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.

Contribuição para o estudo dos Rhinotragini (Coleoptera, Cerambycidae). VI. Ecliptoides Tavakilian & Peñaherrera-Leiva, 2005

The genus Ecliptoides Tavakilian & Peñaherrera-Leiva, 2005, recently revised by Clarke (2009) to include three Bolivian species, is brought up-to-date by the inclusion of further South American species transferred from Eclipta Bates, 1873, and Odontocera Audinet-Serville, 1833. Three new species are described from Brazil: E. schmidi, E. tavakiliani, and E. hogani. Ommata eunomia var. rufula Melzer, 1934, and Ommata (Eclipta) plaumanni Fuchs, 1961, are revalidated and considered species of Ecliptoides. Species transferred from Eclipta to include Ecliptoides: E. bivitticollis (Fisher, 1952); E. eunomia (Newman, 1841); E. pilosipes (Peñaherrera-Leiva & Tavakilian, 2004); E. fanchonae (Tavakilian & Peñaherrera-Leiva, 2003); E. giuglarisi (Peñaherrera-Leiva & Tavakilian, 2004); E. vasconezi (Peñaherrera-Leiva & Tavakilian, 2004); E. vicina (Melzer, 1927); E. lauraceae (Peñaherrera-Leiva & Tavakilian, 2004); and E. bauhiniae (Peñaherrera-Leiva & Tavakilian, 2004). Species transferred from Odontocera to include Ecliptoides: O. quadrivittata Melzer, 1922; O. pusilla Gounelle, 1911; and O. monostigma (Bates, 1869). New synonymy: Ommata (Eclipta) collarti Fuchs, 1959 = Odontocera pusilla Gounelle, 1911 (= Ecliptoides pusillus). Lectotypes are designated for Ommata (Eclipta) vicina, and Ommata (Eclipta) collarti. New distribution records are provided for E. eunomia, E. pilosipes, E. plaumanni and E. fanchonae. A key to the species of Ecliptoides is given.

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 Mg² 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.