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Abstract
Los cinco perfiles de Mollisoles estudiados en el Sector occidental de la Sierra de Gádor son: Lithic vermic Haploxeroll, Entic haploxeroll, Ruptic Palexeralfic lithic Argixeroll, Entic vermic Haploxeroll y Lithic ruptic xerorthentic vermic Haploxeroll. Los factores que condicionan la existencia de este tipo de suelos son roca madre carbonatada (caliza, dolomía, margocaliza, etc.), posición fisiográfica de ladera con pendientes variables (20-60 %), vegetación de matorral, clima mediterráneo con diferentes variantes dependiendo de la altitud, régimen de humedad del suelo Xérico y de temperatura Térmico y Mésico. La secuencia de horizontes es variable. En una parte importante de los suelos, debajo del epipedón móllico se presenta un contacto lítico, en otros existe un horizonte Bw y en menor medida un horizonte Bt las texturas más comunes pertenecen a las clases francas. El contenido de carbonatos es importante salvo en el Argixeroll. El carbono orgánico se presenta en el epipedón móllico en contenidos elevados (2.3 a 6.8 %) a excepción del Entic Haploxeroll, cercano al 1 %. Son suelos de pH 8 y saturados en bases.
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