Efeitos de diferentes frações inspiradas de oxigênio sobre variáveis cardiorrespiratórias e histopatologia pulmonar em coelhos com cardiomiopatia dilatada, anestesiados com sevofluorano

Pós-graduação em Cirurgia Veterinária - FCAV

A Two-Stage Aerobic/Anaerobic Denitrifying Horizontal Bioreactor Designed for Treating Ammonium and H2S Simultaneously

A two-stage bioreactor was operated for a period of 140 days in order to develop a post-treatment process based on anaerobic bioxidation of sulfite. This process was designed for simultaneously treating the effluent and biogas of a full-scale UASB reactor, containing significant concentrations of NH4 and H2S, respectively. The system comprised of two horizontal-flow bed-packed reactors operated with different oxygen concentrations. Ammonium present in the effluent was transformed into nitrates in the first aerobic stage. The second anaerobic stage combined the treatment of nitrates in the liquor with the hydrogen sulfide present in the UASB-reactor biogas. Nitrates were consumed with a significant production of sulfate, resulting in a nitrate removal rate of 0.43 kg N m(3) day(-1) and a parts per thousand yen92 % efficiency. Such a removal rate is comparable to those achieved by heterotrophic denitrifying systems. Polymeric forms of sulfur were not detected (elementary sulfur); sulfate was the main product of the sulfide-based denitrifying process. S-sulfate was produced at a rate of about 0.35 kg m(3) day(-1). Sulfur inputs as S-H2S were estimated at about 0.75 kg m(3) day(-1) and Chemical Oxygen Demand (COD) removal rates did not vary significantly during the process. DGGE profiling and 16S rRNA identified Halothiobacillus-like species as the key microorganism supporting this process; such a strain has not yet been previously associated with such bioengineered systems.

Relationship between space distribution of the benthic macroinvertebrates community and trophic state in a Neotropical reservoir (Itupararanga, Brazil)

The purpose of this work was to verify the benthic macroinvertebrates community responses through environmental factors along a headwater tropical reservoir. Samplings were taken with a Van-Veen grab along the reservoir in littoral and profundal regions and in the headwater, next to the dam and the middle of the reservoir. Samples were taken during both wet and dry seasons. Dissolved oxygen concentrations, electric conductivity, temperature and pH near the sediment have been performed in situ, at every sampling station by using a multiprobe and Secchi disc. Total water phosphorus and chlorophyll a concentrations were analyzed to determine the trophic state index. Sediment's organic matter, total phosphorus, nitrogen concentrations and granulometric composition were measured. In order to verify which environmental variables would have more influence over the benthic macroinvertebrates community, a canonical correspondence analysis (CCA) was performed. The total number of recorded taxa was 28. Among them, the family Chironomidae (Diptera) was the richest group (19 taxa). It can be proposed that the benthic macroinvertebrates community may be influenced by environmental conditions such as nutrient and organic matter availability, as well as dissolved oxygen concentration. Macroinvertebrates are adequate bioindicators of water quality due to their sensibility to environmental changes mentioned before. Chironomus sp, Limnodrilus hoffmeisteri and Branchiura sowerbyi comprises a group that can be considered bio-indicators of eutrophic conditions. A second group can be considered as indicator of mesotrophic conditions. The presence of two or more members from that group which comprises Tanytarsini spp, Fissimentum sp, Pelomus sp and Goeldichironomus sp, like predominant taxa, may indicates mesotrophic conditions.

Deposit-feeding in benthic macrofauna : Tracer studies from the Baltic Sea

A low content of organic matter, which is largely refractory in nature, is characteristic of most sediments, meaning that aquatic deposit-feeders live on a very poor food source. The food is derived mainly from sedimenting phytodetritus, and in temperate waters like the Baltic Sea, from seasonal phytoplankton blooms. Deposit-feeders are either bulk-feeders, or selective feeders, which preferentially ingest the more organic-rich particles in the sediment, including phytodetritus, microbes and meiofauna. The soft-bottom benthos of the Baltic Sea has low species biodiversity and is dominated by a few macrobenthic species, among which the most numerous are the two deposit-feeding amphipods Monoporeia affinis and Pontoporeia femorata, and the bivalve Macoma balthica. This thesis is based on laboratory experiments on the feeding of these three species, and on the priapulid Halicryptus spinulosus. Feeding by benthic animals is often difficult to observe, but can be effectively studied by the use of tracers. Here we used the radioactive isotope 14C to label food items and to trace the organic matter uptake in the animals, while the stable isotopes 13C and 15N were used to follow feeding on aged organic matter in the sediment. The abundance of M. balthica and the amphipods tends to be negatively correlated, i.e., fewer bivalves are found at sites with dense populations of amphipods, with the known explanation that newly settled M. balthica spat are killed by the amphipods. Whether the postlarvae are just accidentally killed, or also ingested after being killed was tested by labelling the postlarvae with 14C and Rhodamine B. Both tracer techniques gave similar evidence for predation on and ingestion of postlarval bivalves. We calculated that this predation was likely to supply less than one percent of the daily carbon requirement for M. affinis, but might nevertheless be an important factor limiting recruitment of M. balthica. The two amphipods M. affinis and P. femorata are partly vertically segregated in the sediment, but whether they also feed at different depths was unknown. By adding fresh 14C-labelled algae either on the sediment surface or mixed into the sediment, we were able to distinguish surface from subsurface feeding. We found M. affinis and P. femorata to be surface and subsurface deposit-feeders, respectively. Whether the amphipods also feed on old organic matter, was studied by adding fresh 14C-labelled algae on the sediment surface, and using aged, one-year-old 13C- and 15N-labelled sediment as deep sediment. Ingestion of old organic matter, traced by the stable isotopes, differed between the two species, with a higher uptake for P. femorata, suggesting that P. femorata utilises the older, deeper-buried organic matter to a greater extent. Feeding studies with juveniles of both M. affinis and P. femorata had not been done previously. In an experiment with the same procedure and treatments as for the adults, juveniles of both amphipod species were found to have similar feeding strategies. They fed on both fresh and old sediment, with no partitioning of food resources, making them likely to be competitors for the same food resource. Oxygen deficiency has become more wide-spread in the Baltic Sea proper in the last half-century, and upwards of 70 000km2 are now devoid of macrofauna, even though part of that area does not have oxygen concentrations low enough to directly kill the macrofauna. We made week-long experiments on the rate of feeding on 14C-labelled diatoms spread on the sediment surface in different oxygen concentrations for both the amphipod species, M. balthica and H. spinulosus. The amphipods were the most sensitive to oxygen deficiency and showed reduced feeding and lower survival at low oxygen concentrations. M. balthica showed reduced feeding at the lowest oxygen concentration, but no mortality increase. The survival of H. spinulosus was unaffected, but it did not feed, showing that it is not a surface deposit-feeder. We conclude that low oxygen concentrations that are not directly lethal, but reduce food intake, may lead to starvation and death in the longer term.

Bioremediation of PAHs - Limitations and soultions

Introduction 1.1 Occurrence of polycyclic aromatic hydrocarbons (PAH) in the environment Worldwide industrial and agricultural developments have released a large number of natural and synthetic hazardous compounds into the environment due to careless waste disposal, illegal waste dumping and accidental spills. As a result, there are numerous sites in the world that require cleanup of soils and groundwater. Polycyclic aromatic hydrocarbons (PAHs) are one of the major groups of these contaminants (Da Silva et al., 2003). PAHs constitute a diverse class of organic compounds consisting of two or more aromatic rings with various structural configurations (Prabhu and Phale, 2003). Being a derivative of benzene, PAHs are thermodynamically stable. In addition, these chemicals tend to adhere to particle surfaces, such as soils, because of their low water solubility and strong hydrophobicity, and this results in greater persistence under natural conditions. This persistence coupled with their potential carcinogenicity makes PAHs problematic environmental contaminants (Cerniglia, 1992; Sutherland, 1992). PAHs are widely found in high concentrations at many industrial sites, particularly those associated with petroleum, gas production and wood preserving industries (Wilson and Jones, 1993). 1.2 Remediation technologies Conventional techniques used for the remediation of soil polluted with organic contaminants include excavation of the contaminated soil and disposal to a landfill or capping - containment - of the contaminated areas of a site. These methods have some drawbacks. The first method simply moves the contamination elsewhere and may create significant risks in the excavation, handling and transport of hazardous material. Additionally, it is very difficult and increasingly expensive to find new landfill sites for the final disposal of the material. The cap and containment method is only an interim solution since the contamination remains on site, requiring monitoring and maintenance of the isolation barriers long into the future, with all the associated costs and potential liability. A better approach than these traditional methods is to completely destroy the pollutants, if possible, or transform them into harmless substances. Some technologies that have been used are high-temperature incineration and various types of chemical decomposition (for example, base-catalyzed dechlorination, UV oxidation). However, these methods have significant disadvantages, principally their technological complexity, high cost , and the lack of public acceptance. Bioremediation, on the contrast, is a promising option for the complete removal and destruction of contaminants. 1.3 Bioremediation of PAH contaminated soil & groundwater Bioremediation is the use of living organisms, primarily microorganisms, to degrade or detoxify hazardous wastes into harmless substances such as carbon dioxide, water and cell biomass Most PAHs are biodegradable unter natural conditions (Da Silva et al., 2003; Meysami and Baheri, 2003) and bioremediation for cleanup of PAH wastes has been extensively studied at both laboratory and commercial levels- It has been implemented at a number of contaminated sites, including the cleanup of the Exxon Valdez oil spill in Prince William Sound, Alaska in 1989, the Mega Borg spill off the Texas coast in 1990 and the Burgan Oil Field, Kuwait in 1994 (Purwaningsih, 2002). Different strategies for PAH bioremediation, such as in situ , ex situ or on site bioremediation were developed in recent years. In situ bioremediation is a technique that is applied to soil and groundwater at the site without removing the contaminated soil or groundwater, based on the provision of optimum conditions for microbiological contaminant breakdown.. Ex situ bioremediation of PAHs, on the other hand, is a technique applied to soil and groundwater which has been removed from the site via excavation (soil) or pumping (water). Hazardous contaminants are converted in controlled bioreactors into harmless compounds in an efficient manner. 1.4 Bioavailability of PAH in the subsurface Frequently, PAH contamination in the environment is occurs as contaminants that are sorbed onto soilparticles rather than in phase (NAPL, non aqueous phase liquids). It is known that the biodegradation rate of most PAHs sorbed onto soil is far lower than rates measured in solution cultures of microorganisms with pure solid pollutants (Alexander and Scow, 1989; Hamaker, 1972). It is generally believed that only that fraction of PAHs dissolved in the solution can be metabolized by microorganisms in soil. The amount of contaminant that can be readily taken up and degraded by microorganisms is defined as bioavailability (Bosma et al., 1997; Maier, 2000). Two phenomena have been suggested to cause the low bioavailability of PAHs in soil (Danielsson, 2000). The first one is strong adsorption of the contaminants to the soil constituents which then leads to very slow release rates of contaminants to the aqueous phase. Sorption is often well correlated with soil organic matter content (Means, 1980) and significantly reduces biodegradation (Manilal and Alexander, 1991). The second phenomenon is slow mass transfer of pollutants, such as pore diffusion in the soil aggregates or diffusion in the organic matter in the soil. The complex set of these physical, chemical and biological processes is schematically illustrated in Figure 1. As shown in Figure 1, biodegradation processes are taking place in the soil solution while diffusion processes occur in the narrow pores in and between soil aggregates (Danielsson, 2000). Seemingly contradictory studies can be found in the literature that indicate the rate and final extent of metabolism may be either lower or higher for sorbed PAHs by soil than those for pure PAHs (Van Loosdrecht et al., 1990). These contrasting results demonstrate that the bioavailability of organic contaminants sorbed onto soil is far from being well understood. Besides bioavailability, there are several other factors influencing the rate and extent of biodegradation of PAHs in soil including microbial population characteristics, physical and chemical properties of PAHs and environmental factors (temperature, moisture, pH, degree of contamination). Figure 1: Schematic diagram showing possible rate-limiting processes during bioremediation of hydrophobic organic contaminants in a contaminated soil-water system (not to scale) (Danielsson, 2000). 1.5 Increasing the bioavailability of PAH in soil Attempts to improve the biodegradation of PAHs in soil by increasing their bioavailability include the use of surfactants , solvents or solubility enhancers.. However, introduction of synthetic surfactant may result in the addition of one more pollutant. (Wang and Brusseau, 1993).A study conducted by Mulder et al. showed that the introduction of hydropropyl-ß-cyclodextrin (HPCD), a well-known PAH solubility enhancer, significantly increased the solubilization of PAHs although it did not improve the biodegradation rate of PAHs (Mulder et al., 1998), indicating that further research is required in order to develop a feasible and efficient remediation method. Enhancing the extent of PAHs mass transfer from the soil phase to the liquid might prove an efficient and environmentally low-risk alternative way of addressing the problem of slow PAH biodegradation in soil.

Neuroglobin, Cytoglobin und Myoglobin in der Blindmaus Spalax ehrenbergi: Adaptation an „unterirdische Verhältnisse“

Hypoxie ist ein Zustand des Sauerstoffmangels, hervorgerufen durch fehlende Verfügbarkeit von Sauerstoff in der Umgebung eines Organismus oder durch pathologisch bedingte unzureichende Nutzbarkeit des Sauerstoffs von Geweben. Die Sensitivität gegenüber Hypoxie variiert enorm im Tierreich zwischen verschiedenen Phyla und Spezies. Die meisten Säugetiere sind nur unzureichend an niedrige Sauerstoffkonzentrationen angepasst, wohingegen einige unterirdisch lebende Säuger sehr resistent gegen Hypoxiestress sind. Um die molekulare Basis der Hypoxietoleranz zu bestimmen, wurden in der vorliegenden Arbeit Globine untersucht, die potenziell in der Lage sind, als respiratorische Proteine zur Hypoxietoleranz von Tieren beizutragen. Dazu wurde die Expression der Globine in der hypoxieresistenten, in Israel lebenden Blindmaus Spalax ehrenbergi mit der Genexpression in der hypoxiesensitiven Ratte (Rattus norvegicus) verglichen. In der vorliegenden Arbeit wurden die erst vor wenigen Jahren entdeckten Globine Neuroglobin und Cytoglobin untersucht, deren exakte physiologische Rolle noch unklar ist, und mit Daten des viel detaillierter untersuchten Myoglobins verglichen. Beim Vergleich der Expression von Cytoglobin und Neuroglobin in Spalax versus Ratte fällt auf, dass Neuroglobin und Cytoglobin bereits unter normoxischen Bedingungen auf mRNA- und Proteinebene in der Blindmaus um einen Faktor von mindesten 2 bis 3 verstärkt exprimiert werden. Bei Myoglobin (als dem Kontrollgen mit bekannter Funktion) konnte auf mRNA-Ebene eine noch weitaus stärkere Expression in Spalax vs. Ratte gefunden werden. Das übergreifende Phänomen der verstärkten Genexpression von Globinen in Spalax kann im Sinne einer Präadaptation an das unterirdische, häufig hypoxische Leben der Blindmaus interpretiert werden. Einen weiteren Hinweis auf eine besondere, spezialisierte Funktion von Neuroglobin in Spalax geben immunhistochemische Daten, die zeigen, dass Neuroglobin im Gehirn von Spalax im Gegensatz zur Ratte nicht nur in Neuronen, sondern auch in Gliazellen exprimiert wird. Dies impliziert Änderungen des oxidativen Stoffwechsels im Nervensystem der hypoxietoleranten Spezies. Die zellulären Expressionsmuster von Cytoglobin erscheinen hingegen in beiden Säugerspezies weitgehend identisch. Es wurde der Frage nachgegangen, ob und wie experimentell induzierte Hypoxie die Genexpression der Globine verändert. Dabei zeigten sich für Neuroglobin und Cytoglobin unterschiedliche Expressionsmuster. Neuroglobin wird unter diversen Sauerstoffmangelbedingungen sowohl in der Ratte als auch in Spalax auf mRNA- und Proteinebene herunterreguliert. Ein ähnliches Regulationsverhalten wurde auch für Myoglobin beobachtet. Die verminderte Expression von Neuroglobin (und evtl. auch Myoglobin) unter Hypoxie ist mit einer gezielten Verringerung der Sauerstoff-Speicherkapazität in Abwesenheit von O2 zu erklären. Ein weiterer denkbarer Grund könnte auch die allgemeine Tendenz sein, unter Hypoxie aus Energiespargründen den Metabolismus herunter zu regulieren. Cytoglobin, das bei normalen Sauerstoffbedingungen nur im Gehirn von Spalax (nicht jedoch in Herz und Leber) ebenfalls um Faktor 2 bis 3 stärker exprimiert wird als in der Ratte, ist mit einiger Sicherheit ebenfalls von adaptivem Nutzen für die Anpassung von Spalax an niedrige Sauerstoffbedingungen, wenngleich seine Funktion unklar bleibt. Unter Hypoxie wird die Cytoglobin-mRNA sowohl in Spalax als auch in der Ratte hochreguliert. Es konnte in der vorliegenden Arbeit dargelegt werden, dass die Expression von Cygb höchstwahrscheinlich durch den Transkriptionsfaktor Hif-1 gesteuert wird, der die molekulare Hypoxieantwort vieler Tierarten zentral steuert. In der vorliegenden Arbeit wurde ebenfalls die Expression von Ngb und Cygb im Gehirn des Hausschweins (Sus scrofa) untersucht. Diese Spezies diente in der Arbeit als weiterer hypoxiesensitiver Organismus sowie als biomedizinisch relevantes Modell für eine Operation an Säuglingen mit angeborenen Herzkrankheiten. Die Versuche haben gezeigt, dass die Gabe bestimmter Medikamente wie dem Immunsuppressivum FK506 zu einer erhöhten Ngb-Konzentration auf mRNA-Ebene führen kann, was potenziell im Zusammenhang mit beobachteten protektiven Effekten der Medikamentengabe während und nach der Herzoperation steht.

Der Einfluss von Chemotherapeutika mit Hypoxie-induzierbarer Faktor (HIF)-modulierendem Potential sowie eines Verlustes des HIF-Regulators von Hippel-Lindau (VHL) auf den Phänotyp und die Funktion dendritischer Zellen

Der Transkriptionsfaktor Hypoxie-induzierbarer Faktor (HIF) gibt dem Organismus die Möglichkeit, sich auf zellulärer Ebene an unterschiedliche Sauerstoffverhältnisse anzupassen. Vor allem Tumorzellen weisen aufgrund ihres ungeregelten Wachstums und der daraus resultierenden unzureichenden Durchblutung (hypoxisches Milieu) eine erhöhte HIF-Expression auf. Die erhöhte HIF-Expression stellt somit ein interessantes Ziel in der Tumortherapie dar. Dendritische Zellen (DCs) besitzen eine bedeutende Rolle in der Generierung und Modulierung von Antitumor-Immunantworten. Aus diesem Grund ist es überaus wichtig zu wissen, welche Effekte Antitumor-Agenzien, im Besonderen HIF-Inhibitoren, auf DCs und somit auch auf die Generierung von adäquaten Immunantworten besitzen.rnIm ersten Teil dieser Arbeit wurde aus diesem Grund der Einfluss der Antitumor-Agenzien Geldanamycin (GA) und Topotecan (TPT) auf den Phänotyp und die Funktion von DCs untersucht. Hierfür wurden Monozyten aus humanen, mononukleären, peripheren Blutzellen isoliert und unter DC-differenzierenden Konditionen kultiviert. Diese immaturen monozytenabgeleiteten DCs (Mo-DCs) wurden mithilfe eines Reifungscocktails ausgereift. Die Applikation der Antitumor-Agenzien erfolgte während der Differenzierungs- bzw. Ausreifungsphase. Abhängig vom Reifungsgrad der Mo-DCs konnte ein differentieller Einfluss von GA bzw. TPT auf die DC-Aktivierung beobachtet werden. Eine Behandlung von unstimulierten Mo-DCs mit GA resultierte in einer partiellen DC-Aktivierung basierend auf einem noch unbekannten Mechanismus. Ebenso führte eine Behandlung von unstimulierten Mo-DCs mit TPT zu einer funktionellen Aktivierung der DCs, die mit einer vermehrten AKT-Expression korrelierte. Die jeweilige Koapplikation der Antitumor-Agenzien mit dem DC-Reifungscocktail führte zu einer reduzierten DC-Aktivierung, die sich in einer verminderten NF-κB-Aktivierung, einer verringerten Oberflächenexpression der getesteten kostimulatorischen Moleküle, einer verringerten Migrationsfähigkeit und einem reduzierten Zellstimulierungspotential widerspiegelte.rnDie autosomal dominant vererbte Tumorerkrankung von Hippel-Lindau (VHL) wird häufig durch genetische Mutationen des als HIF-Negativregulator fungierenden VHL-Gens hervorgerufen. Patienten, die an dem VHL-Syndrom erkrankt sind, weisen oft benigne oder maligne Tumore und Zysten in den verschiedensten Organsystemen auf. Wie schon zuvor erwähnt, besitzen DCs eine essentielle Rolle in der Initiierung und Aufrechterhaltung von Antitumor-Immunantworten. Deshalb wurde im zweiten Abschnitt der vorliegenden Arbeit untersucht, inwieweit ein partieller Verlust von VHL Auswirkungen auf die Ausprägung desrnPhänotyps und der Funktion von DCs hat. Mittels Cre/lox-Technologie wurden transgene Mäuse mit einem heterozygoten Verlust von Exon 1 bzw. Exon 2 des VHL-Gens generiert. Aus diesen Mäusen wurden Knochenmarkszellen isoliert und unter DC-differenzierenden Konditionen kultiviert. Die immaturen knochenmarkabgeleiteten DCs (BM-DCs) wurden mit LPS ausgereift. Weder der heterozygote Verlust von Exon 1 noch von Exon 2 des VHL-Gens bewirkte eine Veränderung der Oberflächenmarkerexpression, der in vitro-Migrations- undrnEndozytosekapazität, sowie der allogenen T-Zellstimulierungskapazität. Allerdings zeigten Mäuse mit einem partiellen Verlust von Exon 2 im Vergleich zu Kontrollmäusen nach Immunisierung und Provokation mit dem Modellallergen OVA eine verminderte Atemwegshyperreaktion, die möglicherweise auf die beobachtete Abnahme der Migrationsfähigkeit in vivo und die verminderte OVA-spezifische T-Zellstimulierungskapazität der DCs zurückzuführen ist.

Outdoor production of Isochrysis galbana (T-iso) in industrial scale photobioreactors and modelling of its photosynthesis and respiration rate

Isochrysis galbana is a widely-used strain in aquaculture in spite of its low productivity. To maximize the productivity of processes based on this microalgae strain, a model was developed considering the influence of irradiance, temperature, pH and dissolved oxygen concentration on the photosynthesis and respiration rate. Results demonstrate that this strain tolerates temperatures up to 35ºC but it is highly sensitive to irradiances higher than 500 µE·m-2·s-1 and dissolved oxygen concentrations higher than 11 mg·l-1. With the researcher group of the “Universidad de Almeria”, the developed model was validated using data from an industrial-scale outdoor tubular photobioreactor demonstrating that inadequate temperature and dissolved oxygen concentrations reduce productivity to half that which is maximal, according to light availability under real outdoor conditions. The developed model is a useful tool for managing working processes, especially in the development of new processes based on this strain and to take decisions regarding optimal control strategies. Also the outdoor production of Isochrysis galbana T-iso in industrial size tubular photobioreactors (3.0 m3) has been studied. Experiments were performed modifying the dilution rate and evaluating the biomass productivity and quality, in addition to the overall performance of the system. Results confirmed that T-iso can be produced outdoor at commercial scale in continuous mode, productivities up to 20 g·m-2·day-1 of biomass rich in proteins (45%) and lipids (25%) being obtained. The utilization of this type of photobioreactors allows controlling the contamination and pH of the cultures, but daily variation of solar radiation imposes the existence of inadequate dissolved oxygen concentration and temperature at which the cells are exposed to inside the reactor. Excessive dissolved oxygen reduced the biomass productivity to 68% of maximal, whereas inadequate temperature reduces to 63% of maximal. Thus, optimally controlling these parameters the biomass productivity can be duplicated. These results confirm the potential to produce this valuable strain at commercial scale in optimally designed/operated tubular photobioreactors as a biotechnological industry.

In vitro expression of the first capsule gene of Streptococcus pneumoniae, cpsA, is associated with serotype-specific colonization prevalence and invasiveness

The polysaccharide capsule protects Streptococcus pneumoniae from phagocytosis during invasive infection, but inhibits adherence. Serotypes vary in their tendency to colonize the nasopharynx or cause invasive infection, and differences in capsule expression may play a role. Expression of the first gene of the capsule operon, cpsA, during in vitro growth of 43 clinical isolates representing 14 common pneumococcal serotypes was compared using quantitative RT-PCR. Serotypes associated with invasive infection (1, 4, 5, 7F, 8 and 14) expressed an average of twofold (P=0.0003) more cpsA than serotypes associated with nasopharyngeal colonization (6A, 6B, 9V, 15, 18C, 19F, 23F and 33). There was no difference in cpsA expression in response to growth under environmental oxygen or anaerobic conditions between the invasive and colonizing transparent strains tested: oxygen concentration did not affect cpsA expression in either the invasive or the colonizing transparent strains. Expression of cpsA at OD(600) 0.6 tended to be greater in strains with a longer lag phase during in vitro growth (P=0.07). Therefore, cpsA expression under ambient oxygen concentrations correlates with serotype-specific invasiveness and is inversely associated with the prevalence of serotype-specific carriage.

Hypoxic expansion promotes the chondrogenic potential of articular chondrocytes

For cell-based cartilage repair strategies, an ex vivo expansion phase is required to obtain sufficient numbers of cells needed for therapy. Although recent reports demonstrated the central role of oxygen for the function and differentiation of chondrocytes, a beneficial effect of low oxygen concentrations during the expansion of the cells to further improve their chondrogenic capacity has not been investigated.Therefore, freshly harvested bovine articular chondrocytes were grown in two-dimensional monolayer cultures at 1.5% and 21% O2 and redifferentiation was subsequently induced in three-dimensional micromass cultures at 1.5%, 5%, and 21% O2. Cells expanded at 1.5% O2 were characterized by low citrate synthase (aerobic energy metabolism)--and high LDH (anaerobic energy metabolism-activities,suggesting an anaerobic energy metabolism. Collagen type II mRNA was twofold higher in cells expanded at 1.5% as compared to expansion at 21% O2. Micromass cultures grown at 21% O2 showed up to a twofold increase in the tissue content of glycosaminoglycans when formed with cells expanded at 1.5% instead of 21% O2. However, no differences in the levels of transcripts and in the staining for collagen type II protein were observed in these micromass cultures. Hypoxia (1.5% and 5% O2) applied during micromass cultures gave rise to tissues with low contents of glycosaminoglycans only. In vivo, the chondrocytes are adapted to a hypoxic environment. Taking this into account, by applying 1.5% O2 in the expansion phase in the course of cell-based cartilage repair strategies, may result in a repair tissue with higher quality by increasing the content of glycosaminoglycans.

An evaluation of a Lake Houston tributary, Cypress Creek, for contamination and water quality

Introduction. Lake Houston serves as a reservoir for both recreational and drinking water for residents of Houston, Texas, and the metropolitan area. The Texas Commission on Environmental Quality (TCEQ) expressed concerns about the water quality and increasing amounts of pathogenic bacteria in Lake Houston (3). The objective of this investigation is to evaluate water quality for the presence of bacteria, nitrates, nitrites, carbon, phosphorus, dissolved oxygen, pH, turbidity, suspended solids, dissolved solids, and chlorine in Cypress Creek. The aims of this project are to analyze samples of water from Cypress Creek and to render a quantitative and graphical representation of the results. The collected information will allow for a better understanding of the aqueous environment in Cypress Creek.^ Methods. Water samples were collected in August 2009 and analyzed in the field and at UTSPH laboratory by spectrophotometry and other methods. Mapping software was utilized to develop novel maps of the sample sites using coordinates attained with the Global Positioning System (GPS). Sample sites and concentrations were mapped using Geographic Information System (GIS) software and correlated with permitted outfalls and other land use characteristic.^ Results. All areas sampled were positive for the presence of total coliform and Escherichia coli (E. coli). The presences of other water contaminants varied at each location in Cypress Creek but were under the maximum allowable limits designated by the Texas Commission on Environmental Quality. However, dissolved oxygen concentrations were elevated above the TCEQ limit of 5.0 mg/L at majority of the sites. One site had near-limit concentration of nitrates at 9.8 mg/L. Land use above this site included farm land, agricultural land, golf course, parks, residential neighborhoods, and nine permitted TCEQ effluent discharge sites within 0.5 miles upstream.^ Significance. Lake Houston and its tributary, Cypress Creek, are used as recreational waters where individuals may become exposed to microbial contamination. Lake Houston also is the source of drinking water for much of Houston/Harris and Galveston Counties. This research identified the presence of microbial contaminates in Cypress Creek above TCEQ regulatory requirements. Other water quality variables measured were in line with TCEQ regulations except for near-limit for nitrate at sample site #10, at Jarvis and Timberlake in Cypress Texas.^

Stable carbon isotope composition of benthic foraminifera from sediments of the Skagerrak, North Sea

The sediment cores 225514 and 225510 were recovered from 420 and 285 m water depth, respectively. They were investigated for their benthic foraminiferal delta13C during the last 500 years. Both cores were recovered from the southern flank of the Skagerrak. The delta13C values of Uvigerina mediterranea and other shallow infaunal species in both cores indicate that organic matter rain rates to the seafloor varied around a mean value until approximately AD 1950 after which they increased. This increase might result from changes in the North Atlantic Current System and a co-occurring persistently high North Atlantic Oscillation index state in the 1980s to 1990s, rather than from anthropogenic eutrophication. Using delta13C mean values of multiple species, we reconstruct delta13C gradients of dissolved inorganic carbon (DIC) within pore waters for the time periods AD 1500 to 1950 and AD 1950 to 2000. The calculated delta13CDIC ranges, interpreted as indicating total organic matter remineralization due to respiration, are generally bigger in Core 225514 than in Core 225510. Since mean delta13C values of U. mediterranea suggest that organic matter rain rates were similar at both locations, differences in total organic matter remineralization are attributed to differing oxygen availability. However, oxygen concentrations in the overlying bottom water masses are not likely to have differed significantly. Thus, we suggest that organic matter remineralization was controlled by oxygen availability within the sediments, reflecting strong differences in sedimentation rates at the two investigated core sites. Based on the assumptions that tests of benthic foraminiferal species inhabiting the same microhabitat depth should show equal delta13C values unless they are affected by vital effects and that Globobulimina turgida records pore water delta13CDIC, we estimate microhabitat-corrected vital effects for several species with respect to G. turgida: >0.7 per mil for Cassidulina laevigata, >1.3 per mil for Hyalinea balthica, and >0.7 per mil for Melonis barleeanus. Melonis zaandami seems to closely record pore water delta13CDIC.

(Table 3) Stable isotope composition of sof t tissues of specimens from the Sea of Okhotsk

We discovered and investigated several cold-seep sites in four depth zones of the Sea of Okhotsk off Northeast Sakhalin: outer shelf (160-250 m), upper slope (250-450 m), intermediate slope (450-800 m), and Derugin Basin (1450-1600 m). Active seepage of free methane or methane-rich fluids was detected in each zone. However, seabed photography and sampling revealed that the number of chemoautotrophic species decreases dramatically with decreasing water depth. At greatest depths in the Derugin Basin, the seeps were inhabited by bacterial mats and bivalves of the families Vesicomyidae (Calyptogena aff. pacifica, C. rectimargo, Archivesica sp.), Solemyidae (Acharax sp.) and Thyasiridae (Conchocele bisecta). In addition, pogonophoran tubeworms of the family Sclerolinidae were found in barite edifices. At the shallowest sites, on the shelf at 160 m, the seeps lack chemoautotrophic macrofauna; their locations were indicated only by the patchy occurrence of bacterial mats. Typical seep-endemic metazoans with chemosynthetic symbionts were confined to seep sites at depths below 370 m. A comparative analysis of the structure of seep and background communities suggests that differences in predation pressure may be an important determinant of this pattern. The abundance of predators such as carnivorous brachyurans and asteroids, which can invade seeps from adjacent habitats and efficiently prey on sessile seep bivalves, decreased very pronouncedly with depth. We conclude from the obvious correlation with the conspicuous pattern in the distribution of seep assemblages that, on the shelf and at the upper slope, predator pressure may be high enough to effectively impede any successful settlement of viable populations of seep-endemic metazoans. However, there was also evidence that other depth-related factors, such as bottom-water current, sedimentary regimes, oxygen concentrations and the supply of suitable settling substrates, may additionally regulate the distribution of seep fauna in the area. As a consequence of the pronounced pattern in the distribution of seep communities, their ecological significance as food sources of surrounding background fauna increased with water depth. Isotopic analyses suggest that in the Derugin Basin seep colonists feed on chemoautotrophic seep organisms, either directly or by preying on metazoans with chemosynthetic symbionts. In contrast, seep organisms apparently do not contribute to the nutrition of the adjacent background fauna on the shelf and at the slope. In this area, elevated epifaunal abundances at seep sites were caused primarily by the availability of suitable settling substrates rather than by an enrichment of food supply.

Distribution of organic carbon in surface sediments covered during SONNE cruise SO184

Sediments were sampled and oxygen profiles of the water column were determined in the Indian Ocean off west and south Indonesia in order to obtain information on the production, transformation, and accumulation of organic matter (OM). The stable carbon isotope composition (d13Corg) in combination with C/N ratios depicts the almost exclusively marine origin of sedimentary organic matter in the entire study area. Maximum concentrations of organic carbon (Corg) and nitrogen (N) of 3.0% and 0.31%, respectively, were observed in the northern Mentawai Basin and in the Savu and Lombok basins. Minimum d15N values of 3.7 per mil were measured in the northern Mentawai Basin, whereas they varied around 5.4 per mil at stations outside this region. Minimum bottom water oxygen concentrations of 1.1 mL L**1, corresponding to an oxygen saturation of 16.1%, indicate reduced ventilation of bottom water in the northern Mentawai Basin. This low bottom water oxygen reduces organic matter decomposition, which is demonstrated by the almost unaltered isotopic composition of nitrogen during early diagenesis. Maximum Corg accumulation rates (CARs) were measured in the Lombok (10.4 g C m**-2 yr**-1) and northern Mentawai basins (5.2 g C m**-2 yr**-1). Upwelling-induced high productivity is responsible for the high CAR off East Java, Lombok, and Savu Basins, while a better OM preservation caused by reduced ventilation contributes to the high CAR observed in the northern Mentawai Basin. The interplay between primary production, remineralisation, and organic carbon burial determines the regional heterogeneity. CAR in the Indian Ocean upwelling region off Indonesia is lower than in the Peru and Chile upwellings, but in the same order of magnitude as in the Arabian Sea, the Benguela, and Gulf of California upwellings, and corresponds to 0.1-7.1% of the global ocean carbon burial. This demonstrates the relevance of the Indian Ocean margin off Indonesia for the global OM burial.

(Table 2) Similarity Indexes (Pearson's correlation coefficient) of the silicoflagellate assemblages of IODP Exp302

The silicoflagellate and ebridian assemblages in early middle Eocene Arctic cores obtained by IODP Expedition 302 (ACEX) were studied in order to decipher the paleoceanography of the upper water column. The assemblages in Lithologic Unit 2 (49.7-45.1 Ma), one of the biosiliceous intervals, were usually endemic as compared to the assemblages that occurred outside of the Arctic Ocean. The presence of these endemic assemblages is probably due to a unique environmental setting, controlled by the degree of mixing between the low-salinity Arctic waters and relatively high salinity waters supplied from outside the Arctic Ocean, such as the Atlantic and possibly the Western Siberian Sea. Using the basin-to-basin fractionation model, the early middle Eocene Arctic Ocean corresponds to an estuarine circulation type, which includes the modern-day Black Sea. The abundant down-core occurrence of ebridians strongly suggests the past presence of low-salinity waters, and may indicate that low oxygen concentrations prevailed in the euphotic layer, on the basis of the ecology of the modern ebridian Hermesinum adriaticum.