O silício encontra-se no meio marinho nas formas: dissolvida e particulada (biogênica e litogênica). O ciclo biogeoquímico deste elemento está sujeito à influência sazonal e às alterações antrópicas. Este trabalho visa entender a relação entre as diferentes formas de silício como resposta a processos de origem natural e antrópica em diferentes ambientes (Estreito de Bransfield, Antártica; Complexo Estuarino-Lagunar de Cananeia-Iguape, SP; região costeira de Recife, PE). O Estreito de Bransfield pela sua localização remota é das áreas estudadas, a menos impactada pelo homem. A região nordeste do Estreito mostrou menores concentrações de silicato na superfície associadas à menor diversidade fitoplanctônica, constituída por diatomáceas do gênero Corethron que facilitam o afundamento de Si e a remineralização do C e N. Já na região sudoeste do Estreito a concentração de silicato foi maior, assim como a influência do degelo, que contribui para uma maior disponibilidade de ferro, indicada pelo traçador Si*, aumentando a diversidade fitoplanctônica. Nesta região também houve a presença de espécies que facilitam o afundamento de C e N e a remineralização de Si. O Complexo Estuarino-Lagunar de Cananeia-Iguape, apresentou sinais de impacto antrópico sobretudo no setor norte (Iguape), mostrado pelas diferentes frações do silício que foram excelentes indicadores de processos erosivos. No setor sul a influência antrópica não foi observada, assim o silício indicou processos de origem natural como a sedimentação, evidenciada pela remoção do BSi e do LSi, e a ressuspensão onde as concentrações das frações particuladas foi maior. A região costeira de Recife está sob a influência dos aportes fluviais provenientes dos rios Capibaribe e Beberibe. A distribuição da maioria dos parâmetros, incluindo o silicato e o BSi, mostraram esta influência vinda de oeste, atingindo a barreira na saída do porto e se propagando em direção a nordeste. Devido ao maior aporte de nutrientes nas estações mais próximas à costa a produção primária foi incentivada, evidenciada pelos maiores valores de clorofila-a e BSi. Nas estações mais distantes da costa os parâmetros tiveram valores característicos de áreas oligotróficas, com as frações de silício mostrando concentrações bastante baixas. O silício se mostrou um excelente indicador de aportes continentais naturais e antrópicos. São poucos os trabalhos que quantificam o BSi e o LSi no meio aquático, assim este estudo consiste em um ponto inicial para o entendimento do silício particulado em águas brasileiras. / Silicon is found in the marine environment under the forms: dissolved and particulate (biogenic and lithogenic). The biogeochemical cycle of this element is subject to seasonal influences and anthropogenic changes. This work aims to understand the relationship between different forms of silicon in response to processes of natural and anthropogenic origin in different environments (Bransfield Strait, Antarctica; Cananeia-Iguape Estuarine-Lagoon Complex, SP ; coastal region of Recife, PE) . The Bransfield Strait is, of the studied areas, the least impacted by man, because of its remote location. The northeastern Strait region showed lower silicate concentrations associated with lower phytoplankton diversity, consisting of diatoms of the genus Corethron that facilitate sinking af Si and remineralization of C and N. In the southwestern region of the Strait silicate concentration was higher, as well as the influence of thaw, which contributes to increased iron availability, indicated by Si* tracer, that increases phytoplankton diversity. In this region there was also the presence of species that facilitate the sinking of C and N and the remineralization of Si. Cananeia-Iguape Estuarine -Lagoon Complex, showed signs of anthropogenic impact especially in the northern sector (Iguape), showed by silicon different fractions, which were excellent indicators of erosion processes. In the southern sector, anthropogenic influence was not observed. Silicon indicated processes of natural origin, like sedimentation, evidenced by the removal of BSi and LSi, and resuspension where concentrations of particulate fractions was higher. The coastal region of Recife is under influence of fluvial inputs from Capibaribe and Beberibe rivers. The distribution of most parameters, including silicate and BSi, showed this influence coming from the west, reaching the barrier at the port exit and propagating toward northeast. Due to higher nutrient availability in the stations nearest to the coast, primary production was encouraged, evidenced by high values of chlorophyll-a and BSi. In the stations more distant to the coast, the parameters had values characteristic of oligotrophic areas , with the forms of silicon showing very low concentrations. Silicon proved to be an excellent indicator of continental natural and anthropogenic contributions. There are few studies that quantify the BSi and LSi in the aquatic environment, therefore this study is a starting point for understanding particulate silicon in Brazilian waters.

Muitos países possuem estações de pesquisa instaladas na Antártica. Hidrocarbonetos de petróleo e os esgotos lançados no mar pelas estações são as fontes potenciais de poluição na Antártica. Peixes da espécie Trematomus newnesi foram utilizados para investigar o potencial genotóxico e os efeitos sobre a morfologia de fígado e brânquias da água diante dos tanques de combustível e da saída de esgoto da Estação Antártica Brasileira ?Comandante Ferraz?, em experimentos in situ e no laboratório. No Ensaio de Mn e ANE, observou-se que a freqüência de R foi, em geral, menor nos controles do que nos grupos expostos, tanto nos bioensaios como nos experimentos in situ, porém não houve diferenças estatisticamente significativas em nenhum dos experimentos. As lesões branquiais mais observadas, nos grupos expostos, foram hipertrofia do epitélio e telangiectasia lamelar. No fígado, as lesões predominantes foram a vacuolização lipídica e a presença de macrófagos, principalmente nos peixes dos experimentos in situ. Não foram verificadas diferenças significativas nos índices de lesões histopatológicas entre os grupos expostos e os controles em nenhum dos experimentos. Contudo, os resultados obtidos sugerem que dos dois locais analisados nas proximidades da Estação Brasileira, a saída de esgoto apresenta maior potencial de risco para T. newnesi. / Many countries have installed research stations in Antarctica. Petroleum hydrocarbons and the sewage disposed into the sea by the stations are potential sources of pollution in Antarctica. Trematomus newnesi specimens were used to assess genotoxic potential and histopathology of the liver and gills of the water surrounding the Brazilian Antarctic Station ?Comandante Ferraz?. Fish were exposed to seawater at the sewage outfall and in front of the fuel tanks, in both in situ and laboratory assays. The Mn and ENA assay showed that the frequency of R was, in general, lower in the control groups than in the exposed ones in both in situ and laboratory assays, however there were no statistically significative differences in any of the experiments. The most frequent branchial lesions observed in the exposed groups were epithelium hipertrophy and lamelar telangiectasis. In the liver, predominant microscopic findings included lipid vacuolization and macrophages, specially in fish from the in situ experiments. Exposed groups did not show significative differences in the histopathological indexes from those of the controls in any of the experiments. Nevertheless, our results suggest that of the places studied the sewage outlet may present a greater potential of risk to T. newnesi nearby the Brazilian Station.

Este trabalho investiga a dinâmica de retração frontal de duas geleiras de maré, Drummond (66°40'S, 65°43'O) e Widdowson (66°43'S, 65°46'O), na costa ocidental da Península Antártica. O estudo usou fotografias aéreas e imagens satelitais LANDSAT (a partir de 1986) para determinar a variação de área dessas geleiras no período 1957–2015 e analisar a sensibilidade às recentes mudanças ambientais na Península Antártica. O modelo digital de elevação AsterGDEM2 foi usado para caracterizar a morfologia e morfometria da bacia de drenagem dessas massas de gelo. A análise estatística dos dados de temperatura média anual da Estação Vernadsky (65°14’ S, 64°15’ O) mostra tendência ao aquecimento atmosférico no período 1950–2015 (0,047°C ano-1) nesta parte da Península Antártica ocidental. As frentes das duas geleiras retraíram ao longo dos últimos 68 anos, no entanto a geleira Widdowson apresentou uma perda maior (36,03 km2, ou 16,81% da área original) e uma linha de neve mais elevada (200 m a.n.m. em 2016) do que a geleira Drummond (18,84 km2, ou 4,26% da área original; linha de neve a 100 m a.n.m. em 2016) no período. Essa diferença na retração da duas geleiras, lado a lado e com a mesma orientação de fluxo do gelo, são atribuídas as diferentes declividades da superfície e proporção da área de acumulação sobre a área total. A geleira de menor área, Widdowson, somente atingiu um ponto de estabilização (apoiada ao embasamento rochoso lateral) em 2001, enquanto a frente da Drummond estabilizou-se em 1974. Além disso, a geleira Widdowson é mais íngreme no setor frontal, o que pode ter influenciado na taxa de desprendimento de icebergs e gerado um deslizamento basal mais eficiente, aumentando a velocidade de fluxo do gelo e, por consequência, aumentando as taxas de retração. Esses resultados condizem com estudos para outras geleiras de descarga com frentes flutuantes na Península Antártica, as quais são mais sensíveis às mudanças climáticas. A dinâmica dessas geleiras também é influenciada por mudanças nas forçantes oceânicas, taxas de precipitação, derretimento superficial e morfologias diferentes do embasamento rochoso; esses pontos devem ser tratados em trabalhos futuros. Como subproduto desta investigação, foi gerado um banco de dados em SIG para a continuidade do monitoramento das duas geleiras. / This work investigates the ice front retreat dynamics of two tidewater glaciers, Drummond (66°40'S, 65°43'W) and Widdowson (66°43'S, 65°46'W), on the western coast of the Antarctic Peninsula, associated with environmental changes in the last six decades. The study uses aerial photographs and LANDSAT satellite images (from 1986 onwards) to determine these glaciers area variations in the period 1957–2015 and to analyze their sensitivity to recent environmental changes in the Antarctic Peninsula. The digital elevation model ASTERDEM2 was edited by a routine to characterize the morphology and the morphometry of the drainage basins of these ice masses. The statistical analysis of the updated mean annual temperature data from the Faraday/Vernadsky station (65°14’ S, 64°15’ W) shows a trend towards regional atmospheric warming in the period 1950–2015 (0.047°C year-1) in this part of the West Antarctic Peninsula. The ice fronts of these two glaciers have retreated for the last 68 years, however, the Widdowson Glacier had a more significant loss (36.03 km² or 16.81% of the original area) and a higher snow line elevation (200 m a.s.l. in 2016) than the Drummond Glacier (18.84 km2, or 4.26% of the original area; snow line at 90 m a.s.l. in 2016) in the period. This retreat difference of the two glaciers, side by side and with the same ice flow orientation is attributed to different surface slopes and accumulation area proportion over the total area. The smaller area glacier, Widdowson, has shown to be more sensitive to environmental changes and only reached a stabilization point (supported to the lateral bedrock) in 2001, while the Drummond front stabilized in 1974. In addition, the Widdowson glacier is steeper in the frontal sector, which may have influenced on the calving rate and generate a more efficient basal slip, increasing the ice flow rate and, consequently, increasing the retraction rate. These results are consistent with studies for other floating outlet glaciers with calving in the Antarctic Peninsula, which are more sensitive to climate change. The dynamics of these glaciers is also influenced by changes in ocean forcing, precipitation rates, surface melting and bedrock morphology; these points should be investigated in future works. As a by-product of this research, a GIS database wasgenerated for a continuous monitoring of the two glaciers.

Baseado em estudos morfológicos, as macroalgas marinhas da Baía do Almirantado (Ilha Rei George, Península Antártica) estão representadas por 55 táxons, sendo 30 Rhodophyta, 16 Phaeophyceae e 9 Chlorophyta. Recentemente foi proposta a utilização de 'DNA barcode' para uma rápida e acurada identificação de espécies de macroalgas. Sendo a região 5\' do gene mitocondrial cox 1utilizado para identificação de algas vermelhas e pardas; o gene plastidial tufA utilizado na identificação de algas verdes; e o domínio V do gene 23S rRNA - UPA, universal plastid amplicon, utilizado na identificação de organismos fotossintetizantes. O objetivo desse trabalho foi obter sequências do tipo 'DNA barcodes' e de outros marcadores filogenéticos para a formação do primeiro banco de dados moleculares para as macroalgas da Baía do Almirantado, Antártica. Cerca de 100 espécimes de macroalgas foram coletados, em diversos pontos da baía, durante as OPERANTARes XXV e XXIX, que ocorreram durante dezembro de 2006 a junho de 2007 e dezembro de 2010 a janeiro de 2011, respectivamente. No presente trabalho, foi obtido um total de 209 sequências, cobrindo 29 espécies das 55 citadas para o local, sendo que 157 sequências são para marcadores moleculares do tipo 'DNA barcode', das quais 95 sequências são para o marcador do cloroplasto UPA, 39 sequências para o marcador mitocondrial cox1 e 23 sequências para o tufA. As sequências consenso dos 'DNA barcodes' foram submetidas à análise de distância para determinar os agrupamentos genéticos. Após a análise dos agrupamentos obtidos para os 'DNA barcodes', foram selecionados espécimes, representando cada táxon, para o sequenciamento dos marcadores filogenéticos rbcL, SSU ou ITS totalizando 52 sequências. Neste estudo, foram obtidos dados moleculares para 8 espécies de Chlorophyta, 9 espécies de Phaeophyceae e 14 espécies de Rhodophyta. Entre as espécies de Chlorophyta, Prasiola sp. e Protomonostroma rosulatum (citada anteriormente como P. undulatum), de Phaeophyceae Chordaria linearis e as Rhodophyta Acanthococcus antarticus, Plumariopsis peninsularis e Callophyllis sp. (citada anteriormente como Callophyllis atrosanguinea) são novas citações para a Baía do Almirantado. Sendo que a espécie Callophyllis sp. é possivelmente uma nova espécie. Outras duas espécies previamente citadas, baseado nos resultados moleculares, não ocorrem no local, Desmarestia chordalis e Pyropia woolhousiae. Com os resultados obtidos neste trabalho o número de espécies que ocorrem na Baía do Almirantado passa a 57 táxons / Based on morphological studies, the marine macroalgae of Admiralty Bay ( King George Island , Antarctic Peninsula ) are represented by 55 taxa: 30 Rhodophyta, 16 Phaeophyceae and 9 Chlorophyta. It was recently proposed the use of DNA barcodes for quick and accurate identification of seaweeds. The 5\' end region of mitochondrial cox1 gene is used to identify brown and red algae, the plastid gene tufA is used in identifying green algae, and the V domain of the 23S rRNA gene - UPA universal plastid amplicon is used to identify photosynthetic organisms in general. The aim of this study was to obtain sequences of DNA barcodes and other phylogenetic markers for the formation of the first molecular database for macroalgae of Admiralty Bay, Antarctica. About 100 specimens of macroalgae were collected at various points of the bay during the OPERANTARs XXV and XXIX , which occurred during December 2006 to June 2007 and December 2010 and January 2011 respectively. In this study, we obtained a total of 209 sequences, covering 29 of the 55 species cited for the site. Of those 157 sequences are DNA barcodes, of which 95 are for the marker sequences of chloroplast UPA, 39 sequences for the mitochondrial markercox1 and 23 sequences for the tufA. The consensus sequences of the DNA barcodes were subjected to distance analysis to determine the genetic groupings.After analyzing the clusters obtained for the DNA barcodes, specimens representing each taxon were selected to the sequencing of phylogenetic markers rbcL, SSU and/or ITS sequences totaling 52 sequences for those markers. In this study, molecular data were obtained for 8 species of Chlorophyta , 9 species of Phaeophyceae and 14 species of Rhodophyta. Among the Chlorophyta species, Prasiola sp. and Protomonostroma rosulatum> (previously cited as P. undulatum), the Phaeophyceae Chordaria linearis and the Rhodophyta Acanthococcus antarticus, Plumariopsis peninsularis and Callophyllis sp. (previously cited as Callophyllis atrosanguinea) are new records for the Admiralty Bay. And the species Callophyllis sp. is possibly a new species. Other two species previously mentioned, based on molecular results, Desmarestia chordalis and Pyropia woolhousiae do not occur at the site. With the results obtained in this work the number of species that occur in Admiralty Bay are of 57 taxa.

Respiration, metabolic enzyme assays, and body composition parameters were measured in the Antarctic krill Euphausia superba during the summer, fall and winter on the Western Antarctic Peninsula (WAP). E. superba of all sizes decrease their metabolism from the summer to the winter. These same parameters were also measured along the WAP during the austral fall 2010. E. superba's enzyme activity indicated that there was a latitudinal gradient to the decline in metabolism along the WAP with the more northerly sites having significantly higher metabolic enzyme activities than the sites to the south. Carbon (δ13C) and nitrogen (δ15N) stable isotopes were measured in E. superba along the WAP to determine if there were any latitudinal trends. δ13C showed a significant trend with latitude with more depleted δ13C values in the southern portion of the WAP. Carbon (δ13C) and nitrogen (δ15N) stable isotopes were also measured in two important prey fishes along the WAP, the silverfish Pleuragramma antarcticum and the myctophid Electrona antarctica. P. antarcticum had a more variable and more enriched δ13C value than E. antarctica indicative of P. antarcticum's more neritic habitat. There were no significant differences between the δ15N values of the two fish, indicating that although they feed in different areas they were feeding at the same trophic level. Carbon (δ13C) and nitrogen (δ15N) stable isotopes were measured in twenty species in the marginal ice zone (MIZ) of the Weddell Sea at the beginning of the austral summer. Samples were taken from under the ice, at the ice edge and in the open ocean. A significant trend in the δ13C values of all species was found with the under-ice δ13C values being more depleted than those in the open ocean. This is most likely due to the reduced atmospheric exchange of CO2, upwelled water with depleted δ13C values, and continuous biological respiration under the ice, all of which contribute to very depleted δ13C values. δ15N values were significantly lower in the open ocean than the other ice conditions due to the increased reliance on primary production. The diapausing copepods Calanoides acutus and Rhincalanus gigas showed similar patterns in their isotopic signatures across the ice zones. Cluster analysis revealed trophic shifts between the different ice zones. The ice edge zone proved to contain the most species and was the best habitat for most species. The trophic shifts observed within species in the differing ice conditions mimicked the seasonal changes they undergo during the course of the productive season every year.

Both physical circulation and biogeochemical characteristics are unique in the Southern Ocean (SO) region, and are fundamentally different from those of the northern hemisphere. Moreover, according to previous research, the oceanic response to the trend of the Southern Annual Mode (SAM) has profound impacts on the future oceanic uptake of carbon dioxide in the SO. In other words, the climate and circulation of the SO are strongly coupled to the overlying atmospheric variability. However, while we have understanding on the SO physical circulation and have the ability to predict the future changes of the SO climate and physical processes, the link between the SO physical processes, the air-sea carbon flux, and correlated climate variability remains unknown. Even though scientists have been studying the spatial and temporal variability of the SO carbon flux and the associated biogeochemical processes, the spatial patterns and the magnitudes of the air-sea carbon flux do not agree between models and observations. Therefore, in this study, we utilized a modified version of a general circulation model (GCM) to performed realistic simulations of the SO carbon on seasonal to interannual timescales, and focused on the crucial physical and biogeochemical processes that control the carbon flux. The spatial pattern and the seasonal cycle of the air-sea carbon dioxide flux is calculated, and is broadly consistent with the climatological observations. The variability of air-sea carbon flux is mainly controlled by the gas exchange rate and the partial pressure of carbon dioxide, which is in turn controlled by the compensating changes in temperature and dissolved inorganic carbon. We investigated the seasonal variability of dissolved inorganic carbon based on different regional processes. Furthermore, we also investigated the dynamical adjustment of the surface carbon flux in response to the different gas exchange parameterizations, and conclude that parameterization has little impact on spatially integrated carbon flux. Our simulation well captured the SO carbon cycle variability on seasonal to interannual timescales, and we will improve our model by employ a better scheme of nutrient cycle, and consider more nutrients as well as ecological processes in our future study.

Nothofagus moorei is a long-lived, Gondwana relict cool temperate rainforest tree. Nothofagus-dominated rainforests were widespread across much of eastern Australia during the mid-Tertiary but today, N. moorei occurs only as a series of disjunct, isolated populations in south-east Queensland and northern New South Wales. Clonal regeneration via coppicing is reported to be a common feature of most N. moorei populations, while successful sexual regeneration is believed to be rare, occurring largely only in niches with high light levels and limited competition. While clonal propagation enables population persistence and individual longevity, it cannot generate novel genotypes. Isolated populations, potentially high levels of clonality, low-potential for successful sexual regeneration, long-lived individuals and predicted global warming effects make N. moorei vulnerable to local, if not total, population extinction. The current study aimed to assess the relative conservation status of extant N. moorei populations in order to develop appropriate conservation management strategies for long-term population persistence. Levels of genetic diversity and population structure were examined across the remaining natural distribution of N. moorei using nuclear amplified fragment length polymorphism (AFLP), microsatellite and chloroplast DNA markers. In total 607 individuals were sampled from 20 populations and 5 geographical regions: Lamington/Border Ranges, Ballow, Dorrigo/New England, Werrikimbe and Barrington. Genetic results were then analysed to assess conservation status of each population and geographical region. Microsatellite and AFLP data identified comparatively high levels of genetic diversity in all remnant populations sampled. The prevalence of coppicing in the northern Lamington/Border Ranges populations appears to have had little impact on relative levels of genetic diversity, heterozygosity or population structure. Population differentiation was limited, with the majority of genetic variation retained within populations, no regional structuring and high levels of admixture. Analysis of cpDNA variation showed that the three Dorrigo/New England populations were divergent from all other populations, suggesting an ancient divergence in N. moorei prior to Pleistocene glaciations. While levels of genetic diversity were essentially the same across all populations, Bayesian analysis of genetic structure did identify four populations with differing gene pool proportions which would be important to include in conservation efforts in addition to individuals from other populations. Similarly, individuals from four significantly differentiated groups identified using traditional F-statistics suggests individuals from each of these four groups should be included in future conservation plans. In order to maintain ancient chloroplast lineages, populations from the Dorrigo/New England region should also be assigned special conservation value. Populations of N. moorei appear to have retained significant levels of genetic diversity and show little population divergence in spite of marked reductions in the natural distribution since the Early Miocene. Sampling of these ancient trees however, suggests current levels of diversity in N. moorei actually reflect past diversity and differentiation, and that there have been insufficient generations since the historical contraction in distribution for genetic diversity to be adversely affected and regional differentiation to evolve. Long-term persistence of N. moorei is still threatened by future accelerated climate change and the limited preferred habitat that remains where N. moorei can expand its range. While the ability to regenerate clonally may enable long-term persistence of N. moorei, populations are still likely to continue to decline as climatic conditions will increasingly favour sub-tropical and warm temperate species across much of N. moorei's northern distribution. Southern populations of N. moorei, in contrast, could expand their ranges into eucalypt woodlands as predicted climate becomes warmer and wetter. However, this will ultimately be determined by the frequency of fires, with increased fire frequencies favouring the expansion of eucalypts and contraction and possible local population extinction of N. moorei dominated cool temperate rainforests.

This thesis is presented as a collection of research papers synthesising knowledge gained during the period of candidacy. Its underlying focus is the examination of evolution from a variety of perspectives for terrestrial arthropods (springtails) in an Antarctic setting. These perspectives include investigation of the ways in which springtail populations respond both physiologically and genetically to environmental variability over historical and contemporary time-scales. While the physiological and genetic may seem two worlds apart, this thesis recognises that, in reality the two are inextricably linked. Thus, when genetic differentiation between populations of the same species can be demonstrated, physiological differentiation of these populations may also be predicted (and vice versa). Therefore, across several locations and springtail species, physiological and genetic parameters of individuals and populations are examined both separately and, where possible, in concert. The physiological aspect of this thesis focuses on the springtail Gomphiocephalus hodgsoni from continental Antarctica. In addition to providing the first metabolic rate data for a continental Antarctic springtail, seasonal variation in metabolic rates is examined across multiple temporal and spatial scales to evaluate the ways in which individuals and populations respond to environmental variability. Metabolic activity in this species is intricately linked to a variety of factors, both intrinsic and extrinsic. These include biological function, temperature profiles in the local microclimate, and body mass and genetic differences among populations. In the genetically-focused aspect of this thesis, population genetic patterns of G. hodgsoni from several continental locations and Cryptopygus antarcticus antarcticus from locations across the Antarctica Peninsula are compared. Here, the importance of differing evolutionary histories in influencing patterns of contemporary genetic population structure is highlighted. While both species have been similarly affected genetically by Pleistocene (2 Ma – present) glacial cycling, it is clear that differences in timing of colonisation events and subsequent population expansions have left distinct genetic signatures in each species. In a separate molecular study, phylogenetic analyses are employed to study members of the circum-Antarctic springtail family Isotomidae. Thesis Abstract The genetic ancestry among these closely related species is shown to reflect a diverse evolutionary origin in the Miocene (23 – 5 Ma), subsequent to which both vicariant and dispersal processes have been important. Phylogenetic re-constructions tease out the relationships among sister species, and the identification of several genetically distant lineages suggests that a revision of current species designations is required. Finally, two studies that integrate the physiological and molecular genetic are presented. First, metabolic rate variation across several locations on sub-Antarctic Marion Island in the springtail Cryptopygus antarcticus travei is examined. This variation is related to the genetic structure of populations to show that historical and contemporary environmental characteristics have left their trace in the expression of both genetic and physiological variability of these populations. Second, the perceived association between metabolic rate and genetic (mutation) rate is investigated more closely - a sophisticated Bayesian correlation analysis detects that there is an indirect relationship between metabolic rate and underlying species phylogeny in C. a. travei. Thus, the physiological and molecular genetic elements of this thesis test or advance important hypotheses within their own fields, and the integrated approach applied is a new step in interpreting evidence of physiological adaptation in Antarctic species. In its multi-faceted approach to evolutionary studies, this thesis enhances understanding of the current picture of springtail evolution in polar environments.

A prospecção biológica (i.e. bioprospecção) é uma atividade, relativamente recente, que ocorre de forma desregulada na região austral, área de vigência do Sistema do Tratado da Antártida (STA). A normatização desta atividade no âmbito do STA é o principal tema em discussão na agenda do Regime Antártico. Este Regime Internacional, constituído pelo Tratado Antártico (de 1959), pela Convenção para Preservação das Focas Antárticas (de 1972), pela Convenção para Conservação dos Recursos Vivos Marinhos Antárticos (de 1980) e pelo Protocolo de Proteção Ambiental do Tratado da Antártida (de 1991), tem cumprido, ao longo de sua história, a missão de preservar a região austral e ordenar as atividades antárticas. Os Estados que o integram, enfrentam os novos desafios, criando instrumentos jurídicos para regulamentar atividades específicas. Todavia, eles encontram dificuldades de repetir este comportamento com relação à bioprospeccão. A razão disso é a complexidade desta atividade, associada à problemática da região austral, uma área sem soberanias reconhecidas. Existe imensa dificuldade de desenvolver uma legislação para contemplar diferentes interesses nacionais, disputas entre empresas e organizações ambientalistas, razões de ordem comercial e desacordos entre os interesses de pesquisa científica e do mercado, respeitando as normas e os princípios formalizados no Tratado Antártico. A bioprospecção na Antártida é um problema cuja solução, provavelmente, demandará longas e difíceis negociações. / Biological prospecting (i.e. bioprospecting) is a relatively recent activity that occurs unregulated in the austral region, area covered by the Antarctic Treaty System (ATS). The normatization of this activity is the main subject being discussed in the agenda of the Antarctic Regime. This International Regime, comprised by the Antarctic Treaty (1959), the Convention on the Conservation of Antarctic Seals (1972), the Convention on the Conservation of Antarctic Marine Living Resources (1980) and the Madrid Protocol to the Antarctic Treaty (1991), fulfills the mission to preserve the austral region and regulate international relations with respect to Antarctica. The nation-states, participants in this regime, have a tendency to face new challenges, by creating aditional agreements to regulate specific activities. Bioprospecting, however, has proven dificult to regulate. This is due to the complexity of the activity and the ambiguous territorial status of Antarctica. It is dificult to develop legislation that satifies interests of nation-states, private companies, environmental NGO’s, scientists and universities, while respecting norms and principles formalized in the Antarctic Treaty. Bioprospecting in Antarctica, therefore, is a problem that demands carefull and thoughtfull considerations, yet to be resolved.

Esta dissertação investiga o registro de conteúdo iônico do testemunho de gelo monte Johns (79°55'28"S; 94°23'18"O) obtido na Antártica Ocidental, contribuindo para o adensamento espacial de informações glacioquímicas empregadas em estudos paleoclimáticos. As concentrações de Na+ (16,6 ± 28,2 μg L-1), K+ (1,3 ± 3,7 μg L-1), Mg2+ (3,7 ± 3,7 μg L-1), Ca2+ (5,4 ± 3,4 μg L-1), Cl- (33,3 ± 43,7 μg L-1), SO42- (25,9 ± 17,7 μg L-1), NO3- (50,8 ± 18,5 μg L-1) e H3CSO3- (7,1 ± 5,4 μg L-1) foram determinadas por cromatografia iônica em 2.164 amostras para o período 1882–2008. A variabilidade sazonal de NO3- e, especialmente do nssSO42-, em antifase com Na+, possibilitou a datação pela contagem de ciclos anuais ao longo do período estudado. A identificação dos sinais vulcânicos do Krakatoa (1883), Agung (1963) e Pinatubo/Hudson (1991) foi usada para determinar horizontes de referência (datação absoluta). Eventos de aporte significativo de aerossóis foram identificados e agrupados considerando o conteúdo iônico, proveniência e estação do ano. A avaliação da proveniência dos íons e do balanço iônico mostra a origem da carga iônica: 36% é oriunda de aerossóis de sal marinho, 13% de poeira mineral, 17% de atividade biogênica marinha e 34% de produtos da reatividade química na atmosfera. É observada uma leve redução nas concentrações de Mg2+ (-0,04 μg L-1 ano-1) e K+ (-0,01 μg L-1 ano-1), e mais forte para NO3- (-0,17 μg L-1 ano-1), no período 1909–2008. A média anual da acumulação líquida de neve foi 0,21 ± 0,04 m eq. H2O no período 1882–2008 sem apresentar tendência significante. A acumulação mostra alta correspondência com dados anuais de reanálise climática, com coeficiente de correlação cruzada de +0,42 (α < 0,05) para o período 1979–2008. / This dissertation investigates the ionic content record of the mount Johns ice core (79°55'28"S; 94°23'18"W) recovered from the West Antarctica, contributing to the spatial densification of glaciochemical information used in paleoclimatic studies. The concentrations of Na+ (16.6 ± 28.2 μg L-1), K+ (1.3 ± 3.7 μg L-1), Mg2+ (3.7 ± 3.7 μg L-1), Ca2+ (5.4 ± 3.4 μg L-1), Cl- (33.3 ± 43.7 μg L-1), SO42- (25.9 ± 17.7 μg L-1), NO3- (50.8 ± 18.5 μg L-1) e H3CSO3- (7.1 ± 5.4 μg L-1) were determined by ion chromatography on 2,164 samples for the period 1882–2008. The NO3- seasonal variability and, especially, of the nssSO42- in antiphase with the Na+, allowed the counting of annual cycles over the studied period. The identification of Krakatau (1883), Agung (1963) and Pinatubo / Hudson (1991) volcanic signals was used to determine reference horizons (absolute dating). Significant aerosols events were identified and grouped considering the ionic content, provenance and season of the year. The evaluation of the ions provenance and of the ionic balance points to ionic content origin: 36% come from sea salt aerosols, 13% from mineral dust, 17% originate from marine biogenic activity and 34% are chemical reactivity products in the atmosphere. It is observed a slight reduction in the Mg2+ (-0.04 μg L-1 y-1) and K+ (-0.01 μg L-1 y-1) concentrations, and stronger in the NO3- (-0.17 μg L-1 y-1), during the 1909–2008 period. The annual mean net accumulation rate averaged 0.21 ± 0.04 m w.e. y-1 in the period 1882–2008 did not show any significant trend and shows high correspondence with climatic reanalysis data in years with data overlap, with a cross-correlation coefficient of +0.42 (α < 0.05) for the period 1979–2008.