Síndrome do comportamento em roedores muroides da Reserva Florestal do Morro Grande e suas possíveis implicações: resposta à fragmentação, dinâmica sucessional e taxa metabólica basal

Embora a fragmentação da paisagem seja apontada como uma das principais alterações antrópicas ao meio ambiente, sabe-se que nem todas as espécies são afetadas da mesma forma por este processo. Resultados obtidos na Reserva Florestal do Morro Grande (RFMG) encontraram ainda relação entre a vulnerabilidade diferenciada à fragmentação e a dinâmica sucessional em roedores. Estudos recentes sugerem que estas respostas diferenciais poderiam estar associadas a perfis metabólico/comportamentais, com consequências para a capacidade de exploração do habitat e utilização de recursos. Neste trabalho investigamos aspectos comportamentais e do metabolismo energético de três espécies de roedores da RFMG, já classificados como sensíveis (Euryoryzomys russatus) e tolerantes à fragmentação (Akodon montensis e Oligoryzomys nigripes), a fim de testar se estes fatores explicariam em parte suas diferentes vulnerabilidades. Analisou-se ainda a relação existente entre o metabolismo energético (expresso pela taxa metabólica basal, TMB) e o comportamento em nível de indivíduos. Por meio de testes comportamentais verificamos que não há diferença significativa entre os níveis exploratórios de espécies tolerantes e sensíveis à fragmentação. Por outro lado, a tendência de diferenciação na TMB entre as espécies foi bastante clara, com Euryoryzomys apresentando o mais alto metabolismo basal. As características de baixo metabolismo basal e plasticidade metabólica encontradas em Akodon e Oligoryzomys podem, de fato, estar contribuindo para o sucesso dessas espécies em áreas fragmentadas e alteradas. Foi encontrada ainda relação negativa entre a TMB e comportamentos custosos para duas das espécies, demonstrando predomínio do Modelo da Partilha, aparentemente adaptativo em ambientes imprevisíveis e com baixa produtividade, já que caracteriza animais com baixa demanda... (Resumo completo, clicar acesso eletrônico abaixo)

Mapeamento geológico-geomorfológico do Morro Azul na região de Limeira, SP, na escala 1:10 000

Geologic and geomorphologic mapping are important ways to characterize the environment, because they look to describe and diagnose landforms, identifying and understanding the morphogenetic processes, making it possible to comprehend the landscape dynamic. This work aimed to make a geological and geomorphological map, in a 1:10.000 scale, of the Morro Azul, the main elevation in the city of Limeira – SP, with the application of photogeological techniques and field descriptions. As final products are presented a geological-geomorphological map, a topographical profile, a slope map, beyond the main characteristics of the geological-geomorphological units of the area. This study presents itself as a preliminary work, and can serve as a subsidy to more specific works, such as geotechnics, environmental problems, among others

Análises de solos e sedimentos de corrente, nas áreas das usinas de fundição de chumbo do Calabouço (CIEM-CPRM) e de beneficiamento de minério aurífero do Morro do Ouro (Parque Municipal Morro do Ouro), no município de Apiaí - SP

Located in Apiaí, Vale do Ribeira, southern region of São Paulo state, the Usina do Calabouço areas (CIEM / CPRM) and Morro do Ouro (Parque Municipal do Morro do Ouro), were targeted for stud ies due to its old buildings, respectively a foundry in lead ore, called Experimental de Chumbo e Prata (Usina Calabouço), and a gold mine with processing plant of the gold-bearing ore produced there. Nowadays, the areas are used for public visitation, and in both places the rests of the buildings remains. Particularly in the CIEM/CPRM, due to the materials witch was produced before, it can suggest the existence of anomalous amounts of the involved metals (CIEM / CPRM) and possible contaminations by chemical products used in the improvement of the auriferous ore (P. M. Morro do Ouro). These potential contamination were confirmed with geochemical survey of soils and current sediments accomplished in both areas, for the elements arsenic, cadmium, lead, copper, mercury, silver and zinc, which were used as parameters guiding values for soil and groundwater the state of São Paulo (CETESB), and watershed values stipulated by CPRM (poor, background and anomalous), in it rising geochemistry during Folha Apiaí's execution (SG-22-X-B-V).

Mapeamento geológico no alvo Morro do Corcunda - Greenstone Belt Pilar de Goiás (Santa Terezinha-GO)

The following work refers to a geologic mapping in the Morro do Corcunda target, located between the cities of Pilar of Goiás and Santa Terezinha in the northwest portion of the State of Goiás. This mapping was carried through in 1:10,000 scale and covers an area of approximately 60km2. Collections of samples had been carried through for laborarorial analysis, and from those twenty-three thin scetions have been produced in order to describe the main lithologies that occur in the area. It was possible to observe anomalous gold targets in the region through chip samples carried through during the stage of field work. The gathered field data and the ones that have been made available by the company Yamana Gold Incorporation were congregated, and a data integration was carried through. This integration made possible the correlation of the litologies found in field with the Greenstone Belt Pilar de Goiás sequence and the structural evolution of the area.

Spatio-temporal distribution of calling male frogs in Morro do Diabo State Park (Southeastern Brazil): implications for conservation and management in a seasonally dry tropical forest

The aims of this study are to determine how anuran calling males are spatially and temporally distributed in the Morro do Diabo State Park (MDSP), and to test for indicator species in different breeding habitats. We found high species turnover among breeding habitats of different hydroperiods. Our results indicate that spatial partitioning is more important than seasonal occurrence in permitting species coexistence at MDSP. Indicator Species Analysis identified one species associated with a local stream, one species associated with permanent ponds, two species associated with temporary ponds, and three species associated with a semipermanent pond. Guilds of species do not appear to stratify their distributions throughout the year, since most species occur during the rainy and warm months and are thus temporally overlapping. The main conservation implication of our work is the need to protect the different areas of the park where these unique breeding habitats, and their associated anuran assemblages, are found.

Prospecção mineral de alvos potenciais à ocorrência de enriquecimento supergênico de níquel no Greenstone belt do Morro do Ferro

Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)

SIG aplicado na caracterização morfométrica da microbacia do Ribeirão Morro Grande - Bofete, SP

Esse trabalho objetivou a aplicação de geoprocessamento na caracterização morfométrica da microbacia do Ribeirão Morro Grande – Bofete (SP) através do Sistema de Informação Geográfica – Selva, visando à preservação, racionalização do seu uso e recuperação ambiental. A microbacia apresenta uma área de 4049ha e está localizada entre os paralelos 22o 50' 05" a 22o 54' 26" de latitude S e 48o 22' 29" a 48o 26' 36" de longitude W Gr. A base cartográfica utilizada foi a carta planialtimétrica de Bofete (SP), em escala 1:50.000 (IBGE, 1968) na extração das curvas de nível, da hidrografia e da topografia, em ambiente de Sistema de Informações Geográficas - Idrisi Selva, para determinação dos índices morfométricos. Os resultados mostram que os baixos valores da densidade de drenagem, associados à presença de rochas permeáveis, facilitam a infiltração da água no solo, diminuindo o escoamento superficial e o risco de erosão e da degradação ambiental, bem como o baixo valor do fator de forma amparado pelo índice de circularidade indica que a microbacia tende a ser mais alongada com menor susceptibilidade à ocorrência de enchentes mais acentuadas. O parâmetro ambiental coeficiente de rugosidade permitiu classificar a microbacia para vocação com floresta e reflorestamento.

Avaliação das áreas de conflito de uso em APP na microbacia do ribeirão Morro Grande

Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)

Multifuncionalidade da paisagem em assentamentos rurais nos entornos de usina canavieira e do Parque Estadual Morro do Diabo (SP)

Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)

Multifuncionalidade da paisagem em assentamentos rurais nos entornos de usina canavieira e do Parque Estadual Morro do Diabo (SP)

Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)

The supergene thorium and rare-earth element deposit at Morro do Ferro, Poços de Caldas, Minas Gerais, Brazil

The thorium and rare-earth element (Th-REE) deposit at Morro do Ferro formed under supergene lateritic weathering conditions. The ore body consists of shallow NW-SE elongated argillaceous lenses that extend from the top of the hill downwards along its south-eastern slope. The deposit is capped by a network of magnetite layers which protected the underlying highly weathered, argillaceous host rock from excessive erosion. The surrounding country rocks comprise a sequence of subvolcanic phonolite intrusions that have been strongly altered by hydrothermal and supergene processes. From petrological, mineralogical and geochemical studies, and mass balance calculations, it is inferred that the highly weathered host rock was originally carbonatitic in composition, initially enriched in Th and REEs compared to the surrounding silicate rocks. The intrusion of the carbonatite caused fenitic alteration in the surrounding phonolites, consisting of early potassic alteration followed by a vein-type Th-REE mineralization with associated fluorite, carbonate, pyrite and zircon. Subsequent weathering has completely decomposed the carbonatite forming a residual supergene enrichment of Th and REEs. Initial weathering of the carbonatite has created a chemical environment that might have been conductive to carbonate and phosphate complexing of the REEs in groundwaters. This may have appreciably restricted the dissolution of primary REE phases. Strongly oxidic weathering has resulted in a fractionation between Ce and the other light rare earth elements (LREEs). Ce3+ is oxidized to Ce4+ and retained together with Th by secondary mineral formation (cerianite, thorianite), and by adsorption on poorly crystalline iron- and aluminium-hydroxides. In contrast, the trivalent LREEs are retained to a lesser degree and are thus more available for secondary mineral formation (Nd-lanthanite) and adsorption at greater depths down the weathering column. Seasonally controlled fluctuations of recharge waters into the weathering column may help to explain the observed repetition of Th-Ce enriched zones underlain by trivalent LREE enriched zones.