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Pedogenesis of plinthite during early Pliocene in the Mediterranean environment

2007; Elsevier BV; Volume: 71; Issue: 3 Linguagem: Inglês

10.1016/j.catena.2007.03.015

1872-6887

Edoardo A.C. Costantini, Simone Priori,

Iron oxide chemistry and applications

A complex buried paleosol at Podere Renieri at Montalcino (central Italy) formed during a series of continental episodes within an interval of Pliocene marine sediments from about 4.1 to 4.8 My BP. The aim of this work was to document the kind of pedogenesis which occurred throughout this time and, in particular, the plinthite formation. Plinthite (soft and hard) is poor in organic carbon, neutral or subalkaline, dominated by illite, and enriched in iron and chromium. The main differences between soft and hard plinthite are attributed to soil structure, which is absent in hard plinthite, and to the abundance of iron depleted zones, which are much larger in soft plinthite. Variations in mineralogy, chemistry and genesis of soft and hard plinthite can be ascribed to the specific environment of plinthite formation, close to the Pliocene sea. Pedogenetic evidence indicates that plinthite evolved in a hot and humid paleoclimate, showing a progressive increase in seasonality, and that low-grade plinthite formation occurred in a time span of a few hundred thousand years. Soils with low-grade plinthite have agronomic value in their suitability for the production of high quality Brunello di Montalcino wine.