Usos e abusos do território: avaliação ambiental da bacia hidrográfica do Ribeirão Paraíso - Charqueada - SP

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

Implementação em hardware de um sistema inteligente para detecção de plantas daninhas em plantações de soja utilizando máquinas de vetores de suporte e redes neurais artificiais

Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)

Sistema silvipastoril com Myracrodruon urundeuva Fr. All. como alternativa de sustentabilidade

Pós-graduação em Agronomia - FEIS

Desenvolvimento e aplicação de um software cristalográfico com protocolo de acesso a um banco de dados distribuído

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

Caracterização dos sedimentos superficiais e avaliação ambiental da Serra de Monte Alto entre os municípios de Palmas de Monte Alto e Sebastião Laranjeiras, BA

Pós-graduação em Geociências e Meio Ambiente - IGCE

O Afogar das veredas: uma análise comparativa espacial e temporal das veredas do Chapadão de Catalão (GO)

Pós-graduação em Geografia - IGCE

Contribuição dos sedimentos e ictiólitos para a identificação do ambiente de formação do Sambaqui do Moa (Saquarema-RJ)

O Sambaqui do Moa é um sítio arqueológico localizado em Itaúna, Saquarema, litoral do Estado do Rio de Janeiro. Três momentos de ocupação foram reconhecidos neste sítio: o estrato 3 na base correspondente ao início da ocupação deste sítio; o 2, intermediário, aponta para uma ocupação mais intensa, com grande concentração de carapaças de moluscos, ossos de peixes e sepultamentos humanos; e o 1, o mais superficial, relacionado à última ocupação. Para identificar as condições ambientais de desenvolvimento do Sambaqui do Moa foram coletadas amostras de sedimentos e material zooarqueológico nestes três estratos. O material zooarqueológico está representado por restos microscópicos de peixes (ictiólitos), compostos por microdentes com diferentes morfologias: caninos, incisivos e molares. Os sedimentos segundo análises por DRX são constituídos além de quartzo e caulinita, calcita, aragonita e por fluorapatita. Este último é o principal mineral do material zooarqueológico, enquanto calcita e aragonita refletem os restos de conchas contidos neles, abundantes no sítio. As análises mineralógicas foram confirmadas pelas análises químicas, em que os teores elevados de P₂O₅, CaO e PF (H₂O, CO₂), respondem pela fluorapatita, calcita e aragonita. Modificações químicas representadas pelas variações nos conteúdos de C e P nos microdentes sugerem que estes experimentaram mineralização, num processo inicial de fossilização, pósdeposição. Os dados de isótopos estáveis ¹³C e ¹⁵N permitiram definir a fonte de matéria orgânica do sambaqui do Moa como marinha/salobra, em que a vegetação representava-se, predominantemente, por plantas do tipo C3 de floresta tropical. As razões ⁸⁷Sr/⁸⁶Sr nos ictiólitos confirmam que o ambiente no entorno do sambaqui tenha sido estuarino. A morfologia dentária permitiu reconhecer cinco famílias até então não registradas para o sítio, como Labridae, Serranidae, Ariidae, Erythrinidae e Characidae, que confirmam o ambiente estuarino. A idade do sambaqui do Moa por datação radiocarbono a partir dos sedimentos mostrou perturbação no estrato 2, ocasionando a inversão das idades entre os estratos o que pode ser justificado por processos de formação e/ou mudanças dos rios que modificaram as configurações geológico-geomorfológicas da área. Outra explicação poderia ser a interferência humana, devido ao grande número de enterramentos (mais de 30), tenha perturbado a ordem dos momentos de ocupação do sambaqui do Moa, além de possíveis processos erosivos. O sambaqui do Moa se instalou, portanto, em uma área de transição marinho-estuarina.

Variação genética para os caracteres fisiológicos, bioquímicos e nutricionais em sementes de uma população base de Myracrodruon urundeuva procedente de Aquidauana-MS

Pós-graduação em Agronomia - FEIS

Conservação genética Ex Situ de populações naturais de Myracrodruon urundeuva Fr. All. em sistema silvipastoril

Pós-graduação em Agronomia - FEIS

Molecular characterization of fire ants, Solenopsis spp., from Brazil based on analysis of mtDNA gene cytochrome oxidase I

Species from the Solenopsis saevissima (Smith) (Hymenoptera: Formicidae) species group are native to South America and have a cosmopolitan distribution because they have been accidentally introduced in many countries around the world. In Brazil, they have a wide distribution, including urban areas. The present study was conducted to investigate the characterization of Solenopsis genus populations associated with urban/human interference sites in Brazil by analyzing the mitochondrial gene cytochrome oxidase I and estimating the degree of relatedness of these populations to make inferences about their phylogeny and also observe the patterns of mitochondrial haplotype (mitotype) distribution across their range. The results revealed complete geographical coherence and polyphyly for the Solenopsis invicta Buren and Solenopsis saevissima species groups, which confirms the diversity of the genera. It also suggests the possibility that reproductively-isolated populations occur, resulting in the evolutionary process of speciation. No predominant haplotype was found in the populations analyzed, but some were more prevalent.

Avaliação da erodibilidade pelo método Inderbitzen em solo não saturado da região de Bauru - SP

Pós-graduação em Engenharia Civil e Ambiental - FEB

A gênese e a distribuição socioespacial das chuvas no município de Ubatuba-SP

This monograph aims to contribute to the understanding and analysis of extreme events and its correlation with anthropogenic actions, in order to understand the levels of human interference in the environment and to identify potential social and environmental damage that such events may result in Ubatuba, located on the northern coast of São Paulo state. Therefore, two strategies were established, on one hand, episodic analysis of extreme weather events, and on the other, the analysis of the impact of atmospheric phenomena in everyday society. In this case we gave greater emphasis to analysis years that had higher total rainfall. In this sense, the research was based on the standard deviation technique and percentages, which supported to characterize the exceptional rainy years, in addition, use of rhythm analysis technique that has helped to identify the active atmospheric systems. From a qualitative point of view, field works were carried out in order to make use of news by the local press and civil defense for years considered extreme (positive standard deviation). From this, it was analyzed how the extreme episodes of rainfall trigger repercussions in geographic space. Also the spatial distribution of rainfall were carried out by means of quantitative analysis of six rain gauges. It was found that the highest occurrences of impacts, are located in the central areas of the city, as well as the highest rainfall totals. In fact, Ubatuba/SP suffers from very high rainfall totals and has a singularity on the climate...

Landscape changes in Serra do Japi: legal protection or scientific expectation?

The creation of new legally protected areas brings many conflicts that distance the real landscape from the expected according to environmental law or conservation researchers. In this study, we mapped and compared the changes in Serra da Japi (Sao Paulo State, Brazil) throughout 40 years with scenarios of legal protection and scientific expectation on forest conservation, to evaluate the distance between them. This may allow us to infer the direction of historical changes and assist in the debate among decision makers. The results showed that most legal requirements on forest protection in the current landscape have been met. The 1960s was the period when the forest cover was closest to the desirable conservation stage. Although the Serra do Japi has maintained large areas of forests during the entire study period, human interference increased with the expansion of reforestation and urban areas, and access roads were identified as a primary potential driving forces of change. In addition, habitat loss was observed in the landscape, which can represent the first phase of a sequence of modifications detrimental to the environmental conservation of this protected area, including decision changes to land use. In conclusion, the changes evolved toward conservation expectations, but not toward the forest configuration of scientific expectation.

Diatoms, total organic carbon, and total nitrogen of sediment core Dethlingen, Germany

To provide insights into the long-term evolution of aquatic ecosystems without human interference, we here evaluate a decadal- to centennial-scale-resolution diatom record spanning about 12 ka of the Holsteinian interglacial (Marine Isotope Stage 11c). Using a partially varved sediment core from the Dethlingen palaeolake (northern Germany), which has previously been studied for palynological and microfacies signals, we document the co-evolution of the aquatic and surrounding terrestrial environment. The diatom record is dominated by the genera Stephanodiscus, Aulacoseira, Ulnaria and Fragilaria. Based on the diatom assemblages and physical sediment properties, the evolution of the Dethlingen palaeolake can be subdivided into three major phases. During the oldest phase (lasting ~1900 varve years), the lake was ~10-15 m deep and characterized by anoxic bottom-water conditions and a high nutrient content. The following ~5600 years exhibited water depths >20 m, maximum diatom and Pediastrum productivity, and a peak in allochtonous nutrient input. During this phase, water-column mixing became more vigorous, resulting in a breakdown of anoxia. The youngest lake phase (~4000-5000 years) was characterized by decreasing water depth, turbulent water conditions and decreased nutrient loading. Based on our palaeolimnological data, we conclude that the evolution of the Dethlingen palaeolake during the Holsteinian interglacial responded closely to (i) changes within the catchment area (as documented by vegetation and sedimentation) related to the transition from closed forests growing on nutrient-rich soils (mesocratic forest phase) to open forests developing on poor soils (oligocratic forest phase), and (ii) short-term climate variability as reflected in centennial-scale climate perturbations.