<?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>S1405-33222022000300003</article-id>
<article-id pub-id-type="doi">10.18268/bsgm2022v74n3a080822</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[Micromorphological features of medieval cultural layers formed in different environmental backgrounds]]></article-title>
<article-title xml:lang="es"><![CDATA[Rasgos micromorfológicos de los estratos culturales medievales formadas en diferentes entornos ambientales]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Bronnikova]]></surname>
<given-names><![CDATA[Maria A.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Karpova]]></surname>
<given-names><![CDATA[Julia O.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Murasheva]]></surname>
<given-names><![CDATA[Veronika V.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Kochkina]]></surname>
<given-names><![CDATA[Anna F.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Stashenkov]]></surname>
<given-names><![CDATA[Dmitry A.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Arzhantseva]]></surname>
<given-names><![CDATA[Irina A.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
<xref ref-type="aff" rid="Aaf"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Härke]]></surname>
<given-names><![CDATA[Heinrich]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
<xref ref-type="aff" rid="Aaf"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Russian Academy of Sciences Institute of Geography ]]></institution>
<addr-line><![CDATA[Moscow ]]></addr-line>
<country>Russian Federation</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,State Historical Museum  ]]></institution>
<addr-line><![CDATA[Moscow ]]></addr-line>
<country>Russian Federation</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Samara Regional History and Natural History Museum  ]]></institution>
<addr-line><![CDATA[Samara ]]></addr-line>
<country>Russian Federation</country>
</aff>
<aff id="Af4">
<institution><![CDATA[,Russian Academy of Science Institute of Ethnology and Anthropology ]]></institution>
<addr-line><![CDATA[Moscow ]]></addr-line>
<country>Russian Federation</country>
</aff>
<aff id="Af5">
<institution><![CDATA[,Higher School of Economics University Institute for Oriental and Classical Studies ]]></institution>
<addr-line><![CDATA[Moscow ]]></addr-line>
<country>Russian Federation</country>
</aff>
<aff id="Af6">
<institution><![CDATA[,Tübingen University Department of Medieval Archaeology ]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>00</month>
<year>2022</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>00</month>
<year>2022</year>
</pub-date>
<volume>74</volume>
<numero>3</numero>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1405-33222022000300003&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1405-33222022000300003&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1405-33222022000300003&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT This research compares results of micromorphological case studies conducted on four early medieval archaeological sites with differentiated spatialization of human impacts and a varied craft production located in different background environments: humid climate, subzone of mixed forests, floodplain of the Dnieper River (Gnezdovo site); semi-humid climate, subzone of forest-steppe, Middle Volga region (Muromsky Gorodok and Malaya Ryazan&#8217; sites); arid climate, cold desert of the Aral region, ancient delta-alluvial plain of the Syr-Darya River (Dzhankent site). Micromorphological studies of habitation deposits revealed clear geographical and geochemical regularities in the occurrence of geogenic (soil, sedimentary and post-sedimentary) features. Intrasoil migration and accumulation of clay and coarser silicate material in textural pedofeatures were described in cultural layers of sites located in forest and the forest-steppe zones. An anthropogenic input of phosphates provokes simultaneous migration and illuvial accumulation of phosphates and clay. In the habitation deposits in steppe landscapes with calcareous lithology, the key background soil process is redistribution and intrasoil accumulation of calcium carbonates. In the alluvial desert landscape, major soil processes are accumulation of gypsum and readily soluble salts. All layers are or were affected by at least some seasonal over-moisturizing that resulted in a variety of redoximorphic features depending on their palaeo- and/or contemporary water regime. The high variety of anthropogenic processes and corresponding microfeatures was grouped as follows: (1) input, output, turbation, compaction; (2) neoformation and migration; (3) pyrogenic processes (products); technological processes (products). The set of anthropogenic features records past human impact in the locality. The higher the variety of anthropogenic features and their general abundance is, the more intensive and variable the human impact which had occurred in the past. At the same time, the occurrence of certain anthropogenic features may indicate not only human-related processes of their formation (or input), but also a contemporary soil environment. This environment can be favorable, or, in the opposite, deteriorative for earlier formed anthropogenic features.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN Esta investigación compara los resultados de estudios de casos micromorfológicos, realizados en cuatro sitios arqueológicos del medieval temprano con una diferenciación espacial del impacto humano y de la producción artesanal, localizados en diferentes entornos ambientales: clima húmedo, subzona de bosques mixtos, planicie de inundación del Río Dnieper (sitio Gnezdovo); clima semi-húmedo, subzona de bosque-estepa, región del Volga Central (sitios Muromsky Gorodok y Ryazan); clima árido, desierto frío de la región de Aral, planicie antigua deltáica-aluvial del Río Syr-Darya (sitio Dzhankent). Los estudios micromorfológicos de los depósitos habitacionales revelaron claras regularidades geográficas y geoquímicas en las ocurrencias de las características geogénicas (pedológicas, sedimentarias y post-sedimentarias). La migración de intrasuelo y la acumulación de arcilla y material de silicato más grueso en pedocaracterísticas texturales se encontraron en capas culturales de sitios ubicados en el bosque y las zonas de bosque-estepario. El aporte antropogénico de fosfatos provoca la migración simultánea y la acumulación iluvial de fosfatos y arcilla. En los depósitos habitacionales en paisajes esteparios con litología calcárea, el proceso fundamental del suelo es la redistribución y acumulación intrasuelo de carbonatos de calcio. En el paisaje desértico aluvial, los principales procesos del suelo son la acumulación de yeso y sales fácilmente solubles. Todas las capas están o fueron afectadas por al menos un exceso de humedad estacional que resultó en una variedad de características redoximórficas dependiendo de su régimen hídrico paleo y/o contemporáneo. La gran variedad de procesos antropogénicos y microcaracterísticas correspondientes se agrupó de la siguiente manera: (1) entrada, salida, turbación, compactación; (2) neoformación y migración; (3) procesos pirogénicos (productos); procesos tecnológicos (productos).El conjunto de características antropogénicas registra el pasado del impacto humano en la localidad. Cuanto mayor sea la variedad de características antropogénicas y su abundancia general, más intenso y variable será el impacto humano que ha ocurrido en el pasado. Al mismo tiempo, la aparición de ciertas características antropogénicas puede indicar no solo procesos de formación (o entrada) relacionados con el hombre, sino también un entorno de suelo contemporáneo. Este entorno puede ser favorable o, por el contrario, desfavorable para las características antropogénicas formadas anteriormente.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[cultural layers]]></kwd>
<kwd lng="en"><![CDATA[micromorphology]]></kwd>
<kwd lng="en"><![CDATA[anthropogenic processes]]></kwd>
<kwd lng="en"><![CDATA[geogenic processes]]></kwd>
<kwd lng="en"><![CDATA[environmental conditions]]></kwd>
<kwd lng="es"><![CDATA[estratos culturales]]></kwd>
<kwd lng="es"><![CDATA[micromorfología]]></kwd>
<kwd lng="es"><![CDATA[procesos antropogénicos]]></kwd>
<kwd lng="es"><![CDATA[procesos geogénicos]]></kwd>
<kwd lng="es"><![CDATA[condiciones ambientales]]></kwd>
</kwd-group>
</article-meta>
</front><back>
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