CHARACTERIZATION AND CLASSIFICATION OF SOILS IN THE TAQUARI RIVER BASIN - PANTANAL REGION, STATE OF MATO GROSSO DO SUL, BRAZIL

Among the soils in the Mato Grosso do Sul, stand out in the Pantanal biome, the Spodosols. Despite being recorded in considerable extensions, few studies aiming to characterize and classify these soils were performed. The purpose of this study was to characterize and classify soils in three areas of two physiographic types in the Taquari river basin: bay and flooded fields. Two trenches were opened in the bay area (P1 and P2) and two in the flooded field (P3 and P4). The third area (saline) with high sodium levels was sampled for further studies. In the soils in both areas the sand fraction was predominant and the texture from sand to sandy loam, with the main constituent quartz. In the bay area, the soil organic carbon in the surface layer (P1) was (OC) > 80 g kg(-1), being diagnosed as Histic epipedon. In the other profiles the surface horizons had low OC levels which, associated with other properties, classified them as Ochric epipedons. In the soils of the bay area (P1 and P2), the pH ranged from 5.0 to 7.5, associated with dominance of Ca2+ and Mg2+, with base saturation above 50 % in some horizons. In the flooded fields (P3 and P4) the soil pH ranged from 4.9 to 5.9, H+ contents were high in the surface horizons (0.8-10.5 cmol(c) kg(-1)), Ca2+ and Mg-2 contents ranged from 0.4 to 0.8 cmol(c) kg(-1) and base saturation was < 50 %. In the soils of the bay area (P1 and P2) iron was accumulated (extracted by dithionite - Fed) and OC in the spodic horizon; in the P3 and P4 soils only Fed was accumulated (in the subsurface layers). According to the criteria adopted by the Brazilian System of Soil Classification (SiBCS) at the subgroup level, the soils were classified as: P1: Organic Hydromorphic Ferrohumiluvic Spodosol. P2: Typical Orthic Ferrohumiluvic Spodosol. P3: Typical Hydromorphic Ferroluvic Spodosol. P4: Arenic Orthic Ferroluvic Spodosol.

Composição e estrutura arbórea em floresta estacional semidecidual no Espinhaço Meridional (Serra do Cipó, MG)

Estudos florísticos e fitossociológicos têm sido feitos em áreas de Mata Atlântica, sendo parte desses em remanescentes de Floresta Estacional Semidecidual. Entretanto, no cômputo geral, as florestas na Serra do Espinhaço têm sido pouco estudadas. Este trabalho objetiva descrever e analisar a composição e estrutura de espécies arbóreas de uma área de Floresta Estacional Semidecidual na face leste da Serra do Cipó, porção meridional da Serra do Espinhaço (MG). O método de ponto-quadrante foi utilizado para estudo fitossociológico, sendo o levantamento florístico total incrementado por coletas não-sistematizadas. Foram calculados: área basal total, densidade, frequência e dominância relativas, além do índice de valor de importância. O levantamento florístico total registrou 280 espécies, número que destaca a riqueza da área, cuja maior afinidade florística é com outras áreas florestais localizadas nas bacias dos Rios Doce e Paraíba do Sul. Os parâmetros fitossociológicos destacam a predominância de espécies pioneiras e secundárias iniciais, o que, assim como os valores estruturais, caracteriza um estádio secundário inicial a intermediário de regeneração. Os dados deste trabalho realçam a importância da preservação das florestas estacionais da Mata Atlântica e, particularmente, de áreas florestais na porção leste do Espinhaço.