Lakes are increasingly being recognized as an important component of the global carbon cycle, yet anthropogenic activities that alter their community structure may change the way they transport and process carbon. This research focuses on the relationship between carbon cycling and community structure of primary producers in small, shallow lakes, which are the most abundant lake type in the world, and furthermore subject to intense terrestrial-aquatic coupling due to their high perimeter:area ratio. Shifts between macrophyte and phytoplankton dominance are widespread and common in shallow lakes, with potentially large consequences to regional carbon cycling. I thus compared a lake with clear-water conditions and a submerged macrophyte community to a turbid, phytoplankton-dominated lake, describing differences in the availability, processing, and export of organic and inorganic carbon. I furthermore examined the effects of increasing terrestrial carbon inputs on internal carbon cycling processes. Pelagic diel (24-hour) oxygen curves and independent fluorometric approaches of individual primary producers together indicated that the presence of a submerged macrophyte community facilitated higher annual rates of gross primary production than could be supported in a phytoplankton-dominated lake at similar nutrient concentrations. A simple model constructed from the empirical data suggested that this difference between regime types could be common in moderately eutrophic lakes with mean depths under three to four meters, where benthic primary production is a potentially major contributor to the whole-lake primary production. It thus appears likely that a regime shift from macrophyte to phytoplankton dominance in shallow lakes would typically decrease the quantity of autochthonous organic carbon available to lake food webs. Sediment core analyses indicated that a regime shift from macrophyte to phytoplankton dominance was associated with a four-fold increase in carbon burial rates, signalling a major change in lake carbon cycling dynamics. Carbon mass balances suggested that increasing carbon burial rates were not due to an increase in primary production or allochthonous loading, but instead were due to a higher carbon burial efficiency (carbon burial / carbon deposition). This, in turn, was associated with diminished benthic mineralization rates and an increase in calcite precipitation, together resulting in lower surface carbon dioxide emissions. Finally, a period of unusually high precipitation led to rising water levels, resulting in a feedback loop linking increasing concentrations of dissolved organic carbon (DOC) to severely anoxic conditions in the phytoplankton-dominated system. High water levels and DOC concentrations diminished benthic primary production (via shading) and boosted pelagic respiration rates, diminishing the hypolimnetic oxygen supply. The resulting anoxia created redox conditions which led to a major release of nutrients, DOC, and iron from the sediments. This further transformed the lake metabolism, providing a prolonged summertime anoxia below a water depth of 1 m, and leading to the near-complete loss of fish and macroinvertebrates. Pelagic pH levels also decreased significantly, increasing surface carbon dioxide emissions by an order of magnitude compared to previous years. Altogether, this thesis adds an important body of knowledge to our understanding of the significance of the benthic zone to carbon cycling in shallow lakes. The contribution of the benthic zone towards whole-lake primary production was quantified, and was identified as an important but vulnerable site for primary production. Benthic mineralization rates were furthermore found to influence carbon burial and surface emission rates, and benthic primary productivity played an important role in determining hypolimnetic oxygen availability, thus controlling the internal sediment loading of nutrients and carbon. This thesis also uniquely demonstrates that the ecological community structure (i.e. stable regime) of a eutrophic, shallow lake can significantly influence carbon availability and processing. By changing carbon cycling pathways, regime shifts in shallow lakes may significantly alter the role of these ecosystems with respect to the global carbon cycle. / Seen werden zunehmend als wichtige Komponente im globalen Kohlenstoffkreislauf anerkannt. Natürliche Veränderungen und anthropogene Aktivitäten beeinflussen die Struktur der Artengemeinschaft von Seen, was Auswirkungen auf den Transport und Umsatz von Kohlenstoff hat. Diese Arbeit konzentriert sich auf die Beziehung zwischen Kohlenstoffkreislauf und der Gemeinschaftsstruktur der Primärproduzenten in kleinen Flachseen. Diese sind der weltweit häufigste Seentyp und weisen durch ihren im Vergleich zur Fläche großen Umfang eine intensive aquatisch-terrestrische Kopplung auf. In Flachseen treten oft Regimewechsel zwischen Makrophyten- und Phytoplankton-Dominanz auf. Diese können potenziell große Konsequenzen für den regionalen Kohlenstoffkreislauf haben. In dieser Dissertation vergleiche ich einen Klarwassersee mit submersen Makrophyten und einen trüben, Phytoplankton-dominierten See hinsichtlich Verfügbarkeit, Umsatz und Export von organischem und anorganischem Kohlenstoff. Des Weiteren habe ich den Effekt der erhöhten Zufuhr von terrestrischem Kohlenstoff auf den internen Kohlenstoffumsatz untersucht. Sowohl die Tagesgänge der pelagischen Sauerstoff-Konzentrationen als auch Fluoreszenz-basierte Messungen der Primärproduktion bewiesen, dass die Präsenz von submersen Makrophyten eine höhere jährliche Brutto-Primärproduktion im Vergleich zu einem Phytoplankton-dominierten See mit ähnlichen Nährstoffkonzentrationen ermöglicht. Ein einfaches, auf den empirischen Daten basierendes Model zeigt, dass diese Unterschiede in der Brutto-Primärproduktion typisch sind für moderat eutrophe Seen mit einer mittleren Tiefe von unter 3 bis vier Metern. In diesen Seen leistet die benthische Primärproduktion den Hauptbeitrag zur Primärproduktion des ganzen Sees. Daraus wird ersichtlich, dass Regimewechsel von Makrophyten- zur Phytoplankton-Dominanz in Flachseen die Verfügbarkeit von autochthonem organischem Kohlenstoff für das Nahrungsnetz reduzieren. Paläolimnologische Analysen in Sedimentkernen beider Seen wiesen darauf hin, dass der Verlust der Makrophyten mit einer vierfachen Zunahme der Kohlenstoff-Speicherraten einhergeht, und somit zu einer großen Veränderung der Dynamik des Kohlenstoffkreislaufs im See führt. Unsere Kohlenstoff-Massenbilanzen zeigen, dass die Erhöhung der Kohlenstoff-Speicherung im Sediment nicht durch die Erhöhung der Primärproduktion oder durch externe Quellen, sondern durch erhöhte der Effizienz der Speicherung begründet war. Dies geht mit einer reduzierten benthischen Mineralisierungsrate und einer erhöhten Calcitfällung einher und führt zu reduzierten Kohlendioxid-Emissionen. Eine Periode ungewöhnlich hoher Niederschläge mit erhöhten Wasserständen führte im Phytoplankton-dominierten See zu zu einem starken Anstieg der Konzentrationen an gelöstem organischem Kohlenstoff (DOC) und zu anoxischen Bedingungen. Es wurde postuliert, dass zwischen diesen Prozessen eine positive Rückkopplung besteht. Die hohen Wasserstände und DOC-Konzentrationen reduzierten die Lichtversorgung und damit die Primärproduktion im Benthal und erhöhten die pelagischen Respirationsraten. Dadurch verringerte sich die Sauerstoffverfügbarkeit im Hypolimnion. Die dadurch erzeugten Redox-Verhältnisse führten zu einer Freisetzung großer Mengen an Nährstoffen, DOC und Eisen aus dem Sediment. Die während des gesamten Sommers andauernden anoxischen Verhältnisse in Wassertiefen unter 1 m führten zu einem fast vollständigen Verlust von Fischen und Makroinvertebraten. Zusätzlich wurde der pH-Wert im Pelagial signifikant erniedrigt und die Kohlenstoffdioxid-Emissionen im Vergleich zu früheren Jahren verzehnfacht. Insgesamt trägt diese Dissertation wesentliche Aspekte zum besseren Verständnis der Bedeutung des Benthals für den Kohlenstoffkreislauf in Flachseen bei. Der Anteil der benthischen Zone an der Primärproduktion in kleinen Flachseen wurde in Relation zur Gesamtproduktion des Systems quantifiziert. Letztlich zeigt diese Arbeit, dass die Gemeinschaftsstruktur der Primärproduzenten eines eutrophen Flachsees die Verfügbarkeit und den Umsatz von Kohlenstoff signifikant beeinflusst. Regimewechsel in Flachseen können durch Änderungen im internen Kohlenstoffkreislauf deren Rolle im globalen Kohlenstoffkreislauf verändern.

Oxygen can be limited at the environmental (e.g. flood-prone burrows) or cellular (e.g. stroke, heart attack) levels. O2 deprivation in nervous tissue depolarizes cell membranes, incrementing extracellular potassium concentration ([K+]o). Consequently, [K+]o can be used to assess neural failure during anoxia. The effect of temperature on the maintenance of brain [K+]o homeostasis in male and female Drosophila melanogaster (W1118) was assessed during repeated anoxic comas induced by N2 gas. Brain [K+]o was continuously monitored using K+-sensitive microelectrodes while body temperature was gradually increased/decreased using a Peltier plate. Once the desired temperature was reached (16°C/17°C, 23°C or 29°C/30°C), it was maintained for the rest of the experiment and the fly was subjected to repeated anoxic bouts. Repetitive anoxia resulted in a loss of the ability to maintain [K+]o baseline at ~10 mM. In both sexes, the total [K+]o baseline variation (D[K+]o) was augmented at 30°C (D[K+]o male = 119.2 ± 21.9 mM; D[K+]o female = 51.2 ± 8.1 mM), whereas 16°C stabilized [K+]o baseline for the duration of the experiment (D[K+]o male = 17.5 ± 4.1 mM; D[K+]o female = 16.9 ± 6.8 mM). Additionally, D[K+]o in males was significantly greater (114.3 ± 10.5 mM ) than in females (36.1 ± 10.5 mM) at 23°C. Under reduced dehydration, experiments performed only in males showed the same trends although the D[K+]o values where considerably reduced at 17°C (D[K+]o male = -1.0 ± 1.3 mM) and 23°C (D[K+]o male = 17.3 ± 1.5 mM) and increased at 29°C (D[K+]o male = 332.7 ± 83.0 mM). It was concluded that 1) N2-delivery patterns consisting of long anoxia, short normoxia and high cycle frequency increased disruption of brain [K+]o baseline maintenance, 2) males were more susceptible to repeated anoxia than females at room temperature, and 3) hypothermia had a protective effect on brain K+ homeostasis during repetitive anoxia. Male flies are suggested as a useful model for examining deleterious consequences of O2 reperfusion with extensive application on therapeutical treatment of stroke or heart attack. / Thesis (Master, Biology) -- Queen's University, 2012-01-30 13:03:10.913

The ocean is the most extended biome present on our planet. Recent decades have seen a dramatic increase in the number and gravity of threats impacting the ocean, including discharge of pollutants, cultural eutrophication and spread of alien species. It is essential therefore to understand how different impacts may affect the marine realm, its life forms and biogeochemical cycles. The marine nitrogen cycle is of particular importance because nitrogen is the limiting factor in the ocean and a better understanding of its reaction mechanisms and regulation is indispensable. Furthermore, new nitrogen pathways have continuously been described. The scope of this project was to better constrain cause-effect mechanisms of microbially mediated nitrogen pathways, and how these can be affected by biotic and abiotic factors. This thesis demonstrates that meiofauna, the most abundant animal group inhabiting the world’s seafloors, considerably alters nitrogen cycling by enhancing nitrogen loss from the system. In contrast, larger fauna such as the polychaete Marenzelleria spp. enhance nitrogen retention, when they invade eutrophic Baltic Sea sediments. Sediment anoxia, caused by nutrient excess, has negative consequences for ecosystem processes such as nitrogen removal because it stops nitrification, which in turn limits both denitrification and anammox. This was the case of Himmerfjärden and Byfjord, two estuarine systems affected by anthropogenic activities, such as treated sewage discharges. When Byfjord was artificially oxygenated, nitrate reduction mechanisms started just one month after pumping. However, the balance between denitrification and nitrate ammonification did not favor either nitrogen removal or its retention. Anoxia is also present in aggregates of the filamentous cyanobacteria Nodularia spumigena. This thesis shows that even in fully oxic waters, millimetric aggregates can host anaerobic nitrogen processes, with clear implications for the pelagic compartment. While the thesis contributed to our knowledge on marine nitrogen cycling, more data need to be collected and experiments performed in order to understand key processes and regulation mechanisms of element cycles in the ocean. In this way, stakeholders may follow and take decisions in order to limit the continuous flow of human metabolites and impacts on the marine environment. / <p>At the time of the doctoral defense, the following paper was unpublished and had a status as follows: Paper 2: Manuscript.</p>

Serotonin (5-HT)-containing neuroepithelial cells (NECs) of the gill filament are believed to be the primary O2 chemosensors in fish. In the mammalian carotid body (CB), 5-HT is one of many neurotransmitters believed to play a role in transduction of hypoxic stimuli, with acetylcholine (ACh) being the primary fast-acting excitatory neurotransmitter. Immunohistochemistry and confocal microscopy was used to observe the presence of the vesicular acetylcholine transporter (VAChT), a marker for the presence of ACh, and its associated innervation in the gills of zebrafish. VAChT-positive cells were observed primarily along the afferent side of the filament, with some cells receiving extrabranchial innervation. No VAChT-positive cells were observed in the gills of goldfish; however, certain key morphological differences in the innervation of goldfish gills was observed, as compared to zebrafish. In addition, in zebrafish NECs, whole-cell current is dominated by an O2-sensitive background K+ current; however, this is just one of several currents observed in the mammalian CB. In zebrafish NECs and the CB, membrane depolarization in response to hypoxia, mediated by inhibition of the background K+ (KB) channels, is believed to lead to activation of voltage-gated Ca2+ (CaV) channels and Ca2+-dependent neurosecretion. Using patch-clamp electrophysiology, I discovered several ion channel types not previously observed in the gill chemosensors, including Ca2+-activated K+ (KCa), voltage-dependent K+ (KV), and voltage-activated Ca2+ (CaV) channels. Under whole-cell patch-clamp conditions, the goldfish NECs did not respond to hypoxia (PO2 ~ 11 mmHg). Employing ratiometric calcium imaging and an activity-dependent fluorescent vital dye, I observed that intact goldfish NECs respond to hypoxia (PO2 ~ 11 mmHg) with an increase in intracellular Ca2+ ([Ca2+]i) and increased synaptic vesicle activity. The results of these experiments demonstrate that (1) ACh appears to play a role in the zebrafish, but not goldfish gill, (2) goldfish NECs likely signal hypoxic stimuli primarily via the central nervous system (CNS), (3) goldfish NECs express a broad range of ion channels as compared to the NECs of zebrafish, and (4) goldfish NECs rely on some cytosolic factor(s) when responding to hypoxia (PO2 ~ 11 mmHg). This thesis represents a further step in the study of neurochemical and physiological adaptations to tolerance of extreme hypoxia.

[Truncated abstract] In this thesis the role of lactate measurement has been evaluated in intrapartum assessment of fetal wellbeing. Specifically, I have addressed the question of whether fetal lactate measurement is better than the assessment of fetal heart rate patterns or the measurement of pH at predicting fetal brain injury after intrapartum asphyxia. Using an ovine model of repeated umbilical cord occlusion designed to mimic events which may occur during human labour, I have shown that the measurement of fetal lactate levels after repeated cord occlusion is significantly associated with the severity of brain injury after the asphyxial insult. No significant associations were identified with fetal pH measurements or with the duration of decelerative or compound fetal heart rate patterns; however, this is the first study to describe an association between the duration of both increased fetal heart rate variability and fetal heart rate overshoot with the severity of subsequent brain injury. Although no significant association was identified between fetal arterial pressure measured between umbilical cord occlusions and the grade of brain injury, the studies performed in this thesis are the first to show a strong correlation between the duration of specific arterial pressure responses during cord occlusions and the grade of brain injury, accounting for approximately 90% of the variability seen in the severity of injury. The mechanism responsible for the improved ability of lactate measurement to predict fetal brain injury is unknown. It may be because fetal lactate levels are a more stable marker of anaerobic metabolism of glucose than fetal pH levels, which are influenced by both increasing levels of carbon dioxide and anaerobic metabolism of amino-acids and fatty acids. In addition fetal pH levels can be rapidly normalised through placental exchange of carbon dioxide whereas fetal lactate levels are slow to normalise across the placenta as they rely on facilitated diffusion.

Diss. (sammanfattning) Stockholm : Karolinska institutet, 2005. / Härtill 4 uppsatser.

abstract: The ability to tolerate bouts of oxygen deprivation varies tremendously across the animal kingdom. Adult humans from different regions show large variation in tolerance to hypoxia; additionally, it is widely known that neonatal mammals are much more tolerant to anoxia than their adult counterparts, including in humans. Drosophila melanogaster are very anoxia-tolerant relative to mammals, with adults able to survive 12 h of anoxia, and represent a well-suited model for studying anoxia tolerance. Drosophila live in rotting, fermenting media and a result are more likely to experience environmental hypoxia; therefore, they could be expected to be more tolerant of anoxia than adults. However, adults have the capacity to survive anoxic exposure times ~8 times longer than larvae. This dissertation focuses on understanding the mechanisms responsible for variation in survival from anoxic exposure in the genetic model organism, Drosophila melanogaster, focused in particular on effects of developmental stage (larval vs. adults) and within-population variation among individuals. Vertebrate studies suggest that surviving anoxia requires the maintenance of ATP despite the loss of aerobic metabolism in a manner that prevents a disruption of ionic homeostasis. Instead, the abilities to maintain a hypometabolic state with low ATP and tolerate large disturbances in ionic status appear to contribute to the higher anoxia tolerance of adults. Furthermore, metabolomics experiments support this notion by showing that larvae had higher metabolic rates during the initial 30 min of anoxia and that protective metabolites were upregulated in adults but not larvae. Lastly, I investigated the genetic variation in anoxia tolerance using a genome wide association study (GWAS) to identify target genes associated with anoxia tolerance. Results from the GWAS also suggest mechanisms related to protection from ionic and oxidative stress, in addition to a protective role for immune function. / Dissertation/Thesis / Results of GWAS for Adults Exposed to 6 H of Anoxia / Results of GWAS for Larvae Exposed to 1 H of Anoxia / Doctoral Dissertation Evolutionary Biology 2018

abstract: There is a growing body of evidence that the evolving redox structure of the oceans has been an important influence on the evolutionary trajectory of animals. However, current understanding of connections between marine redox conditions and marine extinctions and recoveries is hampered by limited detailed knowledge of the timing, duration, and extent of marine redox changes. The recent development of U isotopes (δ238U) in carbonates as a global ocean redox proxy has provided new insight into this problem. Reliable application and interpretation of the δ238U paleoproxy in geological records requires a thorough understanding of the reliability of δ238U recorded by bulk carbonate sediments. In this dissertation, I evaluate the robustness of δ238U paleoproxy by examining δ238U variations in marine carbonates across Permian-Triassic boundary (PTB) sections from different paleogeographic locations. Close agreement of δ238U profiles from coeval carbonate sections thousands of kilometers apart, in different ocean basins, and with different diagenetic histories, strongly suggests that bulk carbonate sediments can reliably preserve primary marine δ238U signals, validating the carbonate U-isotope proxy for global-ocean redox analysis. To improve understanding of the role of marine redox in shaping the evolutionary trajectory of animals, high-resolution δ238U records were generated across several key evolutionary periods, including the Ediacaran-to-Early Cambrian Explosion of complex life (635-541 Ma) and the delayed Early Triassic Earth system recovery from the PTB extinction (252-246 Ma). Based on U isotope variations in the Ediacaran-to-the Early Cambrian ocean, the initial diversification of the Ediacara biota immediately postdates an episode of pervasive ocean oxygenation across the Shuram event. The subsequent decline and extinction of the Ediacara biota is coincident with an episode of extensive anoxic conditions during the latest Ediacaran Period. These findings suggest that global marine redox changes drove the rise and fall of the Ediacara biota. Based on U isotope variations, the Early Triassic ocean was characterized by multiple episodes of extensive marine anoxia. By comparing the high-resolution δ238U record with the sub-stage ammonoid extinction rate curve, it appears that multiple oscillations in marine anoxia modulated the recovery of marine ecosystems following the latest Permian mass extinction. / Dissertation/Thesis / Doctoral Dissertation Geological Sciences 2018

Orientador: Carlos Alfredo Joly / Dissertação (mestrado) - Universidade Estadual de Campinas, Instituto de Biologia / Made available in DSpace on 2018-08-12T20:33:26Z (GMT). No. of bitstreams: 1 Brigitte_PriscilaAugusta_M.pdf: 2206000 bytes, checksum: 45f6665ec05b449a5637ed3193764cac (MD5) Previous issue date: 2008 / Resumo: Foram estudados aspectos ecofisiológicos da germinação de Hedychium coronarium J. König e suas características quanto à anatomia e à reserva das sementes. O principal foco foi o estudo de seu comportamento sob diferentes condições de oxigenação, sendo estes os tratamentos: normoxia, hipoxia e anoxia. Trata-se de uma espécie exótica, invasora de ambientes brejosos, nos quais há, periódica e naturalmente, uma restrição na disponibilidade de oxigênio dissolvido no solo em virtude da saturação hídrica que ocorre nestas áreas. Sob tais condições, Hedychium apresenta vantagem competitiva e impede a regeneração das plantas nativas. Atualmente presente em praticamente toda a América, é uma espécie originária da Ásia, trazida inicialmente com fins ornamentais, mas hoje é também utilizada como planta medicinal, dentre outras aplicações já dadas à espécie. As sementes utilizadas foram coletadas no Núcleo Picinguaba, do Parque Estadual da Serra do Mar, Ubatuba-SP. Os testes de germinação compararam suas respostas à luz, à alternância de temperaturas e à disponibilidade de oxigênio e determinaram a longevidade das sementes. Também foi verificada a viabilidade das sementes através do teste com tetrazólio. Em relação ao estudo dos tecidos de reserva, foram feitos cortes anatômicos em sementes submetidas a diferentes condições de oxigenação, com posterior coloração com diferentes substâncias, com diferentes afinidades, para verificar quais as reservas presentes e verificar possível diferença quanto ao consumo das mesmas de acordo com o tratamento recebido pela semente durante o processo de germinação. Os resultados demonstraram que a espécie germina indiferente à luz, ou seja, é fotoblástica neutra, e tem sua germinação retardada, porém não diminuída, sob temperaturas que simulam as condições de inverno da região de coleta das sementes utilizadas neste estudo. As sementes mostraram boa viabilidade até cerca de um ano após a dispersão, sendo que, após esse período, a taxa de germinação caiu sensivelmente. Embora esta espécie tolere bem condições de pouca disponibilidade de oxigênio e seja capaz de colonizar ambientes que apresentem esta característica com sucesso, seu melhor desempenho em relação à germinação, ocorre sob condições drenadas e de boa aeração. Os estudos anatômicos indicaram que o processo de germinação foi iniciado sob privação de oxigênio, porém não foi viável pelo período testado (30 dias), pois provocou a morte das sementes. As sementes apresentam dois tipos de tecidos de reservas, perisperma e endosperma, de acordo com o esperado para a família (Zingiberaceae), porém de ocorrência conhecida apenas para poucos grupos de plantas. A composição dos tecidos indica que sua principal reserva é composta por polissacarídeos, sendo amido o principal, encontrado tanto no perisperma, como no endosperma, e proteínas dispersas no citoplasma das células do endosperma. / Abstract: Ecophysiological aspects of Hedychium coronarium J. König and its characteristics concerning anatomy and seeds storage were studied aiming to understand its behavior under different oxygenation conditions, with the following treatment: normoxia, hypoxia e anoxia. This is an exotic species, invasive of water logging environments, where there is, regular and naturally, a restriction on the availability of dissolved oxygen in the soil, because of water saturation in these areas. Under such conditions, the competitive advantage of Hedychium prevents the regeneration of native plants. Currently present in almost all of America, it is a species originated in Asia, initially brought with ornamental purposes, but today is also used as a medicinal plant, among other applications already given to the species. The seeds used were collected in Ubatuba-SP, at "Núcleo Picinguaba", from PESM. Tests for germination compared their responses to light, the alternation of temperatures and availability of oxygen and determine the seeds' longevity. The viability of seeds was also verified through the test with tetrazolium. Regarding the study of storage tissues, anatomical cuts were made in seeds subjected to different conditions of oxygenation, with subsequent staining with different substances, with different affinities, to check the present storages and check possible difference in regard to their consumption according to the treatment received by the seed during germination. The results have shown that the species germinates indifferent to light, i.e, it is a neutral photoblastic, and it has its germination delayed, but not decreased, under temperatures that simulate the winter conditions of the region where the seeds used in this study were collected. The seeds resist with good viability until about a year after the dispersion, when the germination rate falls significantly.Although well able to tolerate low availability of oxygen and capable of colonizing environments that successfully present this characteristic, its best performance concerning germination occurs under conditions of good aeration and drained conditions. Anatomical studies indicate that the process of germination was initiated, but not viable for the testing period (30 days), under this condition. The seeds feature two types of storage tissue, perisperm and endosperm, according to the expected for the family (Zingiberaceae), but occurring for only a few groups of plants. The composition of tissues indicates that its main storage is composed of polysaccharides, being starch the main one, found both in perisperm and endosperm, and protein scattered in the cytoplasm of cells in the endosperm. / Mestrado / Mestre em Biologia Vegetal

Agressões nos períodos críticos do crescimento do sistema nervoso podem modificar os eventos de desenvolvimento. Entre os vários fatores nocivos está a anóxia. O organismo do neonato tem suprimento de energia anaeróbica relativamente rica, foi observado que a acidose ocorre com menor facilidade, propiciam sobrevivência. A proteína de astrócitos, S100<font face=\"Symbol\">b, exerce efeitos parácrinos e autócrinos em neurônios e glia. Sua estimulação promove sobrevivência e proteção neuronal, atuando como fator trófico e neurotrófico. Modelo animal de anóxia neonatal desenvolvido em nosso laboratório, nos revelou ativação neural pela expressão de Fos e alterações comportamentais, o que nos instigou a explorar os efeitos da anóxia nas células da glia no Hipocampo e Núcleo do Trato Solitário. Para sua exposição à anoxia, durante 25 minutos, foi utilizada câmara, saturada com nitrogênio gasoso 100%. Grupos P2 e P7 nas condições: Basal (B), sem estimulo; Sham (S) como controle experimental e Anóxia (A) com falta de oxigênio, foram analisados por S100<font face=\"Symbol\">b-IR com técnicas ABC/DAB e Western blot. Observamos significante diferença de S100<font face=\"Symbol\">b-IR no núcleo do trato solitário, somente no grupo P2 A 2 h em relação ao grupo P2 S 2 h. A reatividade glial de S100<font face=\"Symbol\">b na formação hipocampal (CA1, CA3+CA2 e DG), apresentou diferença significante no grupo anoxia de acordo com o estágio de maturação do animal. A técnica por Western blot em toda a formação hipocampal, apresentou aumento de S100<font face=\"Symbol\">b no grupo A em ambos P2 e P7, a avaliação de um todo foi diferente daquela de áreas especificas. / Attacks to the nervous system at critical growth periods can modify developmental events. Among the various harmful factors at is anoxia. The high anaerobic energy supply to the newborn and a less easily acidosis occurrence provides survival. The astrocyte S100<font face=\"Symbol\">b protein exerts paracrine and autocrine effects on neurons and glia. Its stimulation promotes neuronal survival and protection, as a trophic and neurotrophic factor. An animal model of neonatal anoxia improved in our lab revealed neural activation by Fos expression and behavioral changes, which prompted us to explore the anoxia effects on glial cells in the Hypocampus and Nucleus of Solitary Tract. For their exposure to anoxia, a chamber, saturated with 100% nitrogen gas, for 25 minutes were used. Groups with P2 and P7, conditions: Baseline, without stimulation; Sham as the experimental control, and Anoxia with lack of oxygen, were evaluated by S100<font face=\"Symbol\">b-IR by ABC/DAB and Western blot techniques. The nucleus of solitary tract, significant different S100<font face=\"Symbol\">b-IR observed, only in the P2 A 2 h compared to P2 S 2 h. The glial S100<font face=\"Symbol\">b-IR at the hippocampal formation (CA1, CA2 + CA3 and DG) presented significant difference in the anoxic group according to the maturational stage of the animal. Western blot technique of the entire hippocampal formation, showed increase of S100<font face=\"Symbol\">b at the group A at both P2 and P7, the whole evaluation was different from of that of specific areas.