<?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>S1405-33222022000300009</article-id>
<article-id pub-id-type="doi">10.18268/bsgm2022v74n3a060622</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[Fire microfacies and pyroresidues tracing atmospheric electrification impacts on the Moche Valley and on the Mochica (North Peru)]]></article-title>
<article-title xml:lang="es"><![CDATA[Microfacies de fuego y piroresiduos como traza de impactos por electrificación atmosférica en el valle de Moche y en los Mochicas (norte de Perú)]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Courty]]></surname>
<given-names><![CDATA[Marie-Agnès]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universitat de Perpinyà Via Domícia  ]]></institution>
<addr-line><![CDATA[Perpinyà ]]></addr-line>
<country>France</country>
</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=S1405-33222022000300009&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1405-33222022000300009&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1405-33222022000300009&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT The effects of environmental events on living conditions during occupation periods are studied by comparing alluvial soils and occupation floors that formed during the late Holocene in the Moche valley (North Peruvian coast). The microcontextual study comprises (1) microsurface identification in the field; (2) micromorphological analysis of thin sections; (3) multi-scale characterization of soil components based on digital stereo microscope and scanning electron microscope analysis. The alluvial sequence consists of a 6 m thick alternation of organic silty-clay, fine sandy strata with well-preserved ashy charcoal strata and massive grey sandy beds. This cyclical pattern reflects alternation of stable episodes with a dense reed-bed vegetation, regularly affected by wildfires and drought marked by sand invasions from coastal dunes during El Niño events. The 14C dates show that these contrasting conditions lasted for one millennium up to establishment of the Mochica empire at the Huaca at 300 years cal. BC. Vesicular slags produced by flash-melting of the soil components, biosourced quartz and nanostructured polymers formed from flash-ionization of the reed vegetation, all with FeCrNi metals coatings, were retrieved in the fired surfaces. They trace impact at the soil surface of electrically charged particles, lightning-flashes, nanoaerosol production by enhanced atmospheric electrification, i.e., flash-heating, shock vaporization, plasma-polymerization of the vegetation and the host matrix. The study shows the occurrence in the basal Uhle platform occupation deposits at the foot of the Huaca de la Luna of similar cemented ashy microfacies associated with a funerary deposit with food offerings in ritual vessels and an intriguing scoriaceous slag. The evidence for ritual disposal of imperishable offerings to deaths is interpreted as the memorial record of the Mochica knowledge of long-lived materials produced by lightning-triggered plasma processes. This integrated study of the environmental and cultural contexts refutes previous assumptions of long-term engineering of the arable alluvial plain to counteract sand invasion and torrential floods. In contrast, the establishment of the Moche pyramids is shown to have occurred during a period of floodplain stability marked by high-energy natural events and lightning processes that offered access to durable soil resources of important social values.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN Se estudia los efectos de los eventos ambientales para las condiciones de vida durante los periodos de ocupación, comparando los suelos aluviales y los pisos de ocupación que se formaron durante el Holoceno tardío en el valle de Moche (costa norperuana). El estudio microcontextual comprende (1) la identificación de la microsuperficie en el campo; (2) el análisis micromorfológico de secciones delgadas; (3) la caracterización multiescalar de los componentes del suelo a partir del análisis con estereomicroscopio digital y microscopio electrónico de barrido. La secuencia aluvial consiste en una alternancia de 6 m de espesor de arcilla limosa orgánica, estratos arenosos finos con estratos de carbón vegetal ceniciento bien conservados y lechos arenosos grises masivos. Esta alternancia refleja episodios estables con una densa vegetación de cañaveral, afectada regularmente por incendios forestales que se alternan con sequías e invasiones de arena de las dunas costeras durante los eventos de El Niño. Las fechas de 14C muestran que estas condiciones contrastantes duraron un milenio hasta el establecimiento del imperio Mochica en la Huaca en 300 años cal. AC. En las superficies impactadas se recuperaron vesicular-escoriáceos producidas por la fusión instantánea de los componentes del suelo, cuarzo de origen biológico y polímeros nanoestructurados formados a partir de la ionización instantánea de la vegetación de caña, todos ellos con recubrimientos de metales FeCrNi. Se rastrea el impacto en la superficie del suelo de la carga de partículas, los relámpagos, la producción de nanoaerosoles por electrificación atmosférica mejorada, es decir, el calentamiento por destellos, la vaporización por choque, la polimerización por plasma de la vegetación y de la matriz anfitriona. El estudio muestra la ocurrencia en los depósitos de ocupación de la plataforma basal Uhle al pie de la Huaca de la Luna de una microfacies cenicienta cementada similar asociada a un depósito funerario con ofrendas de alimentos en vasijas rituales y a una intrigante escoria vesicular. Este depósito ritual de ofrendas de larga duración a los muertos se interpreta como el registro conmemorativo del conocimiento Mochica de los materiales de larga duración producidos por procesos plasmáticos desencadenados por el rayo. Este estudio integrado de los contextos ambiental y cultural refuta las suposiciones anteriores sobre la ingeniería a largo plazo de la llanura aluvial cultivable para contrarrestar la invasión de arena y las inundaciones torrenciales. Por el contrario, se demuestra que el establecimiento de las pirámides Moche se produjo durante un período de estabilidad de la llanura aluvial marcado por eventos naturales de alta energía y procesos de iluminación que ofrecían acceso a recursos de suelo duraderos de importantes valores sociales.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[microcontextual]]></kwd>
<kwd lng="en"><![CDATA[aerosol]]></kwd>
<kwd lng="en"><![CDATA[lightning]]></kwd>
<kwd lng="en"><![CDATA[plasma]]></kwd>
<kwd lng="en"><![CDATA[flash]]></kwd>
<kwd lng="en"><![CDATA[heating]]></kwd>
<kwd lng="en"><![CDATA[polymerization]]></kwd>
<kwd lng="en"><![CDATA[preservation]]></kwd>
<kwd lng="es"><![CDATA[microcontexto]]></kwd>
<kwd lng="es"><![CDATA[aerosol]]></kwd>
<kwd lng="es"><![CDATA[rayo]]></kwd>
<kwd lng="es"><![CDATA[plasma]]></kwd>
<kwd lng="es"><![CDATA[destello]]></kwd>
<kwd lng="es"><![CDATA[calentamiento]]></kwd>
<kwd lng="es"><![CDATA[polimerización]]></kwd>
<kwd lng="es"><![CDATA[preservación]]></kwd>
</kwd-group>
</article-meta>
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