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Diversity and effect of the microbial community of aging horse manure on stable fly (Stomoxys calcitrans) fitnessAlbuquerque, Thais Aguiar De January 1900 (has links)
Doctor of Philosophy / Department of Entomology / Ludek Zurek / Stable flies (Stomoxys calcitrans L.) are blood-feeding insects with a great negative impact on livestock resulting in annual losses around $2 billion in the USA alone. One of the main reasons for such an impact is because stable fly management is very difficult. Stable fly larvae develop primarily in animal manure and live bacteria were shown to be essential for stable fly development. I hypothesized that the microbial community of horse manure changes over time and plays an important role in stable fly fitness. Two-choice bioassays were conducted using 2 week old horse manure (control) and aging horse manure (fresh to 5 week old) to evaluate the effect of manure age on stable fly oviposition. The results showed that fresh manure did not stimulate oviposition and that the attractiveness increased as manure aged but started to decline after 3 weeks. Stable fly eggs artificially placed on 1, 2, and 3 week old manure resulted in significantly higher survival and heavier adults comparing to those developing in fresh, 4, and 5 week old manure. Analysis of the bacterial community of aging horse manure by 454-pyrosequencing of 16S rDNA revealed a major shift from strict anaerobes (e.g. Clostridium, Eubacterium, Prevotella, Bacteroidales) in fresh manure to facultative anaerobes and strict aerobes (e.g. Rhizobium, Devosia, Brevundimonas, Sphingopyxis, Comamonas, Pseudomonas) in 1-5 week old manure. Identified volatile compounds emitted from 2 and 3 week old horse manure included phenol, indole, p-cresol, and m-cresol. However, none of them stimulated stable fly oviposition in two-choice assays. In conclusion, the microbial community of 2 and 3 week old horse manure stimulates stable fly oviposition and provides a suitable habitat for stable fly development. Manure at this stage should be the main target for disrupting the stable fly life cycle. Volatile compounds acting as oviposition stimulants/attractants and their specific bacterial origin remain to be determined. Better understanding of stable fly microbial ecology is critical for development of novel management strategies based on alteration of the microbial community of stable fly habitat to generate a substrate that is non-conducive to fly oviposition and/or larval development.
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Stable tearing characterization of three materials with three methodsJohnston, Elizabeth Nicole January 1900 (has links)
Master of Science / Department of Mechanical and Nuclear Engineering / Kevin Lease / Over the past several years the crack tip opening angle (CTOA) has been identified as one of the key fracture parameters to characterize low constraint stable tearing and instability in structural metallic alloys. This document presents the results of experimental stable tearing characterizations. Characterization methods include optical microscopy and marker band measurements of crack front tunneling. Specific attention is given to the measurement methods used, and also the correlation between CTOA and Delta-5. The effect of tunneling and comparisons with computational results are discussed, and the effect of material and measurement method on CTOA is observed and a clear relationship is seen. Preliminary work on future studies into internal features and behavior is also presented.
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Grid stabilization for the one-dimensional advection equation using biased finite differnces of odd orders and orders higher than twenty-twoWhitley, Michael Aaron January 1900 (has links)
Master of Science / Department of Mathematics / Nathan Albin / This work utilizes finite differences to approximate the first derivative of non-periodic smooth functions. Math literature indicates that stabilizing Partial Differential Equation solvers based on high order finite difference approximations of spatial derivatives of a non-periodic function becomes problematic near a boundary. Hagstrom and Hagstrom have discovered a method of introducing additional grid points near a boundary, which has proven to be effective in stabilizing Partial Differential Equation solvers. Hagstrom and Hagstrom demonstrated their method for the case of the one-dimensional advection equation using spatial derivative approximations of even orders up to twenty-second order. In this dissertation, we explore the efficacy of the Hagstrom and Hagstrom method for the same Partial Differential Equation with spatial derivative approximations of odd orders and orders higher than twenty-two and report the number and locations of additional grid points required for stability in each case.
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Synthesis, Activation and Catalytic Activity of N-Heterocyclic Carbene Bearing Palladium CatalystsNavarro-Fernandez, Oscar 20 January 2006 (has links)
The syntheses and characterization of a series of (NHC)Pd(II) complexes (NHC = N-heterocyclic carbene) are described. A variety of architectures and precursors have been employed to lead to numerous air- and moisture-stable complexes. The use of those complexes as pre-catalysts in cross-coupling (Suzuki- Miyaura, Buchwald-Hartwig) and related (catalytic dehalogenation, £-ketone arylation) reactions is also discussed. A comparison of the activity of a variety of (NHC)Pd complexes as pre-catalysts for cross-coupling reactions was carried out. The results indicate that the activation of those pre-catalysts, leading to the catalytically active [(NHC)Pd(0)] species, was key in assuring high catalytic performance under mild reaction conditions. For the first series of complexes described, (NHC)Pd(allyl)Cl complexes, a better understanding of the process leading to the catalytically active species has permitted us to introduce simple modifications (alkyl or aryl groups at the allyl moiety) that dramatically alter the performance of the complexes by facilitating their activation, decreasing reaction times, catalyst loadings and even allowing reactions to be conducted at room temperature. Catalyst loadings as low as 0.05 mol% can be used for the Suzuki-Miyaura crosscoupling of aryl chlorides and aryl boronic acids at room temperature, leading to the synthesis of poly-ortho-substituted biaryls in excellent yields. This catalyst loading is the lowest ever used for this purpose. The system also allows for the first examples of coupling between aryl chlorides and alkenyl boronic acids at room temperature. When the temperature is raised to 80 ¢ XC for these reactions, a catalyst loading as low as 50 ppm can be used to effectively carry out Suzuki-Miyaura cross-couplings in remarkably short reaction times. As an added advantage, these complexes are air- and moisture-stable and can be prepared in a facile one-pot, multigram scale synthesis from commercially available starting materials in very high yields. The second series of complexes described revolves around the (NHC)Pd(acac)n framework. These complexes are also air- and moisture-stable and can be prepared in a one-step synthesis in high yields from commercially available materials. These complexes were tested forƒn £-ketone arylation and Buchwald-Hartwig amination reactions affording high yields of the desired products, in short reaction times and mild reaction conditions.
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Stable isotope analyses of African grey parrots: a forensic isotope approachAlexander, Jarryd January 2016 (has links)
A dissertation submitted to the Faculty of Science, University of the Witwatersrand, Johannesburg, in fulfilment of requirements for the degree of Master of Science. Johannesburg, 2016. / Stable isotope analyses have been used to infer diets of organisms, define trophic partitioning, and infer geographic origins of species. It has further been applied to forensic ecology to infer the origins of deceased humans and illegally traded animal (elephant ivory and rhinoceros horn) and plant (cycads, coca, and cannabis) material. However, no research has focused on the isotope analysis of avian material in forensic ecology. African grey parrots Psittacus erithacus are one of the most traded species in the world, with the trade often being illegal, and the origins of confiscated or deceased specimens being unknown. The aim of this study was to determine if stable isotopes (δ 13C, δ 15N, and δ 2H) in African grey parrot feathers could be used to determine the wild or captive origins of birds. African grey parrot feathers (primary, body, and tail) differed isotopically so standardising isotope values of African grey parrot feathers to a single feather type was recommended, to maintain consistent sampling and allow for comparisons to be drawn between different feather types. African grey parrot feathers from unknown origins can be identified as wild or captive using δ 13C and δ 2H values, but not δ 15N values. Known wild and captive feathers possibly differ isotopically from one another because of dietary and location differences. Wild African grey parrots inhabit and feed in isotopically depleted C3 forests compared to captive African grey parrots which are usually fed C4 based foods with more positive isotope values. Wild African grey parrot δ 2H isotope values were the most negative in the central region of their native distribution. The ability to differentiate wild from captive African grey parrots, as well as infer basic origins (East from West Africa) may improve the monitoring of the illegal trade as well as help in tracing illegally traded parrots. / LG2017
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Evolução sedimentar holocênica do delta do rio Tubarão, Estado de Santa Catarina / Holocene sedimentary evolution of the Tubarão river delta, Santa Catarina State (Brazil)Nascimento Junior, Daniel Rodrigues do 11 February 2011 (has links)
O delta do rio Tubarão, situado na costa centro-sul catarinense entre os municípios de Tubarão, Jaguaruna e Laguna, constitui raro exemplo de delta lagunar ativo no Brasil. Sua planície deltaica cobre área aproximada de 250km2, onde são encontradas evidências de migração de canais fluviais dadas por séries de truncamentos de antigos distributários, alguns ainda ativos. Dez testemunhos foram obtidos junto aos principais canais distributários do rio Tubarão, a partir dos quais foram realizadas análises de fácies, granulométrica, de minerais pesados, de teor de matéria orgânica e de relações químio-isotópicas, além de datações 14C. Também foram levantados acervos históricos de fotografias aéreas e de dados de prospecção mineral de subsuperfície. Cerca de 5000 anos atrás, na região de seu ápice, próximo ao rio tributário Capivari de Baixo, o delta do rio Tubarão ingressou numa antiga baía lagunar e ramificou-se em sete distributários principais que, desde seus momentos iniciais de migração, foram controlados por avulsões autogênicas rumo a antigas depressões do fundo da bacia receptora. Tais avulsões progradaram o delta inicialmente para SW, depois para ENE, e então para NNE, favorecendo a fragmentação da antiga baía lagunar em uma série de lagos e lagunas menores. Diante deste cenário dinâmico, sambaquis foram erigidos no entorno do sistema lagunar, constituindo importantes registros arqueológicos de interação entre evolução sedimentar e ocupação humana pré-histórica. O resultado das análises granulométricas indicou que a sedimentação deltaica, nas proximidades de encostas de morros, foi misturada com colúvio e/ou depósitos de fluxos gravitacionais, como evidenciado pela presença de intervalos texturalmente muito imaturos em alguns testemunhos. Em relação à análise de minerais pesados, o principal fator de controle nas variações da assembleia em depósitos de delta e de bacia é a proveniência sedimentar. Em termos mediatos, essa proveniência reflete fontes plutônicas e metamórficas (médio a alto grau) do Batólito de Florianópolis (e xenólitos associados) e do Complexo Granito-Gnáissico, e rochas arenáceas alteradas da Bacia do Paraná. Em termos imediatos, depósitos deltaicos destacam-se pela afinidade mineralógica com as areias do rio Tubarão, inferida sobretudo a partir da presença mútua de grãos alterados de cianita e estaurolita, enquanto que depósitos da bacia lagunar destacam-se por sua similaridade mineralógica com areias dos rios tributários Braço do Norte e Capivari de Baixo, neste caso principalmente pela presença de zircão. A matéria orgânica presente nos depósitos do delta e de sua bacia receptora resulta do aporte de fontes terrestres (fornecido pelos rios) e marinhas (trazido via desembocaduras lagunares), fato que é evidenciado pelos resultados de \'delta\'\'POT.13 C\', \'delta\'\'POT.15 N\' e razão \'C IND.ORG\'/\'N IND.TOTAL\'. Particularmente, nos sedimentos da bacia, variações entre diferentes tipos de matéria orgânica têm ocorrido ao longo do Holoceno, as quais são atribuídas tanto ao isolamento físico progressivo do sistema lagunar em relação ao mar aberto como por mudança climática regional (aumento destacado de precipitação). A análise isotópica de oxigênio (\'delta\'\'POT 18 O\') de conchas de moluscos em depósitos da bacia indicou enriquecimento relativo em \'ANTPOT.16 O\' durante o Holoceno. Este resultado, a exemplo daquele dos isótopos de carbono e de nitrogênio dos sedimentos, sugere isolamento gradual das águas lagunares em relação às de mar aberto. / The Tubarão river delta, located on the centre-south coast of Santa Catarina State, among the municipalities of Tubarão, Jaguaruna and Laguna, is rare example of active lagoonal delta in Brazil. Its delta plain covers an area of about 250km2, where there are evidences of migration of fluvial channels in a set of truncations of ancient distributaries, some of these still in activity. Ten cores were acquired adjacent to the main distributary channels of the Tubarão river, from which analyses of facies, grain size, heavy minerals, organic matter, chemistry-isotope ratios, and radiocarbon datings were performed. Also, aerial photographies and data of subsurface mining were surveyed from historical collections. Thereabout 5,000 years ago, in the region of its apex, near Capivari de Baixo tributary river, the Tubarão river delta entered an ancient lagoonal bay and branched seven main distributaries. Since the beginning of its migration, these distributaries were controlled by autogenic avulsions towards ancient depressions in the bottom of the basin. Initially, these avulsions prograded the delta towards SW, afterwards to ENE, and then to NNE, favoring the fragmentation of the ancient lagoonal bay in a set of smaller lakes and lagoons. Faced with this dynamical scenario, shellmounds were erected surrounding the lagoon system, composing important archaeological records of the interaction between sedimentary evolution and prehistoric human occupation. The results of the grain size analysis showed that the deltaic sedimentation, in the vicinity of slopes of hills, was mixed with colluvium and/or gravity flow deposits, that is evidenced by the presence of texturally very immature intervals in some cores. The analysis of heavy minerals, by its turn, showed that the main controlling factor in the variations of its assemblage in deposits of delta and basin is the sedimentary provenance. In terms of mediate sources, this provenance reflects plutonic and metamorphic (medium to high grade) rocks of the Florianópolis batholith (including its xenoliths) and of the Granite-Gneiss Complex, and weathered sedimentary sandstones of the Palaeozoic Paraná basin. Regarding immediate sources, deltaic deposits stand out by its mineralogical affinity with sands of the Tubarão river, mainly by the mutual presence of weathered grains of kyanite and staurolite, whereas deposits of the lagoon have mineralogical similarity with the sands of Braço do Norte and Capivari de Baixo tributary rivers, especially in relation to the presence of zircon. The origin of the organic matter found in the deposits of the delta and in its lagoonal basin is both from sedimentary input of terrestrial sources (provided by rivers) and marine (brought via inlets), fact evidenced by results of \'delta\'\'POT.13 C\', \'delta\'\' POT.15 N\', and \'C IND.ORG\'/\'N IND. TOTAL\' ratio. Particularly, in the sediments of the basin, variations between different types of organic matter have occurred during the Holocene, and are attributed both to the progressive physical isolament of the lagoon system from the open sea, and by local climate change (pronounced augment of precipitation). The isotope analyses of oxygen (\'delta\'\'POT.18 O\') of molluskan shells from the deposits of the basin present relative enrichment in \'ANTPOT.16 O\' during the Holocene. This result, as well as the one from isotope analyses of carbon and nitrogen of sediments, suggests gradual isolation of the lagoonal waters of influence of waters from the open sea.
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A 2,205-year record of tropical cyclone strikes near Yucatán, Mexico, from mud layers in a stalagmitePyburn, James January 2010 (has links)
Thesis advisor: Amy Frappier / Tropical cyclones (TCs), known as hurricanes in the Atlantic and Typhoons in the Pacific, are among the most destructive and deadly natural disasters that occur on Earth. Attempts to understand how TCs relate to the global climate system, and future risk assessments are dependent upon having records of TC activity that pre-date the modern meteorological records, which are commonly not older than 130 years (Nott, 2003). Paleotempestology is a sub-discipline of paleoclimatology that attempts to extend the TC record beyond the meteorological record through the use of proxies. Presented here is the establishment of a paleotempestology proxy based on clastic mud being suspended in the water column by floods caused by TCs and deposited in stalagmite CH-1, collected in June of 2007 from Cenote Chaltun-Ha, a low-lying cave from the Yucatán Peninsula. CH-1 was dated by a combination of <super>210</super>Pb, U/Th, and layer counting techniques, creating an age model for its entire length. The years with mud layers were compared to the historical TC record from 1852-2006. Nineteen mud layers were identified for this time period. All of the mud layers deposited in years with at least one TC passing within 330 km of Cenote Chaltun-Ha. A total of 265 mud layers were identified in CH-1 dating from 198 BC to 2006 AD. Relatively high TC frequency, ~16 mud layers/century, was recorded in CH-1 from 198 BC to ~1233 AD. This period was followed by eight centuries of relatively low TC frequency, ~7 mud layers/century. The low frequency period hit a low point in the 1600s with 4 mud layers. Since the 1600s the TC frequency recorded in CH-1 has been on the rise, indicating possible periods of higher than present TC frequency in the future for the Yucatán region. This trend of high TC frequency followed by a sudden drop and subsequent increase is also reported in published sand overwash deposit research. δ;<super>18</super>O and δ;<super>13</super> values collected from CH-1 provide insight into the timing of regional droughts. A low δ;<super>18</super>O value from 1815 provides evidence that "The Year Without a Summer" caused by the 1815 eruption of the Tambora volcano in Indonesia had a climatic effect on the Yucatán. A land-use signal related to the agricultural production boom of Agave Fourcroydes, a succulent plant known as Henequen, in the early 20th century was also detected in δ;<super>13</super>C values. / Thesis (MS) — Boston College, 2010. / Submitted to: Boston College. Graduate School of Arts and Sciences. / Discipline: Geology and Geophysics.
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Estimativa da taxa de turnover e fator de discriminação isotópico em espécies de quelônios / Estimation of turnover rate and discrimination factor in species of cheloniansConsolmagno, Luiza Camargo 03 July 2018 (has links)
A utilização de traçadores como os isótopos estáveis de carbono e nitrogênio, é crescente e complementa as técnicas convencionais nos estudos referentes à dieta em animais silvestres. Isso é possível pois o valor isotópico dos itens utilizados na alimentação é refletido nos tecidos. A diferença isotópica resultante chamada de fator de discriminação ou fracionamento, está associada aos processos metabólicos necessários para que ocorra a incorporação de nutrientes. O estudo teve como objetivo medir o tempo de incorporação dos isótopos no plasma e nas células sanguíneas, componentes de \"tecido\" não mortal reamostrável, e determinar o fator de discriminação em cinco espécies de quelônios de água doce: Podocnemis expansa (tartaruga-da-Amazônia), Podocnemis unifilis (tracajá), Phrynops geofroanus (cágado-de-barbicha), Trachemys scripta (tartaruga-de-orelha-vermelha) e Trachemys dorbigni (tigre-d\'água). Os animais foram mantidos em cativeiro e as diferenças isotópicas dos 10 indivíduos adultos de cada espécie, foram medidas a partir da troca de dietas com valores isotópicos distintos. Com a mudança da dieta, o turnover do carbono e nitrogênio foram estimados entre 7 e 185 dias por meio de regressão exponencial não linear, quando os novos fatores de fracionamento foram estimados. O tempo de turnover para as espécies de quelônios variou de 72 a 337 dias para o carbono, e de 29 a 270 dias para o nitrogênio no plasma. Nas células sanguíneas o turnover variou de 3 a 373 dias para o carbono, e de 51 a 216 dias para o nitrogênio. Os fatores de discriminação que eram em média próximos a zero para o carbono, e entre 3-4‰ para o nitrogênio, variaram de 1,01 a 3,28‰ para o 13C e -0,76 a 0,49‰ para o 15N no plasma, e de 1,49 a 3,98‰ para o 13C e 0,99‰ a 4,69 para o 15N nas células sanguíneas, com a diminuição de 3,7‰ e aumento de 6,2‰, respectivamente para carbono e nitrogênio, na nova dieta. A diferença encontrada entre os fatores de discriminação calculados anteriormente a troca da dieta e após a troca, mostraram que provavelmente a incorporação dos isótopos estáveis se dá de forma heterogênea nos tecidos. De acordo com a literatura foi possível analisar que fatores como a memória isotópica, as rotas metabólicas e elementos característicos dos répteis possivelmente estão ligados ao turnover mais lento, diferente dos animais endotérmicos em que esse processo é mais rápido. / The use of tracers such as stable carbon and nitrogen isotopes is crescent and complements the conventional techniques used in the studies referring to the diet in wild animals. This is possible because the isotopic value of the items used in the diet reflects their isotopic values on the tissues. The resulting isotopic difference called the discrimination factor or fractionation is associated with the metabolic processes required for nutrient incorporation to occur. The object of the study was to measure the incorporation time of isotopes into plasma and blood cells, components of re-portable non-lethal \"tissue\", and to determine the discriminant factor of five species of freshwater chelonians: Podocnemis expansa (Amazonia tortoise), Podocnemis unifilis (tracajá), Phrynops geofroanus (geoffroy´s side necked turtle), Trachemys scripta (red-eared slider turtle) and Trachemys dorbigni (d\'orbigny\'s slider). The isotopic differences of 10 adult individuals of each species kept in captivity were measured through shifting diets with different isotopic values. With the diet variation, carbon and nitrogen turnover was estimated between 7 and 185 days by non-linear exponential regression, when the new fractionation factors were estimated. The turnover time for the chelonians species varied from 72 to 337 days for carbon, and from 29 to 270 days for the plasma nitrogen. In blood cells, the turnover ranged from 3 to 373 days for carbon, and from 51 to 216 days for nitrogen. Discrimination factors that were, in average, close to zero for carbon and between 3 and 4‰ for nitrogen ranged from 1.01 to 3.28‰ for 13C and -0.76 to 0.49‰ for 15N in plasma, and from 1.49 to 3.98‰ for 13C and 0.99 to 4.69 for 15N in blood cells, with a decrease of 3.7‰ and an increase of 6.2‰, respectively for carbon and nitrogen in the new diet. The difference found between the discrimination factors calculated before and after the diet shift, showed that stable isotopes incorporation probably occurs in a heterogenous way in tissues. According to the literature it was possible to analyze that factors such as isotopic memory, metabolic routes and reptiles characteristic elements are possibly linked to slower turnover, different from endothermic animals in which this process is faster.
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The development and use of stable isotope analysis of felids’ whiskers as a tool to study their feeding ecologyMutirwara, Ruwimbo January 2017 (has links)
Thesis (MTech (Nature Conservation))--Cape Peninsula University of Technology, 2017. / Stable isotope analysis (SIA) of whiskers has been used to identify temporal feeding habits, intra-population diet variation, as well as individual dietary specialisation of marine and terrestrial carnivores. However, the potential of the method to disclose such dietary information for large wild felids has been little explored. The accurate interpretation of stable isotope ratios along serially sampled whiskers is hampered by lack of information on species-specific whisker growth rates, whisker growth patterns and whisker-diet trophic discrimination factors (TDFs). Whisker growth rate and growth pattern informs on the time period encapsulated in the analysed segment of a whisker, while whisker-diet TDFs are required to make correct deductions of the prey species consumed by a predator. The aim of this study was to develop and evaluate the technique of using stable carbon and nitrogen isotope analysis of felid whiskers to quantify the diet of wild felids and in particular, to identify diet variation among individuals. To achieve this, lion Panthera leo and leopard Panthera pardus whisker growth rate and growth pattern, and lion whisker-diet TDFs were measured, using captive individuals held at the National Zoological Gardens, Pretoria. The viability and applicability of the technique was then explored on six free-ranging leopards in Phinda Private Game Reserve (hereafter Phinda), northern KwaZulu-Natal (KZN) whose diets have been intensively studied using traditional methods.
Whisker growth rates and growth patterns were measured for four lions (three sub-adult females and one adult male) and an adult male leopard over 185 days using giraffe Giraffa camelopardalis meat as an endogenous biomarker to consecutively mark whiskers as they grew. The 13C-depleted, C3-derived giraffe meat with its characteristic isotopic signature could be discerned from the 13C-enriched diet of C4 grain-fed beef and chicken the felids were sustained on. Two whiskers were removed from each felid at the beginning of the experiment, and felids were fed the giraffe meat at four predetermined periods to mark the whiskers replacing the removed ones. The periods with low δ13C values, identified following serial sectioning of the regrown whiskers at 1 mm intervals (and stable isotope analysis of these sections), were then correlated to specific giraffe meat feeding bouts and hence growth periods. Knowledge of the duration between giraffe meat feeding bouts enabled the calculation of whisker growth rate and determination of growth pattern. δ13C and δ15N whisker-diet TDFs were estimated for five lions whose diet remained consistent over multiple years. Whiskers removed from four lions at the beginning of the whisker growth experiment, a whisker removed from a female lion as part of a pilot study a year before the experiment and the diet (chicken and beef) samples collected during the experiment were analysed for their isotopic ratios. These were used to calculate isotopic differences between lion whiskers and diet.
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Isotopic evidence of Bronze Age diet and subsistence practices in the southeastern Carpathian Bend area, RomaniaAguraiuja, Ülle January 2017 (has links)
Human and faunal osteological material from the southeastern Carpathian Bend area, Romania, was analysed for δ13C, δ15N and δ34S to reconstruct the dietary practices of the Middle Bronze Age Monteoru culture. As a secondary objective, the extent of intraskeletal variation in stable isotope values was investigated by comparing skeletal elements with differing collagen turnover rates. The intraskeletal isotope results revealed a pattern where cortical bone samples produced statistically lower δ13C values compared to trabecular bone samples, highlighting the necessity for more systematic research to understand how stable isotopes are incorporated into bone collagen of various skeletal elements. Diet in the Monteoru culture was shown to be exclusively or predominantly terrestrial in origin with no detectable input of C4 or marine resources. Differences in average δ13C and δ15N values between the two sites included in the study (representing distinct phases of the culture) suggest a shift in dietary preferences from a more meat-based economy to a more dairy- and plant-based economy. The dissimilar contribution of animal foods to overall diet between the two sites was supported by estimates generated by the Bayesian mixing model FRUITS, which also showed that in both sites plant foods accounted for most of the calories consumed. The faunal isotopic data contained a few outliers, suggestive of deliberate movement of livestock, either through long-distance herding or trade. A combined approach using juvenile bone collagen and incrementally sectioned tooth dentine from adults demonstrates that the duration of breastfeeding varied between individuals, but that there were no significant differences in weaning practices between survivors and non-survivors. Sulphur isotopes reflect a population that was relatively homogeneous in its isotopic composition and local in origin, except for the presence of two possible migrants. The δ13C and δ15N data from the Carpathian Bend are comparable to those from contemporaneous sites in coastal and inland Greece and Croatia, suggesting a broad uniformity in Bronze Age dietary practices across Southeast Europe. As the first major stable isotope study conducted on osteological material from the Romanian Sub- Carpathians, this thesis provides new insights into the lives of these communities, expands our knowledge of Bronze Age subsistence strategies in Southeast Europe, and establishes a foundation for further isotopic investigations in the region.
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