Call number: LD2668 .T4 1985 D59 / Master of Science

Call number: LD2668 .T4 1985 K87 / Master of Science / Agronomy

Call number: LD2668 .T4 1986 H534 / Master of Science / Horticulture, Forestry, and Recreation Resources

Orientador: Carmen Regina Marcati / Coorientador: Fabio Bosio / Banca: Elizabeth Orika Ono / Banca: Clivia Carolina Forilo Possobom / Resumo:No cerrado, as estações são bem demarcadas pela sazonalidade pluvial, portanto, espera-se que haja uma sazonalidade na atividade do câmbio vascular. Kielmeyera grandiflora é considerada uma espécie modelo para estudos de atividade cambial em ramos, pois possui módulos de crescimento bem demarcados, formados por cicatrizes da gema terminal. Nosso objetivo foi de entender qual a relação entre a atividade cambial de Kielmeyera grandiflora (Wawra) Saddi (Calophyllaceae), os fatores ambientais e a fenologia e responder se a atividade cambial varia entre três módulos de crescimentos consecutivos. A área de estudo é um fragmento de cerrado em regeneração no município de Botucatu, estado de São Paulo, Brasil (S 22º53'11.0', W 48º29'17.3'). Foram amostrados mensalmente os três últimos módulos de crescimento dos ramos de três indivíduos durante o período de fevereiro de 2012 a fevereiro de 2013. No mesmo período, a fenologia (brotação, folhas novas, folhas adultas, folhas senescentes e queda foliar) foram avaliadas. O material foi fixado em CRAF III para conservação do conteúdo celular. As amostras foram desidratadas em série alcoólica e incluídas em resina metacrilato para posterior corte em micrótomo rotativo. As análises foram feitas em fotomicroscópio de luz. Utilizamos Modelo Generalizado Linear Misto (GLMM) com erro Binomial para a variável resposta presença/ausência da atividade cambial e erro de Poisson para a variável resposta de contagem de paredes recém formadas. O início da atividade cambial, a brotação e o desenvolvimento de folhas novas ocorreram durante o mês de agosto no período seco. O período de atividade cambial sobrepôs-se à estação chuvosa, temperaturas elevadas e comprimento do dia entre 12 e 13,6 h. O câmbio vascular entrou em dormência em maio, mês que ainda chovia, contudo a temperatura e o comprimento do dia passavam ... / Abstract: In the cerrado, the seasons are well marked by rain seasonality; therefore, there is a seasonality in the vascular cambium activity. Kielmeyera grandiflora is considered a model for branch cambial activity studies because it has well marked growth modules formed by terminal bud scars. Our goal was to understand what the relationship between cambial activity of Kielmeyera grandiflora (Wawra) Saddi (Calophyllaceae), environmental factors and the phenology and answear wheter cambial activity varies between three consecutive sections of internodal growth. The study area is a cerrado fragment in regeneration in the city of Botucatu, São Paulo State, Brazil (22° 53 ' S 11.0 ', W 48° 29 ' 17.3 '). Were sampled on a monthly basis the last three modules of growth of branches of three individuals during the period between February 2012 to February 2013. The material was fixed in CRAF III for preservation of cell content. The samples were dehydrated in alcohol series and included in historesin for further cut in rotary microtome. Analyses were made on light microscope. We used Generalized Linear Mixed Model (GLMM) with Binomial error for the variable reply presence/absence of cambial activity and Poisson error for the variable count response of newly formed walls. The beginning of cambial activity, the sprouting and the development of new leaves occurred during the month of August in the dry period. The period of cambial activity overlapped the rainy season, high temperatures and day length between 12 and 13, 6 h. The vascular cambium dormancy was observed in May, a raining month; however, temperature and day length was decreasing. The variation of cambial activity between the internodal growth sections was representative just in reactivation period, showing that the younger internodal section, closest to the sources of auxin, has produced in the whole study period a larger number of new cells that ... / Mestre

Predicting how increasing atmospheric carbon dioxide concentration will affect the hydrologic cycle is of utmost importance for water resource management, ecological systems and for human life and activities. A typical perspective is that the water cycle will mostly be altered by atmospheric effects of climate change, precipitation and radiation, and that the land surface will adjust accordingly. Terrestrial processes can however feedback significantly on the hydrologic changes themselves. Vegetation is indeed at the center of the carbon, water and energy nexus. This work investigates the processes, the timing and the geography of these feedbacks. Using Earth System Models simulations from the Coupled Model Intercomparison Project, Phase 5 (CMIP5), with decoupled surface (vegetation physiology) and atmospheric (radiative) responses to increased atmospheric carbon dioxide concentration, we first evaluate the individual contribution of precipitation, radiation and physiological forcings for several key hydrological variables. Over the largest fraction of the globe the physiological response indeed not only impacts, but also dominates the change in the continental hydrologic cycle compared to either radiative or precipitation changes due to increased atmospheric carbon dioxide concentration. It is however complicated to draw any conclusion for the soil moisture as it exhibits a particularly nonlinear response. The physiological feedbacks are especially important for extreme temperature events. The 2003 European heat wave is an interesting and crucial case study, as extreme heat waves are anticipated to become more frequent and more severe with increasing atmospheric carbon dioxide concentration. The soil moisture and land-atmosphere feedbacks were responsible for the severity of this episode unique for this region. Instead of focusing on statistical change, we use the framework of Regional Climate Modeling to simulate this specific event under higher levels of surface atmospheric carbon dioxide concentration and to assess how this heat wave could be altered by land-atmosphere interactions in the future. Increased atmospheric carbon dioxide concentration modifies the seasonality of the water cycle through stomatal regulation and increased leaf area. As a result, the water saved during the growing season through higher water use efficiency mitigates summer dryness and the heat wave impact. Land-atmosphere interactions and carbon dioxide fertilization together synergistically contribute to increased summer transpiration if rainfall does not change. This, in turn, alters the surface energy budget and decreases sensible heat flux, mitigating air temperature rise during extreme heat periods. This soil moisture feedback, which is mediated and enabled by the vegetation on a seasonal scale is a European example of the impacts the vegetation could have in an atmosphere enriched in carbon dioxide. We again use Earth System Models to systematically and statistically investigate the influence of the vegetation feedbacks on the global and regional changes of extreme temperatures. Physiological effects typically contribute to the increase of the annual daily maximum temperature with increasing atmospheric carbon dioxide concentration, accounting for around 15% of the full trend by the end of the XXIth Century. Except in Northern latitudes, the annual daily maximum temperature increases at a faster pace than the mean temperature, which is reinforced by vegetation feedbacks in Europe but reduced in North America. This work highlights the key role of vegetation in influencing future terrestrial hydrologic responses. Accurate representation of the response to higher atmospheric carbon dioxide concentration levels, and of the coupling between the carbon and water cycles are therefore critical to forecasting seasonal climate, water cycle dynamics and to enhance the accuracy of extreme event prediction under future climates in various regions of the globe.

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xxi, 299 leaves : ill. ; 25 cm / Title page, contents and abstract only. The complete thesis in print form is available from the University Library. / Thesis (Ph.D.1976) from the Dept. of Plant Physiology, University of Adelaide

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It is now well established that cold-triggered calcium influx mediates cold-induced gene expression and development of freezing tolerance (cold acclimation). In this thesis, cold signaling events both upstream and downstream of calcium influx were examined. / First, it was shown that the studies on calcium mediation of cold acclimation in alfalfa cell suspension cultures could be applied to intact seedlings of Arabidopsis. Calcium chelators and channel blockers caused a strong reduction in the cold-induced accumulation of kin1 and kin2 transcripts, suggesting that calcium influx was an essential event during cold signaling and that the source of calcium for this influx was largely the calcium-rich cell wall. Evidence suggesting the involvement of calcium-dependent protein kinases (CDPKs) was also obtained. / Second, the nature of events upstream of calcium influx was explored. For this study, transgenic Brassica napus seedlings possessing both the endogenous cold-inducible BN115 gene and the coding part of beta-glucuronidase (GUS) gene placed under the control of the BN115 promoter were used. Thus cold-activation of the BN115 promoter drove the expression of both BN115 at the transcriptional level and the GUS enzyme activity at the translational level. Cold-activation of BN115 was inhibited by chemicals which cause membrane fluidization, cytoskeletal stabilization and inhibition of Ca2+ influx, and mimicked at 25°C by chemicals causing membrane rigidification, cytoskeletal destabilization and Ca2+ influx. Inhibitors of protein and lipid kinases prevented cold-activation of BN115, but inhibition of protein phosphatases activated BN115 at 25°C. / Third, given the increasing importance of mitogen-activated protein kinases (MAPKs) in signal transduction, the nature of molecular mechanisms that lead to cold-activation of a previously reported MAPK, SAMK, was investigated. During this study, the first plant MAPK activated by heat shock was discovered and named HAMK (Heat-shock-activated MAPK). It was shown that cold-activation of SAMK is mediated by cold-induced membrane rigidification, whereas the heat shock-activation of HAMK occurs through heat shock-induced membrane fluidization. Whereas activation of both SAMK and HAMK is blocked by an actin microfilament stabilizer, it is mimicked at 25°C by chemical destabilizers of microtubules or actin microfilaments. All of these events are inhibited by blocking the influx of extracellular Ca 2+. Cold-activation of SAMK and heat-activation of HAMK was prevented by treatment of cells with inhibitors of CDPKs. Thus, cold and heat shock are sensed by structural changes in the plasma membrane, which transduces the signal via cytoskeletal rearrangements to the opening of calcium channels, leading to Ca2+ influx, activation of CDPKs and activation of distinct MAPK cascades.

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