The regulation of protein kinase C by thiol oxidation

The Ser/Thr protein kinase C (PKC) isozyme family plays an important role in cell growth and differentiation and also contributes to key events in the development and progression of cancer. PKC isozymes are activated by phospholipid-dependent mechanisms, and they are also subject to oxidative activation and inactivation. Oxidative regulatory mechanisms are important in the governance of PKC isozyme action. While oxidative PKC activation involves phospho-tyrosine (P-Y) stabilization, the molecular mechanism(s) for oxidative PKC inactivation have not been defined. We previously reported that Thr → Cys peptide-substrate analogs inactivate several PKC isozymes including PKC-α via S-thiolation, i.e., by forming disulfides with PKC thiols. This inactivation mechanism is chemically analogous to protein S-glutathiolation, a post-translational modification that has been shown to oxidatively regulate several enzymes. To determine if PKC-α could be inactivated by S-glutathiolation, we employed the thiol-specific oxidant diamide (0.01–10mM) and 100μM glutathione (GSH). Diamide alone (0.1–5.0 mM) weakly inactivated PKC-α (<20%), and GSH alone had no effect on the isozyme activity. Marked potentiation of diamide-induced PKC-α inactivation (>90%) was achieved by 100μM GSH, resulting in full inactivation of the isozyme. Inactivation was reversed by DTT, consistent with a mechanism involving PKC-α S-glutathiolation. S-glutathiolation was demonstrated as DTT-reversible incorporation of [35S] GSH into PKC-α isozyme structure. These results indicate that a mild oxidative stimulus can inactivate purified PKC-α via S-glutathiolation. In addition, diamide treatment of metabolically labeled NIH3T3 cells induced potent PKC-α inactivation via isozyme [35S] S-thiolation. These results indicate that cellular PKC-α can be regulated via S-glutathiolation. ^

Activation of c -Met contributes to growth and metastasis of human colorectal carcinoma

c-Met is the protein tyrosine kinase receptor for hepatocyte growth factor/scatter factor (HGF/SF) and mediates several normal cellular functions including proliferation, survival, and migration. Overexpression of c-Met correlates with progression and metastasis of human colorectal carcinoma (CRC). The goals of this study were to determine if overexpression of c-Met directly contributes to tumorigenicity and liver metastatic potential of colon cancer, and what are the critical pathways regulated by c-Met in this process. The studies used two colon tumor cell lines, KM12SM and KM20, which express high levels of constitutively active c-Met and are highly metastatic in nude mice. To examine the effects of c-Met overexpression, subclones of theses lines with reduced c-Met expression were obtained following transfection with a c-Met specific targeting ribozyme. Reduction of c-Met in KM12SM cells abolished liver metastases when cells were injected intrasplenically in an experimental metastasis assay. However, c-Met downregulation in theses clones was unstable. Three stable KM20 clones with a 25–35% reduction in c-Met protein levels but 60–90% reduction in basal c-Met autophosphorylation and kinase activity were obtained. While HGF increased c-Met kinase activity in the clones with reduced c-Met, the activity was less than that observed in parental or control transfected cells. Correlating with the reduction in c-Met kinase activity, subclones with reduced c-Met expression had significantly reduced in vitro growth rates, soft-agar colony forming abilities, and increased apoptosis. HGF/SF treatment did not affect anchorage-dependent growth or soft-agar colony forming abilities. Further, c-Met downregulation significantly impaired the ability of HGF/SF to induce migration. To examine the effects of reduced c-Met on tumor formation, parental and c-Met reduced KM20 cells were grown subcutaneously and intrahepatically in nude mice. c-Met downregulation delayed, but did not abolish growth at the subcutaneous site. When these cells were injected intrahepatically, both tumor incidences and size were significantly reduced. To further understand the molecular basis of c-Met in promoting tumor growth, the activation of several signaling intermediates that have been implicated in c-Met mediated growth, survival and migration were compared between KM20 parental cells and subclones with reduced c-Met expression levels. The expression and activity (as determined by phosphorylation) of AKT and Erk1/2 were unaltered. In contrast, Src kinase activity, as measured by immune complex kinase assay, was reduced 2–5 fold following c-Met downregulation. As Src has been implicated in growth, survival and migration, Src activation in c-Met overexpressing lines is likely contributing to the tumorigenic and metastatic capabilities of colon tumor cell lines that overexpress c-Met. Collectively, these results suggest that c-Met overexpression plays a causal role in the development of CRC liver metastases, and that c-Src and c-Met inhibitors may be of potential therapeutic benefit for late-stage colon cancer. ^

Dust record from the EPICA Dome C ice core, Antarctica, covering 0 to 800 kyr BP

Dust can affect the radiative balance of the atmosphere by absorbing or reflecting incoming solar radiation and it can be a source of micronutrients, such as iron, to the ocean. It has been suggested that production, transport, and deposition of dust is influenced by climatic changes on glacial-interglacial timescales. Here we present a high-resolution aeolian dust record from the EPICA Dome C ice core in East Antarctica, which provides an undisturbed climate sequence over the last eight climatic cycles. We find that there is a significant correlation between dust flux and temperature records during glacial periods that is absent during interglacial periods. Our data suggests that dust flux is increasingly correlated with Antarctic temperature as climate becomes colder. We interpret this as progressive coupling of Antarctic and lower latitudes climate. Limited changes in glacial-interglacial atmospheric transport time Mahowald et al. (1999, doi:10.1029/1999JD900084), Jouzel et al. (2007, doi:10.1126/science.1141038), and Werner et al. (2002, doi:10.1029/2002JD002365) suggest that the sources and lifetime of dust are the major factors controlling the high glacial dust input. We propose that the observed ~25-fold increase in glacial dust flux over all eight glacial periods can be attributed to a strengthening of South American dust sources, together with a longer atmospheric dust particle life-time in the upper troposphere resulting from a reduced hydrological cycle during the ice ages.

Average nutrient concentration, and growth characteristics of bacteria during USCGC Healy cruises in 2002 and 2004

Standing stocks and production rates for phytoplankton and heterotrophic bacteria were examined during four expeditions in the western Arctic Ocean (Chukchi Sea and Canada Basin) in the spring and summer of 2002 and 2004. Rates of primary production (PP) and bacterial production (BP) were higher in the summer than in spring and in shelf waters than in the basin. Most surprisingly, PP was 3-fold higher in 2004 than in 2002; ice-corrected rates were 1581 and 458 mg C/m**2/d respectively, for the entire region. The difference between years was mainly due to low ice coverage in the summer of 2004. The spatial and temporal variation in PP led to comparable variation in BP. Although temperature explained as much variability in BP as did PP or phytoplankton biomass, there was no relationship between temperature and bacterial growth rates above about 0°C. The average ratio of BP to PP was 0.06 and 0.79 when ice-corrected PP rates were greater than and less than 100 mg C/m**2/d, respectively; the overall average was 0.34. Bacteria accounted for a highly variable fraction of total respiration, from 3% to over 60% with a mean of 25%. Likewise, the fraction of PP consumed by bacterial respiration, when calculated from growth efficiency (average of 6.9%) and BP estimates, varied greatly over time and space (7% to >500%). The apparent uncoupling between respiration and PP has several implications for carbon export and storage in the western Arctic Ocean.

Stable oxygen isotope record and Mg/Ca ratios at the Mid-Pleistocene Climate Transition, ODP Site 181-1123

Earth's climate underwent a fundamental change between 1250 and 700 thousand years ago, the Mid-Pleistocene Transition (MPT), when the dominant periodicity of climate cycles changed from 41,000 to 100,000 years in the absence of significant change in orbital forcing. Over this time, an increase occurred in the amplitude of change of deep ocean foraminiferal oxygen isotopic ratios, traditionally interpreted as defining the main rhythm of ice ages although containing large effects of changes in deep-ocean temperature. We have separated the effects of decreasing temperature and increasing global ice volume on oxygen isotope ratios. Our results suggest that the MPT was initiated by an abrupt increase in Antarctic ice volume at 900 ka. We see no evidence of a pattern of gradual cooling but near-freezing temperatures occur at every glacial maximum.