica de rituales mortuorios (crematorios, cremaciones e inhumaciones), juegan un papel importante en las transformaciones de los rasgos naturales del suelo. En este artículo se muestran las características de los paleosuelos de La Playa, que constituyeron la superficie de ocupación durante el Periodo de Agricultura Temprana (4500-1800 cal AP), y la influencia que las actividades de subsistencia diaria tuvieron en su configuración. Para ello, se muestran los resultados obtenidos en campo y en laboratorio de tres perfiles de secuencias pedosedimentarias formadas durante el Holoceno tardío en La Playa, Sonora (NW de México). Las características evaluadas son: estructuración, diferenciación de horizontes, textura (a tacto y por separación de fracciones), color, porosidad, pedregosidad, propiedades magnéticas, contenido de carbono orgánico, carbonatación, presencia de cutanes, nódulos y/o concreciones, entre otros rasgos pedológicos. Estudios previos muestran que los Fluvisoles de La Playa están pobremente desarrollados y se formaron a partir de depósitos aluviales (compuestos en gran medida por suelos redepositados). Las propiedades físicas y químicas indican periodos cortos de pedogénesis superpuestos, desarrollados bajo un clima árido durante los últimos 4000 años. Las características de todos los perfiles son muy similares, indicando las mismas condiciones pedogenéticas; mientras que las propiedades micromorfológicas y magnéticas muestran claramente que el suelo está profundamente perturbado por las actividades humanas, principalmente quema en los hornos y cremaciones.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[Soil degradation]]></kwd>
<kwd lng="en"><![CDATA[human activities]]></kwd>
<kwd lng="en"><![CDATA[magnetic properties]]></kwd>
<kwd lng="en"><![CDATA[paleosols]]></kwd>
<kwd lng="en"><![CDATA[Sonora]]></kwd>
<kwd lng="es"><![CDATA[Degradación de suelo]]></kwd>
<kwd lng="es"><![CDATA[impacto antrópico]]></kwd>
<kwd lng="es"><![CDATA[propiedades magnéticas]]></kwd>
<kwd lng="es"><![CDATA[paleosuelos]]></kwd>
<kwd lng="es"><![CDATA[Sonora]]></kwd>
</kwd-group>
</article-meta>
</front><back>
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