Cytokine secretion via cholesterol-rich lipid raft-associated SNAREs at the phagocytic cup

Lipopolysaccharide-activated macrophages rapidly synthesize and secrete tumor necrosis factor alpha(TNF alpha) to prime the immune system. Surface delivery of membrane carrying newly synthesized TNF alpha is controlled and limited by the level of soluble N-ethylmaleimide-sensitive factor attachment protein receptor ( SNARE) proteins syntaxin 4 and SNAP-23. Many functions in immune cells are coordinated from lipid rafts in the plasma membrane, and we investigated a possible role for lipid rafts in TNF alpha trafficking and secretion. TNF alpha surface delivery and secretion were found to be cholesterol-dependent. Upon macrophage activation, syntaxin 4 was recruited to cholesterol-dependent lipid rafts, whereas its regulatory protein, Munc18c, was excluded from the rafts. Syntaxin 4 in activated macrophages localized to discrete cholesterol-dependent puncta on the plasma membrane, particularly on filopodia. Imaging the early stages of TNF alpha surface distribution revealed these puncta to be the initial points of TNF alpha delivery. During the early stages of phagocytosis, syntaxin 4 was recruited to the phagocytic cup in a cholesterol-dependent manner. Insertion of VAMP3-positive recycling endosome membrane is required for efficient ingestion of a pathogen. Without this recruitment of syntaxin 4, it is not incorporated into the plasma membrane, and phagocytosis is greatly reduced. Thus, relocation of syntaxin 4 into lipid rafts in macrophages is a critical and rate-limiting step in initiating an effective immune response.

A role for the phagosome in cytokine secretion

Membrane traffic in activated macrophages is required for two critical events in innate immunity: proinflammatory cytokine secretion and phagocytosis of pathogens. We found a joint trafficking pathway linking both actions, which may economize membrane transport and augment the immune response. Tumor necrosis factor α (TNFα) is trafficked from the Golgi to the recycling endosome (RE), where vesicle-associated membrane protein 3 mediates its delivery to the cell surface at the site of phagocytic cup formation. Fusion of the RE at the cup simultaneously allows rapid release of TNFα and expands the membrane for phagocytosis.

Caractérisation moléculaire de la modulation spatio-temporelle des fonctions du phagosome

La phagocytose est un processus par lequel des cellules spécialisées du système immunitaire comme les macrophages ingèrent des microorganismes envahisseurs afin de les détruire. Les microbes phagocytés se retrouvent dans un compartiment intracellulaire nommé le phagosome, qui acquiert graduellement de nombreuses molécules lui permettant de se transformer en phagolysosome possédant la capacité de tuer et dégrader son contenu. L’utilisation de la protéomique a permis de mettre en évidence la présence de microdomaines (aussi nommés radeaux lipidiques ou radeaux membranaires) sur les phagosomes des macrophages. Notre équipe a démontré que ces radeaux exercent des fonctions cruciales au niveau de la membrane du phagosome. D’abord nous avons observé que la survie du parasite intracellulaire L. donovani est possible dans un phagosome dépourvu de radeaux lipidiques. Parallèlement nous avons constaté qu’un mutant de L. donovani n’exprimant pas de LPG à sa surface(LPG-) est rapidement tué dans un phagosome arborant des radeaux membranaires. Pour comprendre le mécanisme de perturbation des microdomaines du phagosome par la molécule LPG, nous avons provoqué la phagocytose de mutants LPG- du parasite et comparé par microscopie les différences avec le parasite de type sauvage. Nous avons ainsi démontré que le LPG de L. donovani est nécessaire et suffisant au parasite pour empêcher la maturation normale du phagosome. Nous avons également découvert que la molécule LPG permet d’empêcher la formation des radeaux lipidiques sur le phagosome et peut aussi désorganiser les radeaux lipidiques préexistants. Enfin, nous avons montré que l’action de LPG est proportionnelle au nombre d’unités répétitives de sucres (Gal(β1,4)-Manα1-PO4) qui composent cette molécule. Nos travaux ont démontré pour la première fois le rôle important de ces sous-domaines membranaires dans la maturation du phagosome. De plus, nos conclusions seront des pistes à suivre au cours des études cliniques ayant pour but d’enrayer la leishmaniose. Le second objectif de ce travail consistait à effectuer la caractérisation des radeaux lipidiques par une analyse protéomique et lipidomique à l’aide de la spectrométrie de masse. Nous avons ainsi entrepris l’identification systématique des protéines présentes dans les radeaux membranaires des phagosomes et ce, à trois moments clés de leurmaturation. Le traitement des phagosomes purifiés avec un détergent nous a permis d’isoler les «Detergent Resistent Membranes» (DRMs) des phagosomes, qui sont l’équivalent biochimique des radeaux membranaires. Nous avons ainsi établi une liste de 921 protéines associées au phagosome, dont 352 sont présentes dans les DRMs. Les protéines du phagosome sont partagées presque également entre trois tendances cinétiques (augmentation, diminution et présence transitoire). Cependant, une analyse plus spécifique des protéines des DRMs démontre qu’une majorité d’entre elles augmentent en fonction de la maturation. Cette observation ainsi que certains de nos résultats montrent que les radeaux lipidiques des phagosomes précoces sont soit très peu nombreux, soit pauvres en protéines, et qu’ils sont recrutés au cours de la maturation du phagosome. Nous avons aussi analysé les phospholipides du phagosome et constaté que la proportion entre chaque classe varie lors de la maturation. De plus, en regardant spécifiquement les différentes espèces de phospholipides nous avons constaté que ce ne sont pas uniquement les espèces majoritaires de la cellule qui dominent la composition de la membrane du phagosome. L’ensemble de nos résultats a permis de mettre en évidence plusieurs fonctions potentielles des radeaux lipidiques, lesquelles sont essentielles à la biogenèse des phagolysosomes (signalisation, fusion membranaire, action microbicide, transport transmembranaire, remodelage de l’actine). De plus, la cinétique d’acquisition des protéines de radeaux lipidiques indique que ceux-ci exerceraient leurs fonctions principalement au niveau des phagosomes ayant atteint un certain niveau de maturation. L’augmentation du nombre de protéines des radeaux membranaires qui s’effectue durant la maturation du phagosome s’accompagne d’une modulation des phospholipides, ce qui laisse penser que les radeaux membranaires se forment graduellement sur le phagosome et que ce ne sont pas seulement les protéines qui sont importées.

A role for the phagosome in cytokine secretion

Membrane traffic in activated macrophages is required for two critical events in innate immunity: proinflammatory cytokine secretion and phagocytosis of pathogens. We found a joint trafficking pathway linking both actions, which may economize membrane transport and augment the immune response. Tumor necrosis factor alpha (TNF alpha) is trafficked from the Golgi to the recycling endosome (RE), where vesicle-associated membrane protein 3 mediates its delivery to the cell surface at the site of phagocytic cup formation. Fusion of the RE at the cup simultaneously allows rapid release of TNF alpha and expands the membrane for phagocytosis.

New particle formation and growth at a remote, sub-tropical coastal location

A month-long intensive measurement campaign was conducted in March/April 2007 at Agnes Water, a remote coastal site just south of the Great Barrier Reef on the east coast of Australia. Particle and ion size distributions were continuously measured during the campaign. Coastal nucleation events were observed in clean, marine air masses coming from the south-east on 65% of the days. The events usually began at ~10:00 local time and lasted for 1-4 hrs. They were characterised by the appearance of a nucleation mode with a peak diameter of ~10 nm. The freshly nucleated particles grew within 1-4 hrs up to sizes of 20-50 nm. The events occurred when solar intensity was high (~1000 W m-2) and RH was low (~60%). Interestingly, the events were not related to tide height. The volatile and hygroscopic properties of freshly nucleated particles (17-22.5 nm), simultaneously measured with a volatility-hygroscopicity-tandem differential mobility analyser (VH-TDMA), were used to infer chemical composition. The majority of the volume of these particles was attributed to internally mixed sulphate and organic components. After ruling out coagulation as a source of significant particle growth, we conclude that the condensation of sulphate and/or organic vapours was most likely responsible for driving particle growth during the nucleation events. We cannot make any direct conclusions regarding the chemical species that participated in the initial particle nucleation. However, we suggest that nucleation may have resulted from the photo-oxidation products of unknown sulphur or organic vapours emitted from the waters of Hervey Bay, or from the formation of DMS-derived sulphate clusters over the open ocean that were activated to observable particles by condensable vapours emitted from the nutrient rich waters around Fraser Island or Hervey Bay. Furthermore, a unique and particularly strong nucleation event was observed during northerly wind. The event began early one morning (08:00) and lasted almost the entire day resulting in the production of a large number of ~80 nm particles (average modal concentration during the event was 3200 cm-3). The Great Barrier Reef was the most likely source of precursor vapours responsible for this event.

Long-term trends in fine particle number concentrations in the urban atmosphere of Brisbane : the relevance of traffic emissions and new particle formation

The measurement of submicrometre (< 1.0 m) and ultrafine particles (diameter < 0.1 m) number concentration have attracted attention since the last decade because the potential health impacts associated with exposure to these particles can be more significant than those due to exposure to larger particles. At present, ultrafine particles are not regularly monitored and they are yet to be incorporated into air quality monitoring programs. As a result, very few studies have analysed their long-term and spatial variations in ultrafine particle concentration, and none have been in Australia. To address this gap in scientific knowledge, the aim of this research was to investigate the long-term trends and seasonal variations in particle number concentrations in Brisbane, Australia. Data collected over a five-year period were analysed using weighted regression models. Monthly mean concentrations in the morning (6:00-10:00) and the afternoon (16:00-19:00) were plotted against time in months, using the monthly variance as the weights. During the five-year period, submicrometre and ultrafine particle concentrations increased in the morning by 105.7% and 81.5% respectively whereas in the afternoon there was no significant trend. The morning concentrations were associated with fresh traffic emissions and the afternoon concentrations with the background. The statistical tests applied to the seasonal models, on the other hand, indicated that there was no seasonal component. The spatial variation in size distribution in a large urban area was investigated using particle number size distribution data collected at nine different locations during different campaigns. The size distributions were represented by the modal structures and cumulative size distributions. Particle number peaked at around 30 nm, except at an isolated site dominated by diesel trucks, where the particle number peaked at around 60 nm. It was found that ultrafine particles contributed to 82%-90% of the total particle number. At the sites dominated by petrol vehicles, nanoparticles (< 50 nm) contributed 60%-70% of the total particle number, and at the site dominated by diesel trucks they contributed 50%. Although the sampling campaigns took place during different seasons and were of varying duration these variations did not have an effect on the particle size distributions. The results suggested that the distributions were rather affected by differences in traffic composition and distance to the road. To investigate the occurrence of nucleation events, that is, secondary particle formation from gaseous precursors, particle size distribution data collected over a 13 month period during 5 different campaigns were analysed. The study area was a complex urban environment influenced by anthropogenic and natural sources. The study introduced a new application of time series differencing for the identification of nucleation events. To evaluate the conditions favourable to nucleation, the meteorological conditions and gaseous concentrations prior to and during nucleation events were recorded. Gaseous concentrations did not exhibit a clear pattern of change in concentration. It was also found that nucleation was associated with sea breeze and long-range transport. The implications of this finding are that whilst vehicles are the most important source of ultrafine particles, sea breeze and aged gaseous emissions play a more important role in secondary particle formation in the study area.

The mechanism of breath aerosol formation

Background: Aerosol production during normal breathing is often attributed to turbulence in the respiratory tract. That mechanism is not consistent with a high degree of asymmetry between aerosol production during inhalation and exhalation. The objective was to investigate production symmetry during breathing. Methods: The aerosol size distribution in exhaled breath was examined for different breathing patterns including normal breathing, varied breath holding periods and contrasting inhalation and exhalation rates. The aerosol droplet size distribution measured in the exhaled breath was examined in real time using an aerodynamic particle sizer. Results and Conclusions: The dependence of the particle concentration decay rate on diameter during breath holding was consistent with gravitational settling in the alveolar spaces. Also, deep exhalation resulted in a 4 to 6 fold increase in concentration and rapid inhalation produced a further 2 to 3 fold increase in concentration. In contrast rapid exhalation had little effect on the measured concentration. A positive correlation of the breath aerosol concentration with subject age was observed. The results were consistent with the breath aerosol being produced through fluid film rupture in the respiratory bronchioles in the early stages of inhalation and the resulting aerosol being drawn into the alveoli and held before exhalation. The observed asymmetry of production in the breathing cycle with very little aerosol being produced during exhalation, is inconsistent with the widely assumed turbulence induced aerosolization mechanism.