Suelos y los servicios ecosistémicos
Soils and ecosystem services
DOI:
https://doi.org/10.56469/rae.v2i1.2063Resumen
La materia orgánica del suelo, y en particular el elemento más abundante en ella, el Carbono (C), son los que movilizan la mayoría de los procesos biológicos, físicos y químicos que ocurren en el suelo.
El manejo de la materia orgánica del suelo (MOS) se ha centrado tradicionalmente en la mejora de la productividad de los cultivos. Por lo tanto, MOS se ha considerado principalmente como una fuente de nutrientes para las plantas, y las prácticas agrícolas fueron desarrollados con la premisa de extraer más fácilmente los nutrientes vegetales durante la fase de cultivo y para reponer las reservas de nutrientes durante la fase de no-cultivo de la rotación (Whitbread et al. 2000). La rotación de cultivos de cosecha y barbechos a base de pasturas perennes confiere estabilidad al sistema del suelo y era un sistema de producción agrícola sostenible hasta la llegada de los fertilizantes inorgánicos, herbicidas, el mejoramiento genético de cultivos de alto rendimiento y la innovación tecnológica de la labranza mecanizada, que en su conjunto constituyó la llamada “revolución verde”. Estos cambios globales provocaron una mejora sustancial en la producción de alimentos pero también producen un desacoplamiento de los procesos biológicos con las concentraciones de los nutrientes esenciales en el suelo (Tonitto et al. 2006). La disponibilidad de fuentes de nitrógeno sintético de bajo costo y herbicidas eficientes ha promovido esta
tendencia, y permitió a vastas áreas de las tierras más productivas del mundo para ser cultivadas con un tipo de cultivo durante períodos prolongados (Tilman et al. 2002). El problema inherente asociado con este tipo de manejo de las tierras es una reducción drástica de la diversidad vegetal sobre el suelo, que también se traduce en una disminución de la actividad y la
diversidad microbiana del suelo (Milcu et al. 2010), y por lo tanto en una pérdida de las funciones vitales el suelo (Nielsen et al. 2011). La producción de biomasa, la protección de los seres humanos y el medio ambiente, reservorio de genes, base física de
las actividades humanas, el origen de las materias primas, y el patrimonio geogénica y cultural se han identificado como principales funciones del suelo (Blum 2005). Los suelos son organismos vivos y sus múltiples funciones ecosistémicas están íntimamente relacionados con las transformaciones y la dinámica de la MOS, que están mediadas por la actividad biótica del suelo y la dinámica estructural del suelo (Six et al. 2002). Por lo tanto, el manejo del suelo para múltiples servicios ecosistémicos tiene que centrarse en el vínculo entre la MOS, la estructura del suelo y la biota del suelo y los factores que regulan de este enlace (Six et al. 2004, Wardle et al. 2004).
Recientemente, se ha producido un fuerte enfoque en la MOS como reservorio de C y un mecanismo de secuestro de C y la protección del cambio climático (Lal 2004, Powlson et al. 2011), pero mucho menos atención fue dada a la gestión de los servicios de regulación, los culturales y los de apoyo. La importancia del carbono del suelo en relación a abordar apremiantes problemas mundiales a través de la provisión de diversos servicios ecosistémicos ha sido reconocido por los responsables políticos hasta hace tiempos muy recientes (Victoria et al. 2012).
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