A novel mechanism of regulation of phosphatidylinositol 3 -kinase: Tyrosine phosphorylation of p85 residue 688

Phosphatidylinositol 3-kinase (PI3K) phosphorylates membrane constituent phosphatidylinositols, producing second messengers that link membrane bound receptor signals to cellular proliferation and survival. PI3K, a heterodimer consisting of a catalytic p110 subunit and a regulatory p85 subunit, can be activated through induced association with other signaling molecules. The p85 subunit serves to both stabilize and inactivate p110. The inhibitory activity of P85 is relieved by occupancy of the N terminal SH2 domain by phosphorylated tyrosine. PI3K becomes phosphorylated and activated subsequent to a variety of stimuli. Indeed, Src family kinases have been demonstrated to phosphorylate p85 at tyrosine 688, but the role of phosphorylation in PI3K function is unclear. We decided to evaluate the importance of tyrosine phosphorylation to PI3K activity. We demonstrate that tyrosine phosphorylated p85 is associated with a higher specific activity than is non-phosphorylated PI3K. Wild type p85 inhibits PI3K enzyme activity, a process accentuated by mutation of tyrosine 688 to alanine and reversed by mutation to aspartate which functions as a phosphotyrosine mimic in multiple systems. Strikingly, the Y688D mutation completely reverses the p85 inhibitory activity on cell viability and activation of downstream protein NFkB. We demonstrate that tyrosine phosphorylated Y688 or Y688D is sufficient to bind the p85 N terminal SH2 domain, either within full length p85 or in an isolated N terminal SH2 domain, suggesting the possibility of an intramolecular interaction between phosphorylated Y688 and the p85 N terminal SH2 domain that can relieve the p85-induced inhibition of p110. Further, we provide evidence that dephosphorylation of Y688 reduces phosphorylation-induced PI3K activity. We demonstrate that tyrosine phosphatase SHP-1 can physically associate with p85 in a SH2-mediated interaction with the C terminal tail of SHP-1. This association is concomitant with both p85 dephosphorylation and decreased PI3K activity. Altogether, our data suggests the phosphorylation state of p85 is the focal point of a novel mechanism for PI3K activity regulation. As PI3K has been shown to be involved in the vital physiological processes of cell proliferation and apoptosis, a thorough understanding of the regulation of this signaling protein may provide opportunities for the design of novel treatments for cancer. ^

Mechanism of translationally coupled mRNA turnover mediated by c-fos protein-coding-region determinant

Proto-oncogene c-fos is a member of the class of early-response genes whose transient expression plays a crucial role in cell proliferation, differentiation, and apoptosis. Degradation of c- fos mRNA is an important mechanism for controlling c-fos expression. Rapid mRNA turnover mediated by the protein-coding-region determinant (mCRD) of the c-fos transcript illustrates a functional interplay between mRNA turnover and translation that coordinately influences the fate of cytoplasmic mRNA. It is suggested that mCRD communicates with the 3′ poly(A) tail via an mRNP complex comprising mCRD-associated proteins, which prevents deadenylation in the absence of translation. Ribosome transit as a result of translation is required to alter the conformation of the mRNP complex, thereby eliciting accelerated deadenylation and mRNA decay. To gain further insight into the mechanism of mCRD-mediated mRNA turnover, Unr was identified as an mCRD-binding protein, and its binding site within mCRD was characterized. Moreover, the functional role for Unr in mRNA decay was demonstrated. The result showed that elevation of Unr protein level in the cytoplasm led to inhibition of mRNA destabilization by mCRD. In addition, GST pull-down assay and immuno-precipitation analysis revealed that Unr interacted with PABP in an RNA-independent manner, which identified Unr as a novel PABP-interacting protein. Furthermore, the Unr interacting domain in PABP was characterized. In vivo mRNA decay experiments demonstrated a role for Unr-PABP interaction in mCRD-mediated mRNA decay. In conclusion, the findings of this study provide the first evidence that Unr plays a key role in mCRD-mediated mRNA decay. It is proposed that Unr is recruited by mCRD to initiate the formation of a dynamic mRNP complex for communicating with poly(A) tail through PABP. This unique mRNP complex may couple translation to mRNA decay, and perhaps to recruit the responsible nuclease for deadenylation. ^

Molecular mechanism of the relaxin signaling pathways: Activation of cAMP, PI3K, and PKCzeta

Relaxin is a polypeptide hormone that has diverse effects on reproductive and non-reproductive tissues. Relaxin activates the G-protein coupled receptors, LGR7 and LRG8. Early studies described increased cAMP and protein kinase A activity upon relaxin treatment, but cAMP accumulation alone could not account for all of the relaxin-mediated effects. We utilized the human monocyte cell line THP-1 to study the mechanism of relaxin-stimulated CAMP production. ^ Relaxin treatment in THP-1 cells produces a biphasic time course in cAMP accumulation, where the first peak appears as early as 1–2 minutes with a second peak at 10–20 minutes. Selective inhibitors for phosphoinositide 3-kinase (P13K), such as wortmannin and LY294002, show a dose-dependent inhibition of relaxin-stimulated cAMP accumulation, specific for the second peak of the relaxin time course. Neither the effects of relaxin nor the inhibition of relaxin by LY294002 is mediated by the activity of phosphodiesterases. Furthermore, LY294002 blocks upregulation of vascular endothelial growth factor transcript levels by relaxin. ^ To further delineate relaxin signaling pathways, we searched for downstream targets of PI3K that could activate adenylyl cyclase (AC). Protein kinase C ζ (PKCζ) was a prime candidate because it activates types II and V AC. Chelerythrine chloride (a general PKC inhibitor) inhibits relaxin-induced cAMP production to the same degree as LY294002 (∼40%). Relaxin stimulates PKCζ translocation to the plasma membrane in THP-1, MCF-7, PHM1-31, and MMC cells, as shown by immunocytochemistry. PKCζ translocation is P13K-dependent and independent of cAMP production. Antisense PKCζ oligodeoxynucleotides (PKCζ-ODNs) deplete both PKCζ transcript and protein levels in THP-1 cells. PKCζ-ODNs abolish relaxin-mediated PKCζ translocation and inhibit relaxin stimulation of cAMP by 40%, as compared to mock and random ODN controls. Treatment with LY294002 in the presence of PKCζ-ODNs results in little further inhibition. Taken together, we present a novel role for PI3K and PKCζ in relaxin stimulation of cAMP and provide the first example of the PKCζ regulation of AC in an endogenous system. Furthermore, we have identified higher order complexes of AC isoforms and PKA anchoring proteins in attempts to explain the differential coupling of relaxin to cAMP and PI3K-signaling pathways in various cell types. ^

Safety door for the unloading mechanism of self-unloading wagons

A safety door for the discharge opening of a selfunloading wagon is disclosed herein. The wagon includes a material receiving box having a first conveyor therein for conveying the material towards one end thereof. A cross conveyor is mounted at the one end of the box for conveying the material outwardly from the box through the lower end of a discharge opening formed in the side of the box. A material beater means is rotatably mounted in the box above the cross conveyor. The safety door extends across the discharge opening to prevent the operator from reaching inwardly through the discharge opening. The safety door is self-closing and is opened by the material being discharged outwardly through the discharge opening.

Shelling mechanism

A corn shelling mechanism comprising an elongated concave means having one end thereof positioned below a rotatable cylinder. A continuous belt sheller is positioned above the concave in a spaced relationship with respect thereto. The corn ears are fed to the rotating cylinder by a feeder housing means with the ear receiving one or more impacts by the rasp bar of the cylinder before it travels out of range of the cylinder. The partially shelled ear passes between the belt sheller and the concave with the belt sheller urging the ears into engagement with the concave to complete the shelling operation.

The Chilean wheat market and its price support mechanism : a spatial market integration analysis

This research investigates the spatial market integration of the Chilean wheat market in relation with its most representative international markets by using a vector error correction model (VECM) and how a price support policy, as a price band, affect it. The international market was characterized by two relevant wheat prices: PAN from Argentina and Hard Red Winter from the United States. The spatial market integration level, expressed in the error correction term (ECT), allowed concluding that there is a high integration degree among these markets with a variable influence of the price band mechanism mainly related with its estimation methodology. Moreover, this paper showed that Chile can be seen as price taker as long as the speed of its adjustment to international shocks, being these reactions faster than in the United States and Argentina. Finally, the results validated the "Law of the One Price", which assumes price equalization across all local markets in the long run.

Investigations on volcanic rocks in sediment core CRP-3 from the Ross Sea, Antarctica

The petrography, mineralogy and geochemistry of volcanic and subvolcanic rocks in CRP-3 core have been examined in detail in order to characterise and to compare them with volcanic and subvolcanic rocks cropping out in the Victoria Land area, and to define the clast provenance or to establish possible volcanic activity coeval with deposition. Clasts with sizes ranging from granule to boulder show geochemical and mineralogical features comparable with those of Ferrar Supergroup rocks. They display a subalkaline affinity and compositions ranging from basalts to dacite. Three different petrographic groups with distinct textural and grain size features (subophitic, intergranular-intersertal, and glassy-hyalopilitic) are recognised and are related to the emplacement/cooling mechanism. In the sand to silt fraction, the few glass shards that have been recognised are strongly altered: however chemical analyses show they have subalkalic magmatic affinity. Mineral compositions of the abundant free clinopyroxene grains found in the core, are less affected by alteration processes, and indicate an origin from subalkaline magmas. This excludes the presence, during the deposition of CRP-3 rocks of alkaline volcanic activity comparable with the McMurdo Volcanic Group. Strong alteration of the magmatic body intruded the Beacon sandstones obliterates the original mineral assemblage. Geochemical investigations confirm that intrusion is part of the Ferar Large Igneous Province.

Chemical composition of minerals and rocks from the Sierra Leone segment of the Mid-Atlantic Ridge and from the Markov depression, Central Atlantic

Silicic Fe-Ti-oxide magmatic series was the first recognized in the Sierra Leone axial segment of the Mid-Atlantic Ridge near 6°N. The series consists of intrusive rocks (harzburgites, lherzolites, bronzitites, norites, gabbronorites, hornblende Fe-Ti-oxide gabbronorites and gabbronorite-diorites, quartz diorites, and trondhjemites) and their subvolcanic (ilmenite-hornblende dolerites) and, possibly, volcanic analogues (ilmenite-bearing basalts). Deficit of most incompatible elements in the rocks of the series suggests that parental melts derived from a source that had already been melted. Correspondingly, these melts could not be MORB derivatives. Origin of the series is thought to be related to melting of the hydrated oceanic lithosphere during emplacement of an asthenospheric plume (protuberance on the surface of large asthenospheric lens beneath MAR). Genesis of different melts was supposedly controlled by ascent of a chamber of hot mantle magmas thought this lithosphere in compliance with the zone melting mechanism. Melt acquired fluid components from heated rocks at peripheries of the plume and became enriched in Fe, Ti, Pb, Cu, Zn, and other components mobile in fluids.

Jelly biomass sinking speed reveals a fast carbon export mechanism

Particulate matter export fuels benthic ecosystems in continental margins and the deep sea, removing carbon from the upper ocean. Gelatinous zooplankton biomass provides a fast carbon vector that has been poorly studied. Observational data of a large-scale benthic trawling survey from 1994 to 2005 provided a unique opportunity to quantify jelly-carbon along an entire continental margin in the Mediterranean Sea and to assess potential links with biological and physical variables. Biomass depositions were sampled in shelves, slopes and canyons with peaks above 1000 carcasses per trawl, translating to standing stock values between 0.3 and 1.4 mg C m2 after trawling and integrating between 30,000 and 175,000 m2 of seabed. The benthopelagic jelly-carbon spatial distribution from the shelf to the canyons may be explained by atmospheric forcing related with NAO events and dense shelf water cascading, which are both known from the open Mediterranean. Over the decadal scale, we show that the jelly-carbon depositions temporal variability paralleled hydroclimate modifications, and that the enhanced jelly-carbon deposits are connected to a temperature-driven system where chlorophyll plays a minor role. Our results highlight the importance of gelatinous groups as indicators of large-scale ecosystem change, where jelly-carbon depositions play an important role in carbon and energy transport to benthic systems.

Jelly biomass sinking speed reveals a fast carbon export mechanism

Sinking of gelatinous zooplankton biomass is an important component of the biological pump removing carbon from the upper ocean. The export efficiency, e.g., how much biomass reaches the ocean interior sequestering carbon, is poorly known because of the absence of reliable sinking speed data. We measured sinking rates of gelatinous particulate organic matter (jelly-POM) from different species of scyphozoans, ctenophores, thaliaceans, and pteropods, both in the field and in the laboratory in vertical columns filled with seawater using high-quality video. Using these data, we determined taxon-specific jelly-POM export efficiencies using equations that integrate biomass decay rate, seawater temperature, and sinking speed. Two depth scenarios in several environments were considered, with jelly-POM sinking from 200 and 600 m in temperate, tropical, and polar regions. Jelly-POM sank on average between 850 and 1500 m/d (salps: 800-1200 m/d; ctenophores: 1200-1500 m/d; scyphozoans: 1000-1100 m d; pyrosomes: 1300 m/d). High latitudes represent a fast-sinking and low-remineralization corridor, regardless of species. In tropical and temperate regions, significant decomposition takes place above 1500 m unless jelly-POM sinks below the permanent thermocline. Sinking jelly-POM sequesters carbon to the deep ocean faster than anticipated, and should be incorporated into biogeochemical and modeling studies to provide more realistic quantification of export via the biological carbon pump worldwide.

Phytoplankton calcification as an effective mechanism to alleviate cellular calcium poisoning

Marine phytoplankton has developed the remarkable ability to tightly regulate the concentration of free calcium ions in the intracellular cytosol at a level of ~ 0.1 µmol /l in the presence of seawater Ca2+ concentrations of 10 mmol/1. The low cytosolic calcium ion concentration is of utmost importance for proper cell signalling function. While the regulatory mechanisms responsible for the tight control of intracellular Ca2+ concentration are not completely understood, phytoplankton taxonomic groups appear to have evolved different strategies, which may affect their ability to cope with changes in seawater Ca2+ concentrations in their environment on geological time scales. For example, the Cretaceous (145 to 66 Ma ago), an era known for the high abundance of coccolithophores and the production of enormous calcium carbonate deposits, exhibited seawater calcium concentrations up to four times present-day levels. We show that calcifying coccolithophore species (Emiliania huxleyi, Gephyrocapsa oceanica and Coccolithus braarudii) are able to maintain their relative fitness (in terms of growth rate and photosynthesis) at simulated Cretaceous seawater calcium concentrations, whereas these rates are severely reduced under these conditions in some non-calcareous phytoplankton species (Chaetoceros sp., Ceratoneis closterium and Heterosigma akashiwo). Most notably, this also applies to a non-calcifying strain of E. huxleyi which displays a calcium-sensitivity similar to the non-calcareous species. We hypothesize that the process of calcification in coccolithophores provides an efficient mechanism to alleviate cellular calcium poisoning and thereby offered a potential key evolutionary advantage, responsible for the proliferation of coccolithophores during times of high seawater calcium concentrations. The exact function of calcification and the reason behind the highly-ornate physical structures of coccoliths remain elusive.

Bicarbonate uptake via an anion exchange protein is the main mechanism of inorganic carbon acquisition by the giant kelp Macrocystis pyrifera (Laminariales, Phaeophyceae) under variable pH

Macrocystis pyrifera is a widely distributed, highly productive, seaweed. It is known to use bicarbonate (HCO3-) from seawater in photosynthesis and the main mechanism of utilization is attributed to the external catalyzed dehydration of HCO3- by the surface-bound enzyme carbonic anhydrase (CAext). Here, we examined other putative HCO3- uptake mechanisms in M. pyrifera under pHT 9.00 (HCO3-: CO2 = 940:1) and pHT 7.65 (HCO3-: CO2 = 51:1). Rates of photosynthesis, and internal CA (CAint) and CAext activity were measured following the application of AZ which inhibits CAext, and DIDS which inhibits a different HCO3- uptake system, via an anion exchange (AE) protein. We found that the main mechanism of HCO3- uptake by M. pyrifera is via an AE protein, regardless of the HCO3-: CO2 ratio, with CAext making little contribution. Inhibiting the AE protein led to a 55%-65% decrease in photosynthetic rates. Inhibiting both the AE protein and CAext at pHT 9.00 led to 80%-100% inhibition of photosynthesis, whereas at pHT 7.65, passive CO2 diffusion supported 33% of photosynthesis. CAint was active at pHT 7.65 and 9.00, and activity was always higher than CAext, because of its role in dehydrating HCO3- to supply CO2 to RuBisCO. Interestingly, the main mechanism of HCO3- uptake in M. pyrifera was different than that in other Laminariales studied (CAext-catalyzed reaction) and we suggest that species-specific knowledge of carbon uptake mechanisms is required in order to elucidate how seaweeds might respond to future changes in HCO3-:CO2 due to ocean acidification.