In the southwest United States, the current prolonged warm drought is similar to the predicted future climate change scenarios for the region. This study aimed to determine patterns in vegetation response to the early 21st century drought across multiple biomes. We hypothesized that different biomes (forests, shrublands, and grasslands) would have different relative sensitivities to both climate drivers (precipitation and temperature) and legacy effects (previous-year's productivity). We tested this hypothesis at eight Ameriflux sites in various Southwest biomes using NASA Moderate-resolution Imaging Spectroradiometer Enhanced Vegetation Index (EVI) from 2001 to 2013. All sites experienced prolonged dry conditions during the study period. The impact of combined precipitation and temperature on Southwest ecosystems at both annual and sub-annual timescales was tested using Standardized Precipitation Evapotranspiration Index (SPEI). All biomes studied had critical sub-annual climate periods during which precipitation and temperature influenced production. In forests, annual peak greenness (EVImax) was best predicted by 9-month SPEI calculated in July (i.e., January-July). In shrublands and grasslands, EVImax was best predicted by SPEI in July through September, with little effect of the previous year's EVImax. Daily gross ecosystem production (GEP) derived from flux tower data yielded further insights into the complex interplay between precipitation and temperature. In forests, GEP was driven by cool-season precipitation and constrained by warm-season maximum temperature. GEP in both shrublands and grasslands was driven by summer precipitation and constrained by high daily summer maximum temperatures. In grasslands, there was a negative relationship between temperature and GEP in July, but no relationship in August and September. Consideration of sub-annual climate conditions and the inclusion of the effect of temperature on the water balance allowed us to generalize the functional responses of vegetation to predicted future climate conditions. We conclude that across biomes, drought conditions during critical sub-annual climate periods could have a strong negative impact on vegetation production in the southwestern United States.

The problem in this study was to examine the relationship between health education and physical education as areas of specialization as perceived by selected health and physical educators in five southwestern states. Data for the study were obtained by use of a questionnaire. Surveyed educators consisted of college and university department chairmen, secondary curriculum directors, and secondary instructors. The data were presented in such a manner to indicate opinions of the total group of respondents as well as those of each of the three categories. The findings of the study indicate that health education and physical education are related historically and are substantially related at the current time, and that specialization in teacher preparation and instruction in each area is desirable.

Ancestral Pueblo communities of the central Mesa Verde region (CMVR) became increasingly reliant on agriculture for their subsistence needs during Basketmaker III (BMIII) through Terminal Pueblo III (TPIII) (AD 600–1300) periods. Researchers have been studying the Ancestral Pueblo people for over a century using a variety of methods to understand the relationships between climate, agriculture, population, and settlement patterns. While these methods and research have produced a well-developed cultural history of the region, studies at a smaller scale are still needed to understand the changes in farming behavior and the distribution of individual sites across the CMVR. Soil moisture is the limiting factor for crop growth in the semi-arid region of the Goodman Watershed in the CMVR. Thus, I constructed the soil moisture proxy model (SMPM) that is on a local scale and focuses on variables relevant to soil moisture – soil particle-size, soil depth, slope, and aspect. From the SMPM output, the areas of very high soil moisture are assumed to represent desirable farmland locations. I describe the relationship between very high soil moisture and site locations, then I infer the relevance of that relationship to settlement patterns and how those patterns changed over time (BMIII – TPIII). The results of the model and its application help to clarify how Ancestral Pueblo people changed as local farming communities. The results of this study indicates that farmers shifted away from use of preferred farmland during Terminal Pueblo III, which may have been caused by other cultural factors. The general outcome of this thesis is an improved understanding of human-environmental relationships on the local landscape in the CMVR.

The archaeofaunal remains left by the Ancestral Puebloan people of Goodman Point Unit provides a valuable, yet underutilized resource into pit structure function. This thesis explores temporal changes in pit structure use and evaluates if a final feast occurred during a kiva decommissioning. The results from zooarchaeological analyses of a pithouse and two great kivas suggest that changes in pit structures at Goodman Point mimic the regional trend toward specialization until late Pueblo III. Cross-cultural studies on feasts, southwest ethnographies and previous zooarchaeological work established methods for identifying a feast. The analysis of differences in faunal remains from a great kiva and multiple room block middens imply that the remains in the kiva were from a final feast prior to a decommissioning ceremony and were not fill. Spatially and temporally the great kiva appears to be a unique, specialized structure in the cultural development of the Goodman Point community.

Os radionuclídeos naturais das séries radioativas do 238U e do 232Th têm sido aplicados com sucesso como traçadores de processos ambientais atuais e mudanças climáticas. O 210Pb (meia-vida de 22,2 anos) é empregado na técnica de datação geocronológica de testemunhos sedimentares dos últimos 100-150 anos e na determinação de taxa de sedimentação. As concentrações dos isótopos 226Ra e 228Ra (meia-vida de 1.600 anos e 5,75 anos, respectivamente) auxiliam no cálculo das atividades de 210Pb em excesso no sedimento e auxiliam na identificação de processos marinhos importantes, como, por exemplo, a intrusão de água subterrânea. Neste trabalho foram quantificadas as concentrações de atividade de 226Ra, 228Ra e 210Pb em quatro testemunhos marinhos curtos coletados desde a plataforma continental até o talude superior do Atlântico Sudoeste. A partir dos resultados obtidos, as taxas de sedimentação em cada local e as idades de cada fatia de sedimento foram determinadas pelo método de datação geocronológica com 210Pb. As amostras sedimentares sofreram digestão total ácida em microondas. A separação radioquímica sequencial de 226Ra, 228Ra e 210Pb foi realizada com a obtenção dos precipitados de Ba(Ra)SO4 e PbCrO4. As medidas α total do 226Ra e β total do 228Ra e do 210Pb a partir dos precipitados foram feitas em um detector proporcional de fluxo gasoso de baixa radiação de fundo. Com relação aos testemunhos analisados, as concentrações de atividade dos radionuclídeos variaram de 14 Bq.kg-1 a 154 Bq.kg-1 para o 226Ra; de 17 Bq.kg-1 a 45 Bq.kg-1 para o 228Ra; de 20 Bq.kg-1 a 2.073 Bq.kg-1 para o 210Pb. Valores altos de 210Pb foram encontrados no topo de todos os perfis sedimentares, proveniente principalmente da deposição atmosférica. Os dados coletados neste trabalho estão na mesma faixa de grandeza de outros relacionados a medições de 226Ra, 228Ra, 210Pb em áreas não contaminadas do Oceano Atlântico Sudoeste. As taxas de sedimentação diminuíram com o aumento da profundidade de coluna dágua, cujos valores variaram de 0,049 cm.ano-1 a 0,40 cm.ano-1. / Natural radionuclides from 238U and 232Th series have been successfully applied as tracers of environmental process and climate changes. The 210Pb (half-life of 22.2 years) is used in the geochronological dating technique of sediment cores of the last 100-150 years, and its respective sedimentation rate determination. The study of 226Ra and 228Ra concentrations (half-lives of 1,600 years and 5.75 years, respectively) helps calculate the activity of 210Pb in excess in the environment, besides being important tracers of marine processes, as ground water discharge. In this work it was determined the activity concentrations of 226Ra, 228Ra and 210Pb in four short marine cores collected since the continental platform to upper slope of Southwest Atlantic Ocean. Taking into account the results obtained, sedimentation rates and the ages of each sediment layer were determined using the geochronological dating method with 210Pb. All sediment samples were total acid digested in microwave. The sequential radiochemical separation of 226Ra, 228Ra, 210Pb were performed, obtaining in the end the precipitation of Ba(Ra)SO4 and PbCrO4. The gross α measurements of 226Ra and gross β measurements of 228Ra and 210Pb from the precipitates were carried out in a gas-flow low background proportional counter. Concerning all cores analyzed, the activities concentrations of 226Ra ranged from 14 Bq.kg-1 to 154 Bq.kg-1; the concentrations of 228Ra ranged from 17 Bq.kg-1 to 45 Bq.kg-1; and the concentrations of 210Pb ranged from 20 Bq.kg-1 to 2,073 Bq.kg-1. High values of 210Pb were observed on the top of all the cores studied, mainly related to atmospheric deposition. The results obtained in this work were of the same order of magnitude of those reported in the literature available on non contaminated areas of Southeast Brazilian Coast. Sedimentation rates fall with the increase of water column depth and ranged from 0,049 cm.ano-1 to 0.40 cm.y-1.

A demanda crescente de alimentos gera problemas ambientais, principalmente devido à remoção das coberturas vegetais nativas para a expansão da agricultura no Brasil. Essas alterações no uso da terra acarretam mudanças na dinâmica da matéria orgânica do solo. O tipo de vegetação também tem influência sobre a biota do solo e, por isso, a sua alteração ocasiona mudanças na biomassa microbiana, como revelam estudos envolvendo desmatamento. Os microorganismos representam a maior diversidade biológica e fisiológica do solo, além de serem responsáveis por mais de 95% dos processos de decomposição e ciclagem de nutrientes. Por este motivo, a demanda por indicadores rápidos e confiáveis para detectar alterações na qualidade do solo, principalmente por aqueles com base nos microrganismos, vem crescendo continuamente. O objetivo geral foi verificar se há diferenciação dos padrões da atividade e da diversidade funcional da biomassa microbiana dos solos sob as diferentes vegetações naturais, pastagens em uso e sistemas agrícolas recém implantados. A área de abrangência desta pesquisa corresponde aos estados de Rondônia (RO) e Mato Grosso (MT), que foi dividida em 11 ecorregiões relativamente homogêneas em termos de solos, vegetação nativa, geologia, clima e relevo. Foi realizada a análise da variável canônica de alguns atributos físicos, químicos e microbiológicos de cada ecorregião e uso da terra, buscando evidenciar padrões e as variáveis que os diferenciam. As áreas nativas apresentaram padrões distintos na dinâmica dos atributos microbiológicos relacionadas principalmente à quantidade de serapilheira em cada bioma estudado. Em relação às áreas antropizadas, observaram-se resultados similares entre pastagens e áreas nativas, significativamente diferentes dos resultados obtidos em áreas agrícolas, que devido à diferença de manejo e diversidade de culturas analisadas apresentou uma grande variabilidade no seu resultado final. Os resultados obtidos reforçam a recomendação da utilização dos atributos microbiológicos como indicadores de mudança de uso da terra, aliados a fatores químicos e físicos. A respiração induzida por substratos (ou diversidade catabólica) mostrou-se eficiente na separação dos usos da terra e ecorregiões. Estes resultados suportam a idéia de que cada forma de uso da terra induz a presença de grupos específicos de microrganismos, independente de tipo de solo, clima ou outras influências externas. / The increasing demand for food creates environmental problems, mainly due to the removal of native vegetation cover for agriculture expansion in Brazil. These changes in land use leads to changes in the soil organic matter dynamics. The vegetation type also affects the soil biota and, therefore, its change causes modifications in the microbial biomass, as shown by studies involving deforestation. Microorganisms represent the most biological and physiological diverse in soil, as well as being responsible for more than 95% of the decomposition and nutrient cycling. For this reason, the demand for fast and reliable indicators to detect changes in soil quality, especially for those based on micro-organisms has been growing continuously. The main objective in this research was to check the differentiation of patterns in activity and functional diversity of soil microbial biomass under natural vegetation, pastures and agricultural systems in use. The area covered by this study corresponds to the states of Rondônia (RO) and Mato Grosso (MT), which was divided into 11 ecoregions relatively homogeneous in terms of soil, vegetation, geology, climate and landscape. A canonical variate analysis was used in some physical, chemical and microbiological factors in each ecoregion and land use, looking for patterns and variables that can differentiate them. The native areas showed distinct patterns in the dynamics of microbiological attributes mainly related to the amount of litter in each biome studied. For the disturbed areas, there were similar results between pastures and native areas, significantly different from the results obtained in agricultural areas, which due to differences in management and kind of cultures analyzed showed a great variability in its final result. The results support the recommendation for use of microbiological attributes as indicators of land use change, combined with chemical and physical factors. The substrate-induced respiration (or catabolic diversity) was efficient in the separation of land uses and ecoregions. These findings support the idea that specific land uses have specific groups of microbial biomass, regardless soil type, climate or other external influences.

A composição e distribuição das larvas pelágicas dos invertebrados bênticos do Banco dos Abrolhos, em especial de caranguejos braquiúros, foram investigadas com base em duas abordagens de campo, em larga e pequena escala. A primeira abrangeu todo o banco e regiões adjacentes, com 46 estações de coleta amostradas uma única vez, entre julho-agosto de 2007. Na segunda, as coletas de plâncton ocorreram em dois períodos e se concentraram ao redor do Recife de Sebastião Gomes (a 15 km da costa) e do Arquipélago dos Abrolhos (a 60 km). Em larga escala, as comunidades meroplanctônica e de larvas de Brachyura foram divididas em comunidades de águas rasas (profundidade < 100 m), com maior abundância e diversidade, e de águas profundas (profundidade > 450 m), indicando que o meroplâncton está bem distribuído ao longo do banco, mas que evita a dispersão para o oceano aberto. A composição de larvas de Brachyura atesta que não houve influência estuarina na área de estudo. Entretanto, a ocorrência e dominância de larvas de espécies típicas do entremarés apenas nas estações mais costeiras, sugere a existência de um mecanismo de retenção larval na região oeste do banco. A homogeneidade na distribuição e abundância das larvas de braquiúros somada às altas concentrações de zoés iniciais da maior parte dos táxons por toda a área rasa indica a existência de certo grau de conectividade via dispersão larval entre as populações adultas. Na pesquisa em pequena escala, a comparação entre os dois ambientes do Banco de Abrolhos com base nos grandes grupos meroplanctônicos não resultou em nenhuma diferença. Por outro lado, a composição da comunidade de larvas de Brachyura diferiu entre os ambientes, mas apenas em termos de espécies dominantes. No geral, não foram verificadas diferenças entre os dois períodos de coleta nas áreas rasas investigadas. O trabalho de identificação das larvas de Brachyura levou à elaboração da primeira chave de identificação ilustrada que engloba as larvas já descritas de todas as espécies do litoral brasileiro. / The composition and distribution of benthic invertebrate larvae of Abrolhos Bank were investigated in this study, with emphasis on brachyuran crabs. A mesoscale field approach encompassed the entire bank and adjacent areas from the inner shelf to the open ocean, where vertical plankton tows were carried out between July-August 2007. Meroplankton larvae, including brachyuran representatives, were more abundant and diverse in shallow stations (depth <100 m) than in deep water (depth> 450 m), suggesting that meroplankton is well distributed along the bank but avoids advection towards the open ocean. The estuarine influence on the study area was negligible or virtually inexistent, as suggested by the brachyuran larval composition. However, the occurrence and dominance of larvae of intertidal species in stations close to the coast suggest the existence of a larval retention mechanism in this area. The homogeneity in the distribution and abundance of brachyuran larvae added to the high concentration of initial zoeae of most taxa across the entire shallow area indicate the existence of some degree of connectivity via larval dispersion among adult populations. In addition to the mesoscale study, a small-scale sampling scheme around Sebastião Gomes reef (15 km from the coast) and Abrolhos Archipelago (60 km) was implemented in two seasonal periods. No difference was found between these two environments based in terms of abundance and ecological indexes. On the other hand, the composition of the brachyuran community was different between the environments, especially in the case of dominant species. No seasonal differences were detected in those shallow areas. The identification of brachyuran larvae during the course of this study led to the development of the first key for the identification of known first zoeal stages of brachyuran crabs from the Brazilian coast.

Esse trabalho busca compreender como ocorreu a ocupação do sítio Jaguarundi, com ênfase no estudo das escolhas técnicas inseridas na confecção dos artefatos arqueológicos, da paisagem arqueológica, da dieta alimentar e do padrão de assentamento. Procura-se estudar comparativamente os dados arqueológicos, históricos e etnográficos da região de modo a elucidar sobre o processo histórico do contexto de ocupação e as dinâmicas sócio-culturais empreendidas pelas populações que ali se estabeleceram, para tanto o estudo se centrou na identificação das estruturas arqueológicas para que elas possam ser utilizadas na construção de um modelo analítico para ser empregado em futuras análises de sítios similares. / This work aimed at finding out how happened the occupation of the Jaguarundi site, with emphasis in the study of the technical choices inserted in the manufacture of the archaeological artifacts, of the archaeological landscape, of the alimentary diet ant de settlement pattern. Aiming for the comparative study of the archaeological historical e ethnological data of the region, escheating a elucidation about the historical process of the settlement context and the socio-cultural dynamics ocasionated by the established populations, for this the research centers in the identification of the archaeological structures for the construction of a analytical model for future comparative analyses in similar sites.

A demanda crescente de alimentos gera problemas ambientais, principalmente devido à remoção das coberturas vegetais nativas para a expansão da agricultura no Brasil. Essas alterações no uso da terra acarretam mudanças na dinâmica da matéria orgânica do solo. O tipo de vegetação também tem influência sobre a biota do solo e, por isso, a sua alteração ocasiona mudanças na biomassa microbiana, como revelam estudos envolvendo desmatamento. Os microorganismos representam a maior diversidade biológica e fisiológica do solo, além de serem responsáveis por mais de 95% dos processos de decomposição e ciclagem de nutrientes. Por este motivo, a demanda por indicadores rápidos e confiáveis para detectar alterações na qualidade do solo, principalmente por aqueles com base nos microrganismos, vem crescendo continuamente. O objetivo geral foi verificar se há diferenciação dos padrões da atividade e da diversidade funcional da biomassa microbiana dos solos sob as diferentes vegetações naturais, pastagens em uso e sistemas agrícolas recém implantados. A área de abrangência desta pesquisa corresponde aos estados de Rondônia (RO) e Mato Grosso (MT), que foi dividida em 11 ecorregiões relativamente homogêneas em termos de solos, vegetação nativa, geologia, clima e relevo. Foi realizada a análise da variável canônica de alguns atributos físicos, químicos e microbiológicos de cada ecorregião e uso da terra, buscando evidenciar padrões e as variáveis que os diferenciam. As áreas nativas apresentaram padrões distintos na dinâmica dos atributos microbiológicos relacionadas principalmente à quantidade de serapilheira em cada bioma estudado. Em relação às áreas antropizadas, observaram-se resultados similares entre pastagens e áreas nativas, significativamente diferentes dos resultados obtidos em áreas agrícolas, que devido à diferença de manejo e diversidade de culturas analisadas apresentou uma grande variabilidade no seu resultado final. Os resultados obtidos reforçam a recomendação da utilização dos atributos microbiológicos como indicadores de mudança de uso da terra, aliados a fatores químicos e físicos. A respiração induzida por substratos (ou diversidade catabólica) mostrou-se eficiente na separação dos usos da terra e ecorregiões. Estes resultados suportam a idéia de que cada forma de uso da terra induz a presença de grupos específicos de microrganismos, independente de tipo de solo, clima ou outras influências externas. / The increasing demand for food creates environmental problems, mainly due to the removal of native vegetation cover for agriculture expansion in Brazil. These changes in land use leads to changes in the soil organic matter dynamics. The vegetation type also affects the soil biota and, therefore, its change causes modifications in the microbial biomass, as shown by studies involving deforestation. Microorganisms represent the most biological and physiological diverse in soil, as well as being responsible for more than 95% of the decomposition and nutrient cycling. For this reason, the demand for fast and reliable indicators to detect changes in soil quality, especially for those based on micro-organisms has been growing continuously. The main objective in this research was to check the differentiation of patterns in activity and functional diversity of soil microbial biomass under natural vegetation, pastures and agricultural systems in use. The area covered by this study corresponds to the states of Rondônia (RO) and Mato Grosso (MT), which was divided into 11 ecoregions relatively homogeneous in terms of soil, vegetation, geology, climate and landscape. A canonical variate analysis was used in some physical, chemical and microbiological factors in each ecoregion and land use, looking for patterns and variables that can differentiate them. The native areas showed distinct patterns in the dynamics of microbiological attributes mainly related to the amount of litter in each biome studied. For the disturbed areas, there were similar results between pastures and native areas, significantly different from the results obtained in agricultural areas, which due to differences in management and kind of cultures analyzed showed a great variability in its final result. The results support the recommendation for use of microbiological attributes as indicators of land use change, combined with chemical and physical factors. The substrate-induced respiration (or catabolic diversity) was efficient in the separation of land uses and ecoregions. These findings support the idea that specific land uses have specific groups of microbial biomass, regardless soil type, climate or other external influences.

Os radionuclídeos naturais das séries radioativas do 238U e do 232Th têm sido aplicados com sucesso como traçadores de processos ambientais atuais e mudanças climáticas. O 210Pb (meia-vida de 22,2 anos) é empregado na técnica de datação geocronológica de testemunhos sedimentares dos últimos 100-150 anos e na determinação de taxa de sedimentação. As concentrações dos isótopos 226Ra e 228Ra (meia-vida de 1.600 anos e 5,75 anos, respectivamente) auxiliam no cálculo das atividades de 210Pb em excesso no sedimento e auxiliam na identificação de processos marinhos importantes, como, por exemplo, a intrusão de água subterrânea. Neste trabalho foram quantificadas as concentrações de atividade de 226Ra, 228Ra e 210Pb em quatro testemunhos marinhos curtos coletados desde a plataforma continental até o talude superior do Atlântico Sudoeste. A partir dos resultados obtidos, as taxas de sedimentação em cada local e as idades de cada fatia de sedimento foram determinadas pelo método de datação geocronológica com 210Pb. As amostras sedimentares sofreram digestão total ácida em microondas. A separação radioquímica sequencial de 226Ra, 228Ra e 210Pb foi realizada com a obtenção dos precipitados de Ba(Ra)SO4 e PbCrO4. As medidas &alpha; total do 226Ra e &beta; total do 228Ra e do 210Pb a partir dos precipitados foram feitas em um detector proporcional de fluxo gasoso de baixa radiação de fundo. Com relação aos testemunhos analisados, as concentrações de atividade dos radionuclídeos variaram de 14 Bq.kg-1 a 154 Bq.kg-1 para o 226Ra; de 17 Bq.kg-1 a 45 Bq.kg-1 para o 228Ra; de 20 Bq.kg-1 a 2.073 Bq.kg-1 para o 210Pb. Valores altos de 210Pb foram encontrados no topo de todos os perfis sedimentares, proveniente principalmente da deposição atmosférica. Os dados coletados neste trabalho estão na mesma faixa de grandeza de outros relacionados a medições de 226Ra, 228Ra, 210Pb em áreas não contaminadas do Oceano Atlântico Sudoeste. As taxas de sedimentação diminuíram com o aumento da profundidade de coluna dágua, cujos valores variaram de 0,049 cm.ano-1 a 0,40 cm.ano-1. / Natural radionuclides from 238U and 232Th series have been successfully applied as tracers of environmental process and climate changes. The 210Pb (half-life of 22.2 years) is used in the geochronological dating technique of sediment cores of the last 100-150 years, and its respective sedimentation rate determination. The study of 226Ra and 228Ra concentrations (half-lives of 1,600 years and 5.75 years, respectively) helps calculate the activity of 210Pb in excess in the environment, besides being important tracers of marine processes, as ground water discharge. In this work it was determined the activity concentrations of 226Ra, 228Ra and 210Pb in four short marine cores collected since the continental platform to upper slope of Southwest Atlantic Ocean. Taking into account the results obtained, sedimentation rates and the ages of each sediment layer were determined using the geochronological dating method with 210Pb. All sediment samples were total acid digested in microwave. The sequential radiochemical separation of 226Ra, 228Ra, 210Pb were performed, obtaining in the end the precipitation of Ba(Ra)SO4 and PbCrO4. The gross &alpha; measurements of 226Ra and gross &beta; measurements of 228Ra and 210Pb from the precipitates were carried out in a gas-flow low background proportional counter. Concerning all cores analyzed, the activities concentrations of 226Ra ranged from 14 Bq.kg-1 to 154 Bq.kg-1; the concentrations of 228Ra ranged from 17 Bq.kg-1 to 45 Bq.kg-1; and the concentrations of 210Pb ranged from 20 Bq.kg-1 to 2,073 Bq.kg-1. High values of 210Pb were observed on the top of all the cores studied, mainly related to atmospheric deposition. The results obtained in this work were of the same order of magnitude of those reported in the literature available on non contaminated areas of Southeast Brazilian Coast. Sedimentation rates fall with the increase of water column depth and ranged from 0,049 cm.ano-1 to 0.40 cm.y-1.