A negative regulator mediates quorum-sensing control of exopolysaccharide production in Pantoea stewartii subsp. stewartii.

Classical quorum-sensing (autoinduction) regulation, as exemplified by the lux system of Vibrio fischeri, requires N-acyl homoserine lactone (AHL) signals to stimulate cognate transcriptional activators for the cell density-dependent expression of specific target gene systems. For Pantoea stewartii subsp. stewartii, a bacterial pathogen of sweet corn and maize, the extracellular polysaccharide (EPS) stewartan is a major virulence factor, and its production is controlled by quorum sensing in a population density-dependent manner. Two genes, esaI and esaR, encode essential regulatory proteins for quorum sensing. EsaI is the AHL signal synthase, and EsaR is the cognate gene regulator. esaI, DeltaesaR, and DeltaesaI-esaR mutations were constructed to establish the regulatory role of EsaR. We report here that strains containing an esaR mutation produce high levels of EPS independently of cell density and in the absence of the AHL signal. Our data indicate that quorum-sensing regulation in P. s. subsp. stewartii, in contrast to most other described systems, uses EsaR to repress EPS synthesis at low cell density, and that derepression requires micromolar amounts of AHL. In addition, derepressed esaR strains, which synthesize EPS constitutively at low cell densities, were significantly less virulent than the wild-type parent. This finding suggests that quorum sensing in P. s. subsp. stewartii may be a mechanism to delay the expression of EPS during the early stages of infection so that it does not interfere with other mechanisms of pathogenesis.

The molecular mechanisms of sensing nucleoside analogue-induced DNA damage

Nucleoside analogues are antimetabolites effective in the treatment of a wide variety of solid tumors and hematological malignancies. Upon being metabolized to their active triphosphate form, these agents are incorporated into DNA during replication or excision repair synthesis. Because DNA polymerases have a greatly decreased affinity for primers terminated by most nucleoside analogues, their incorporation causes stalling of replication forks. The molecular mechanisms that recognize blocked replication may contribute to drug resistance but have not yet been elucidated. Here, several molecules involved in sensing nucleoside analogue-induced stalled replication forks have been identified and examined for their contribution to drug resistance. ^ The phosphorylation of the DNA damage sensor, H2AX, was characterized in response to nucleoside analogues and found to be dependent on both time and drug concentration. This response was most evident in the S-phase fraction and was associated with an inhibition of DNA synthesis, S-phase accumulation, and activation of the S-phase checkpoint pathway (Chk1-Cdc25A-Cdk2). Exposure of the Chk1 inhibitor, 7-hydroxystaurosporine (UCN-01), to cultures previously treated with nucleoside analogues caused increased apoptosis, clonogenic death, and a further log-order increase in H2AX phosphorylation, suggesting enhanced DNA damage. Ataxia-telangiectasia mutated (ATM) has been identified as a key DNA damage signaling kinase for initiating cell cycle arrest, DNA repair, and apoptosis while the Mre11-Rad50-Nbs1 (MRN) complex is known for its functions in double-strand break repair. Activated ATM and the MRN complex formed distinct nuclear foci that colocalized with phosphorylated H2AX after inhibition of DNA synthesis by the nucleoside analogues, gemcitabine, ara-C, and troxacitabine. Since double-strand breaks were undetectable, this response was likely due to stalling of replication forks. A similar DNA damage response was observed in human lymphocytes after exposure to ionizing radiation and in acute myelogenous leukemia blasts during therapy with the ara-C prodrug, CP-4055. Deficiencies in ATM, Mre11, and Rad50 led to a two- to five-fold increase in gemcitabine sensitivity, suggesting that these molecules contribute to drug resistance. Based on these results, a model is proposed for the sensing of nucleoside analogue-induced stalled replication forks that includes H2AX, ATM, and the Mre11-Rad50-Nbs1 complex. ^

A role for p53 in sensing DNA damage and triggering apoptotic responses to anticancer agents

The p53 tumor suppressor protein plays a major role in cellular responses to anticancer agents that target DNA. DNA damage triggers the accumulation of p53, resulting in the transactivation of genes, which induce cell cycle arrest to allow for repair of the damaged DNA, or signal apoptosis. The exact role that p53 plays in sensing DNA damage and the functional consequences remain to be investigated. The main goal of this project was to determine if p53 is directly involved in sensing DNA damage induced by anticancer agents and in mediating down-stream cellular responses. This was tested in two experimental models of DNA damage: (1) DNA strand termination caused by anticancer nucleoside analogs and (2) oxidative DNA damage induced by reactive oxygen species (ROS). Mobility shift assays demonstrated that p53 and DNA-PK/Ku form a complex that binds DNA containing the anticancer nucleoside analog gemcitabine monophosphate in vitro. Binding of the p53-DNA-PK/Ku complex to the analog-containing DNA inhibited DNA strand elongation. Furthermore, treatment of cells with gemcitabine resulted in the induction of apoptosis, which was associated with the accumulation of p53 protein, its phosphorylation, and nuclear localization, suggesting the activation of p53 to trigger apoptosis following gemcitabine induced DNA strand termination. The role of p53 as a DNA damage sensor was further demonstrated in response to oxidative DNA damage. Protein pull-down assays demonstrated that p53 complexes with OGG1 and APE, and binds DNA containing the oxidized DNA base 8-oxoG. Importantly, p53 enhances the activities of APE and OGG1 in excising the 8-oxoG residue as shown by functional assays in vitro. This correlated with the more rapid removal of 8-oxoG from DNA in intact cells with wild-type p53 exposed to exogenous ROS stress. Interestingly, persistent exposure to ROS resulted in the accelerated onset of apoptosis in cells with wild-type p53 when compared to isogenic cells lacking p53. Apoptosis in p53+/+ cells was associated with accumulation and phosphorylation of p53 and its nuclear localization. Taken together, these results indicate that p53 plays a key role in sensing DNA damage induced by anticancer nucleoside analogs and ROS, and in triggering down-stream apoptotic responses. This study provides new mechanistic insights into the functions of p53 in cellular responses to anticancer agents. ^

Radiance, irradiance, and remote sensing reflectance during the North Sea Coast Harmful Algal Bloom (NORCOHAB II) HEINCKE cruise HE302

In this study four data quality flags are presented for automated and unmanned above-water hyperspectral optical measurements collected underway in the North Sea, The Minch, Irish Sea and Celtic Sea in April/May 2009. Coincident to these optical measurements a DualDome D12 (Mobotix, Germany) camera system was used to capture sea surface and sky images. The first three flags are based on meteorological conditions, to select erroneous incoming solar irradiance (ES) taken during dusk, dawn, before significant incoming solar radiation could be detected or under rainfall. Furthermore, the relative azimuthal angle of the optical sensors to the sun is used to identify possible sunglint free sea surface zones. A total of 629 spectra remained after applying the meteorological masks (first three flags). Based on this dataset, a fourth flag for sunglint was generated by analysing and evaluating water leaving radiance (LW) and remote sensing reflectance (RRS) spectral behaviour in the presence and absence of sunglint salient in the simultaneously available sea surface images. Spectra conditions satisfying "mean LW (700-950 nm) < 2 mW/m**2/nm/Sr" or alternatively "minimum RRS (700-950 nm) < 0.010/Sr", mask the most measurements affected by sunglint, providing efficient flagging of sunglint in automated quality control. It is confirmed that valid optical measurements can be performed 0° <= theta <= 360° although 90° <= theta <= 135° is recommended.

(Table 1) Basin area, average late-summer speedup, number of sinks and runoff of West Greenland Ice Sheet catchments

We use interferometric synthetic aperture radar observations recorded in a land-terminating sector of western Greenland to characterise the ice sheet surface hydrology and to quantify spatial variations in the seasonality of ice sheet flow. Our data reveal a non-uniform pattern of late-summer ice speedup that, in places, extends over 100 km inland. We show that the degree of late-summer speedup is positively correlated with modelled runoff within the 10 glacier catchments of our survey, and that the pattern of late-summer speedup follows that of water routed at the ice sheet surface. In late-summer, ice within the largest catchment flows on average 48% faster than during winter, whereas changes in smaller catchments are less pronounced. Our observations show that the routing of seasonal runoff at the ice sheet surface plays an important role in shaping the magnitude and extent of seasonal ice sheet speedup.

Digital elevation model (DEM) of the ice sheet in western Dronning Maud Land, Antarctica

In this paper, a new digital elevation model (DEM) is derived for the ice sheet in western Dronning Maud Land, Antarctica. It is based on differential interferometric synthetic aperture radar (SAR) from the European Remote Sensing 1/2 (ERS-1/2) satellites, in combination with ICESat's Geoscience Laser Altimeter System (GLAS). A DEM mosaic is compiled out of 116 scenes from the ERS-1 ice phase in 1994 and the ERS-1/2 tandem mission between 1996 and 1997 with the GLAS data acquired in 2003 that served as ground control. Using three different SAR processors, uncertainties in phase stability and baseline model, resulting in height errors of up to 20 m, are exemplified. Atmospheric influences at the same order of magnitude are demonstrated, and corresponding scenes are excluded. For validation of the DEM mosaic, covering an area of about 130,000 km**2 on a 50-m grid, independent ICESat heights (2004-2007), ground-based kinematic GPS (2005), and airborne laser scanner data (ALS, 2007) are used. Excluding small areas with low phase coherence, the DEM differs in mean and standard deviation by 0.5 +/- 10.1, 1.1 +/- 6.4, and 3.1 +/- 4.0 m from ICESat, GPS, and ALS, respectively. The excluded data points may deviate by more than 50 m. In order to suppress the spatially variable noise below a 5-m threshold, 18% of the DEM area is selectively averaged to a final product at varying horizontal spatial resolution. Apart from mountainous areas, the new DEM outperforms other currently available DEMs and may serve as a benchmark for future elevation models such as from the TanDEM-X mission to spatially monitor ice sheet elevation.

Comparisons of observed ice properties and Envisat Advanced Synthetic Aperture Radar (ASAR) data during Nathanial B. Palmer cruise NBP09-01 and Oden cruise OSO08/09

Envisat Advanced Synthetic Aperture Radar (ASAR) Wide Swath Mode (WSM) images are used to derive C-band HH-polarization normalized radar cross sections (NRCS). These are compared with ice-core analysis and visual ship-based observations of snow and ice properties observed according to the Antarctic Sea Ice Processes and Climate (ASPeCt) protocol during two International Polar Year summer cruises (Oden 2008 and Palmer 2009) in West Antarctica. Thick first-year (TFY) and multi-year (MY) ice were the dominant ice types. The NRCS value ranges between -16.3 ± 1.1 and -7.6 ± 1.0 dB for TFY ice, and is -12.6 ± 1.3 dB for MY ice; for TFY ice, NRCS values increase from ~-15 dB to -9 dB from December/January to mid-February. In situ and ASPeCt observations are not, however, detailed enough to interpret the observed NRCS change over time. Co-located Advanced Microwave Scanning Radiometer-Earth Observing System (AMSR-E) vertically polarized 37 GHz brightness temperatures (TB37V), 7 day and 1 day averages as well as the TB37V difference between ascending and descending AMSR-E overpasses suggest the low NRCS values (-15 dB) are associated with snowmelt being still in progress, while the change towards higher NRCS values (-9dB) is caused by commencement of melt-refreeze cycles after about mid-January.

(Table 1) Accumulation and ice discharge of West Antarctic glaciers draining into the Amundsen Sea between 1974 and 2007

The Advanced Land Observation System (ALOS) Phased-Array Synthetic-Aperture Radar (PALSAR) is an L-band frequency (1.27 GHz) radar capable of continental-scale interferometric observations of ice sheet motion. Here, we show that PALSAR data yield excellent measurements of ice motion compared to C-band (5.6 GHz) radar data because of greater temporal coherence over snow and firn. We compare PALSAR velocities from year 2006 in Pine Island Bay, West Antarctica with those spanning years 1974 to 2007. Between 1996 and 2007, Pine Island Glacier sped up 42% and ungrounded over most of its ice plain. Smith Glacier accelerated 83% and ungrounded as well. Their largest speed up are recorded in 2007. Thwaites Glacier is not accelerating but widening with time and its eastern ice shelf doubled its speed. Total ice discharge from these glaciers increased 30% in 12 yr and the net mass loss increased 170% from 39 ± 15 Gt/yr to 105 ± 27 Gt/yr. Longer-term velocity changes suggest only a moderate loss in the 1970s. As the glaciers unground into the deeper, smoother beds inland, the mass loss from this region will grow considerably larger in years to come.