Mitochondrial dysfunction leads to NOX activation: A novel mechanism to maintain high glycolysis in cancer cells

Increased glycolysis and oxidative stress are common features of cancer cells. These metabolic alterations are associated with mitochondrial dysfunction and can be caused by mitochondrial DNA (mtDNA) mutations, oncogenic signals, loss of tumor suppressor, and tumor tissue hypoxia. It is well established that mitochondria play central roles in energy metabolism, maintenance of redox balance, and regulation of apoptosis. However, the biochemical and molecular mechanisms that maintain high glycolysis in cancer cells (the Warburg effect) with mitochondrial dysfunction and oxidative stress remain to be determined. The major goals of this study were to establish a unique experimental system in which the mitochondrial respiratory function can be regulated as desired, and to use this system to investigate the mechanistic link between mitochondrial dysfunction and the Warburg effect along with oxidative stress in cancer cells. To achieve these goals, I have established a tetracycline-inducible system in which a dominant negative form of mitochondrial DNA polymerase y (POLGdn) expression could be regulated by tetracycline; thus controlling mitochondrial respiratory function. Using this cell system, I demonstrated that POLGdn expression resulted in mitochondrial dysfunction through decreasing mtDNA content, depletion of mtDNA encoded mRNA and protein expression. This process was mediated by TFAM proteasome degradation. Mitochondrial dysfunction mediated by POLGdn expression led to a significant increase in cellular glycolysis and oxidative stress. Surprisingly, mitochondrial dysfunction also resulted in increased NAD(P)H oxidase (NOX) enzyme activity, which was shown to be essential for maintaining high glycolysis. Chemical Inhibition of NOX activity by diphenyliodonium (DPI) preferentially impacted the survival of mitochondrial defective cells. The colon cancer HCT116-/- cells that have lost transcriptional regulation of the mitochondrial assembling enzyme SCO2, leading to compromised mitochondrial respiratory function, were found to have increased NOX activity and were highly sensitive to DPI treatment. Ovarian epithelial cells with Ras transformation also exhibited an increase in NOX gene expression and NOX enzyme activity, rendering the cells sensitive to DPI inhibition especially under hypoxic condition. These data together suggest that NOX plays a novel role in maintaining high glycolysis in cancer cells with mitochondrial defects, and that NOX may be a potential target for cancer therapy. ^

El cuerpo femenino, el sexo y la muerte en las representaciones de la política y la ciudad : Nox de Thomas Hettche, en contraste con tres relatos de la literatura argentina

Fil: Piccioni, María Laura. Universidad Nacional de La Plata. Facultad de Humanidades y Ciencias de la Educación; Argentina.

High-resolution in situ oxygen microprofiles, porewater and solid phase geochemistry from the Crimean shelf (Black Sea) from Maria S. Merian cruise MSM15/1

The outer western Crimean shelf of the Black Sea is a natural laboratory to investigate effects of stable oxic versus varying hypoxic conditions on seafloor biogeochemical processes and benthic community structure. Bottom-water oxygen concentrations ranged from normoxic (175 µmol O2/L) and hypoxic (< 63 µmol O2/L) or even anoxic/sulfidic conditions within a few kilometers' distance. Variations in oxygen concentrations between 160 and 10 µmol/L even occurred within hours close to the chemocline at 134 m water depth. Total oxygen uptake, including diffusive as well as fauna-mediated oxygen consumption, decreased from 15 mmol/m**2/d on average in the oxic zone, to 7 mmol/m**2/d on average in the hypoxic zone, correlating with changes in macrobenthos composition. Benthic diffusive oxygen uptake rates, comprising respiration of microorganisms and small meiofauna, were similar in oxic and hypoxic zones (on average 4.5 mmol/m**2/d), but declined to 1.3 mmol/m**2/d in bottom waters with oxygen concentrations below 20 µmol/L. Measurements and modeling of porewater profiles indicated that reoxidation of reduced compounds played only a minor role in diffusive oxygen uptake under the different oxygen conditions, leaving the major fraction to aerobic degradation of organic carbon. Remineralization efficiency decreased from nearly 100 % in the oxic zone, to 50 % in the oxic-hypoxic zone, to 10 % in the hypoxic-anoxic zone. Overall, the faunal remineralization rate was more important, but also more influenced by fluctuating oxygen concentrations, than microbial and geochemical oxidation processes.

El cuerpo femenino, el sexo y la muerte en las representaciones de la política y la ciudad : Nox de Thomas Hettche, en contraste con tres relatos de la literatura argentina

Fil: Piccioni, María Laura. Universidad Nacional de La Plata. Facultad de Humanidades y Ciencias de la Educación; Argentina.

Processed CO2/O2 Float data from 4 deployments near Cape Verde Island (11/2010 - 06/2011)

In recent years, profiling floats, which form the basis of the successful international Argo observatory, are also being considered as platforms for marine biogeochemical research. This study showcases the utility of floats as a novel tool for combined gas measurements of CO2 partial pressure (pCO2) and O2. These float prototypes were equipped with a small-sized and submersible pCO2 sensor and an optode O2 sensor for highresolution measurements in the surface ocean layer. Four consecutive deployments were carried out during November 2010 and June 2011 near the Cape Verde Ocean Observatory (CVOO) in the eastern tropical North Atlantic. The profiling float performed upcasts every 31 h while measuring pCO2, O2, salinity, temperature, and hydrostatic pressure in the upper 200 m of the water column. To maintain accuracy, regular pCO2 sensor zeroings at depth and surface, as well as optode measurements in air, were performed for each profile. Through the application of data processing procedures (e.g., time-lag correction), accuracies of floatborne pCO2 measurements were greatly improved (10-15 µatm for the water column and 5 µatm for surface measurements). O2 measurements yielded an accuracy of 2 µmol/kg. First results of this pilot study show the possibility of using profiling floats as a platform for detailed and unattended observations of the marine carbon and oxygen cycle dynamics.

Nitrogen isotope gradients off Peru and Ecuador related to upwelling, productivity, nutrient uptake and oxygen deficiency

We present new nitrogen isotope data from the water column and surface sediments for paleo-proxy validation collected along the Peruvian and Ecuadorian margins between 1°N and 18°S. Productivity proxies in the bulk sediment (organic carbon, total nitrogen, biogenic opal, C37 alkenone concentrations) and 15N/14N ratios were measured at more than 80 locations within and outside the present-day Peruvian oxygen minimum zone (OMZ). Microbial N-loss to N2 in subsurface waters under O2 deficient conditions leaves a characteristic 15N-enriched signal in underlying sediments. We find that phytoplankton nutrient uptake in surface waters within the high nutrient, low chlorophyll (HNLC) regions of the Peruvian upwelling system influences the sedimentary signal as well. How the d15Nsed signal is linked to these processes is studied by comparing core-top values to the 15N/14N of nitrate and nitrite (d15N[NOx]) in the upper 200 m of the water column. Between 1°N and 10°S, subsurface O2 is still high enough to suppress N-loss keeping d15NNOx values relatively low in the subsurface waters. However d15N[NOx] values increase toward the surface due to partial nitrate utilization in the photic zone in this HNLC portion of the system. d15N[sed] is consistently lower than the isotopic signature of upwelled [NO3]-, likely due to the corresponding production of 15N depleted organic matter. Between 10°S and 15°S, the current position of perennial upwelling cells, HNLC conditions are relaxed and biological production and near-surface phytoplankton uptake of upwelled [NO3]- are most intense. In addition, subsurface O2 concentration decreases to levels sufficient for N-loss by denitrification and/or anammox, resulting in elevated subsurface d15N[NOx] values in the source waters for coastal upwelling. Increasingly higher production southward is reflected by various productivity proxies in the sediments, while the north-south gradient towards stronger surface [NO3]- utilization and subsurface N-loss is reflected in the surface sediment 15N/14N ratios. South of 10°S, d15N[sed] is lower than maximum water column d15N[NOx] values most likely because only a portion of the upwelled water originates from the depths where highest d15N[NOx] values prevail. Though the enrichment of d15N[NOx] in the subsurface waters is unambiguously reflected in d15N[sed] values, the magnitude of d15N[sed] enrichment depends on both the depth of upwelled waters and high subsurface d15N[NOx] values produce by N-loss. Overall, the degree of N-loss influencing subsurface d15N[NOx] values, the depth origin of upwelled waters, and the degree of near-surface nitrate utilization under HNLC conditions should be considered for the interpretation of paleo d15N[sed] records from the Peruvian oxygen minimum zone.