<?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>0871-018X</journal-id>
<journal-title><![CDATA[Revista de Ciências Agrárias]]></journal-title>
<abbrev-journal-title><![CDATA[Rev. de Ciências Agrárias]]></abbrev-journal-title>
<issn>0871-018X</issn>
<publisher>
<publisher-name><![CDATA[Sociedade de Ciências Agrárias de Portugal]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S0871-018X2022000301251</article-id>
<article-id pub-id-type="doi">10.19084/rca.28411</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Comparación del microbioma de suelos calcáreos y yesosos en parcelas de secano bajo clima Mediterráneo]]></article-title>
<article-title xml:lang="en"><![CDATA[Comparison of the microbiome of calcareous and gypseous soils in rainfed field plots under Mediterranean climate]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Sierra]]></surname>
<given-names><![CDATA[María-José]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[García-Montero]]></surname>
<given-names><![CDATA[Rocío]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Rodríguez-Rastrero]]></surname>
<given-names><![CDATA[Manuel]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Millá]]></surname>
<given-names><![CDATA[Rocio]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,CIEMAT Departamento de Medio Ambiente ]]></institution>
<addr-line><![CDATA[Madrid ]]></addr-line>
<country>Spain</country>
</aff>
<pub-date pub-type="pub">
<day>30</day>
<month>12</month>
<year>2022</year>
</pub-date>
<pub-date pub-type="epub">
<day>30</day>
<month>12</month>
<year>2022</year>
</pub-date>
<volume>45</volume>
<numero>4</numero>
<fpage>1251</fpage>
<lpage>1260</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://scielo.pt/scielo.php?script=sci_arttext&amp;pid=S0871-018X2022000301251&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://scielo.pt/scielo.php?script=sci_abstract&amp;pid=S0871-018X2022000301251&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://scielo.pt/scielo.php?script=sci_pdf&amp;pid=S0871-018X2022000301251&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen El papel de los microorganismos en el mantenimiento de un suelo sano y equilibrado es primordial debido a las distintas funcionalidades que ofrecen, los cuales, a su vez, influirán directamente sobre los servicios ecosistémicos de dicho suelo. Su utilización como indicador de la salud del suelo puede ser de gran relevancia a nivel global. En los agroecosistemas, la composición y funcionalidad del microbioma, condicionadas por una cadena de variables ambientales, es un factor determinante en su capacidad productiva. Este trabajo se centra en las diferencias existentes entre el microbioma de un suelo calcáreo y uno calcáreo yipsícola dedicados ambos, al monocultivo de cebada. Para ello se evalúan factores como la diversidad, abundancia o funcionalidad de dichos microbiomas. Los resultados de este trabajo, dado las bajas ratios hongo/bacteria, señalan degradación en ambos casos. Aunque, atendiendo a la mayor diversidad del suelo calcáreo, este parece estar más sano. Por otra parte, hay más especialización, reflejada en mayores abundancias relativas de ciertos microorganismos, en el suelo yesoso. Este último presenta además mayor funcionalidad que puede estar relacionada con la adaptación de dichos microorganismos a mayores factores de estrés.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract The role of microorganisms in maintaining healthy and balanced soil is essential due to the different functionalities they offer, which, in turn, will directly influence the soil ecosystem services. The use of microbiome as an indicator of soil health can be of great relevance at a global level. In agroecosystems, the composition of the microbiome together with the functionalities it offers, balanced or not, will determine the agricultural production of the soil. And all this will be influenced by a chain of interconnected variables that differ between ecosystems. This work focuses on the differences between the microbiome of a calcareous soil and a gypseous soil, both dedicated to barley monoculture. Factors such as microbiome diversity, abundance or functionality are evaluated. The results of this work, given the low fungus/bacteria ratios, indicate soil degradation in both cases. If we consider the greater diversity of the calcareous soil, this seems to be the healthiest. On the other hand, there is more specialization, reflected in greater relative abundances of certain microorganisms, in the calcareous gypsum soil. The latter also has greater functionality that may be related to the adaptation of these microorganisms to greater stress factors.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[microbioma]]></kwd>
<kwd lng="es"><![CDATA[salud del suelo]]></kwd>
<kwd lng="es"><![CDATA[suelo calcáreo]]></kwd>
<kwd lng="es"><![CDATA[suelo yesoso]]></kwd>
<kwd lng="es"><![CDATA[agricultura de secano]]></kwd>
<kwd lng="en"><![CDATA[microbiome]]></kwd>
<kwd lng="en"><![CDATA[soil health]]></kwd>
<kwd lng="en"><![CDATA[calcareous soil]]></kwd>
<kwd lng="en"><![CDATA[gypseous soil]]></kwd>
<kwd lng="en"><![CDATA[rainfed agriculture]]></kwd>
</kwd-group>
</article-meta>
</front><back>
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