The role of platelet -derived growth factor (PDGF) signaling in gliomagenesis

Gliomas are primary central nervous system (CNS) neoplasms that are believed to arise from astrocytes, oligodendrocytes or their precursors. Gliomas can be classified into two major histopathological groups: oligodendroglial and astroglial tumors. The most malignant of the astroglial tumors is glioblastoma multiforme (GBM). A great deal of genetic and epigenetic alterations have been implicated in gliomagenesis. In particular, PDGF signaling is frequently over-activated in a large number of human gliomas. In order to gain insights into the biology of gliomas, we manage to model human gliomas in mice using a somatic gene transfer approach—RCAS/TVA system. In our previous study, combined activation of AKT and RAS pathways gave rise to glioblastomas from CNS progenitors. In the present study, we demonstrate that in vivo autocrine PDGF stimulation induces oligodendrogliomas and mixed oligoastrocytomas from CNS progenitors and differentiated astrocytes respectively. In culture autocrine PDGF stimulation dedifferentiates astrocytes into progenitor-like cells and blockade of PDGF signaling reverses these phenotypic changes. Experimental disruption of cell cycle arrest pathway, such as Ink4a-Arf loss, is not required for the initiation of PDGF-induced gliomagenesis; instead, this mutation contributes to the tumor progression by enhancing tumor malignancy and shortening tumor latency. P53 deficiency does not promote the PDGF-induced gliomagenesis. In addition, 1p and 19q, often deleted in human oligodendrogliomas, remain intact in these PDGF-induced gliomas. Therefore, our studies suggest that autocrine PDGF stimulation alone may be sufficient to induce gliomagenesis. In contrast to transient stimulation in vitro, constitutive PDGF stimulation activates neither AKT nor RAS/MAPK pathways during gliomagenesis. This results in the formation of oligodendrogliomas, instead of glioblastomas. Sustained activation of the AKT pathway converts PDGF-induced oligodendrogliomas into astrocytomas. Our studies suggest that constitutive PDGF stimulation is not equivalent to transient PDGF stimulation, and that a transition between oligodendroglial and astroglial tumors in humans may be possible, depending on additional alterations. In summary, PDGF signaling plays a pivotal role in gliomagenesis in the mouse, and its hyperactivity is capable of contributing to both oligodendroglial and astroglial tumorigenesis. ^

Oceanography during TYDEMAN cruise DCM (DeepChlorMax) to the Equatorial Atlantic

The cruise with RV Tydeman was devoted to study permanently stratified plankton systems in the (sub)tropical ocean, which are characterised by a deep chlorophyll peak between 80 and 150 m. To minimise lateral effects by horizontal transport of nutrients and organic matter from river outflow and upwelling regions, stations were selected in the middle of the North Atlantic Ocean between the continents of America and Africa. (5 - 35° N and 50 - 15° W). Here the vertical distributions of light and nutrients control the abundance and growth of autotrophic algae in the thermically stratified water column. This phytoplankton is numerically dominated by the prokaryotic picoplankters Synechococcus spp. and Prochlorococcus spp., which are smaller than 2 ?m. The productivity of the 100 to 150 m deep euphotic zone can be high, because a high heterotrophic/autotrophic biomass ratio induces a rapid regeneration of nutrients and inorganic carbon. Primary grazers are mainly micro-organisms such as heterotrophic nannoflagellates and ciliates, which feed on the small algae and on bacteria. Heterotrophic bacteria can outnumber the autotrophic algae, because their number is related to the substrate pools of dissolved and particulate dead organic matter. These DOC and detritus pools reach equilibrium at a concentration, where the rate of their production (proportional to algal biomass) equals their mineralisation and sinking rate (proportional to the concentration and weight of POC and detritus). At a relatively low value of the weight-specific loss rates, the equilibrium concentration of these carbon pools and their load of bacteria can be high. The bacterial productivity is proportional to the mineralisation rate, which in a steady state can never be higher than the rate of primary production. Hence the ratio in turnover rate of bacteria and autotrophs tends to be reciprocally proportional to their biomass ratio.

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.

Abundance of phytoplankton, heterotrophic nanoflagellates and bacteria through the water column at time series station L4 in the Western English Channel. 2007-2011

The marine laboratories in Plymouth have sampled at two principle sites in the Western English Channel for over a century in open-shelf (station E1; 50° 02'N, 4° 22'W) and coastal (station L4; 50° 15'N, 4° 13'W) waters. These stations are seasonally stratified from late-April until September, and the variable biological response is regulated by subtle variations in temperature, light, nutrients and meteorology. Station L4 is characterized by summer nutrient depletion, although intense summer precipitation, increasing riverine input to the system, results in pulses of increased nitrate concentration and surface freshening. The winter nutrient concentrations at E1 are consistent with an open-shelf site. Both stations have a spring and autumn phytoplankton bloom; at station E1, the autumn bloom tends to dominate in terms of chlorophyll concentration. The last two decades have seen a warming of around 0.6°C per decade, and this is superimposed on several periods of warming and cooling over the past century. In general, over the Western English Channel domain, the end of the 20th century was around 0.5°C warmer than the first half of the century. The warming magnitude and trend is consistent with other stations across the north-west European Shelf and occurred during a period of reduced wind stress and increased levels of insolation (+20%); these are both correlated with the larger scale climatic forcing of the North Atlantic Oscillation.

Experiment: Growth rates and percentages of normal versus malformed versus incomplete versus incomplete and malformed coccoliths

The coccolithophore Emiliania huxleyi (Lohmann) W. W. Hay et H. Mohler was cultured in natural seawater with the addition of either the microtubule-inhibitor colchicine, the actin-inhibitor cytochalasin B, or the photosynthesis inhibitor 3-(3,4 dichlorophenyl)-1,1-dimethyl-urea (DCMU). Additionally, E. huxleyi was cultured at different light intensities and temperatures. Growth rate was monitored, and coccolith morphology analyzed. While every treatment affected growth rate, the percentage of malformed coccoliths increased with colchicine, cytochalasin B, and at higher than optimal temperature. These results represent the first experimental evidence for the role of microtubules and actin microfilaments in coccolith morphogenesis.