Fas ligand expression and tumour immune evasion; the role of prostaglandin E2 and the EP1 receptor

Background and Aim: During carcinogenesis, tumours develop multiple mechanisms to evade the immune system and suppress the anti-tumour immune response. Upregulation of Fas Ligand (FasL/CD95L) expression may represent one such mechanism. FasL is a member of the tumour necrosis factor superfamily that triggers apoptotic cell death following ligation to its receptor Fas. Numerous studies have demonstrated upregulated FasL expression in tumor cells, with FasL expression associated with numerous pro-tumorigenic effects. However, little is known about the mechanisms that regulate FasL expression in tumours. The cyclooxgenase (COX) signalling pathway may play an important role in colon carcinogenesis, via the production of prostaglandins, in particular PGE2. PGE2 signals through four different receptor subtypes, EP1 – EP4. Thus, the aim of this study was to investigate the effect of targeting the PGE2-FasL signaling pathway. Results: (i) PGE2 induces FasL expression via the EP1 receptor in colon cancer cells. (ii) Suppression of FasL expression in colon tumour cells in vivo significantly delays and reduces tumour growth. (iii) Blocking EP1 receptor signaling, or suppression of the EP1 receptor in colon tumour cells, reduces tumour growth in vivo. Suppression of tumour growth correlates in part with suppression of FasL expression. (iv) The reduction in tumour growth is associated with an improved anti-tumour immune response. Tumour infiltration by Treg cells and macrophages was reduced, and the cytotoxic activity of CTL generated from splenocytes isolated from these mice increased. Conclusion: 1) Targeting FasL expression by blocking PGE2-EP1 receptor signalling reduces tumour development in vivo. 2) The mechanism is indirect but is associated with an increased anti-tumour immune response. Thus, unraveling the mechanisms regulating FasL expression and the pro-tumorigenic effects of the EP1 receptor may aid in the search for new therapeutic targets against colon cancer.

Infrared spectra of C2H2 under jet-cooled and para-H2 matrix conditions

In spectra of jet-cooled C2H2 recorded with an FTIR spectrometer, the ν5, ν4 + ν5, ν3 and ν2 + ν4 + ν5 bands all exhibit an intensity distribution corresponding to ∼6 K for rotation, with no evidence of nuclear spin conversion. Spectra of C2H2 isolated in solid p-H2 show no evidence of rotation of C2H2. The strong interaction between ν3 and ν2 + ν4 + ν5 in the gas phase is diminished in solid p-H2. Lines associated with dimer, trimer and tetramer of C2H2 are identified. Spectral features characteristic of solid state acetylene are observed under jet-cooled conditions. © 2007 Elsevier B.V. All rights reserved.

Beta-agonist- and prostaglandin E1-induced translocation of the beta-adrenergic receptor kinase: evidence that the kinase may act on multiple adenylate cyclase-coupled receptors.

beta-Adrenergic receptor kinase (beta-AR kinase) is a cytosolic enzyme that phosphorylates the beta-adrenergic receptor only when it is occupied by an agonist [Benovic, J. Strasser, R. H., Caron, M. G. & Lefkowitz, R. J. (1986) Proc. Natl. Acad. Sci. USA 83, 2797-2801.] It may be crucially involved in the processes that lead to homologous or agonist-specific desensitization of the receptor. Stimulation of DDT1MF-2 hamster smooth muscle cells or S49 mouse lymphoma cells with a beta-agonist leads to translocation of 80-90% of the beta-AR kinase activity from the cytosol to the plasma membrane. The translocation process is quite rapid, is concurrent with receptor phosphorylation, and precedes receptor desensitization and sequestration. It is also transient, since much of the activity returns to the cytosol as the receptors become sequestered. Stimulation of beta-AR kinase translocation is a receptor-mediated event, since the beta-antagonist propranolol blocks the effect of agonist. In the kin- mutant of the S49 cells (lacks cAMP-dependent protein kinase), prostaglandin E1, which provokes homologous desensitization of its own receptor, is at least as effective as isoproterenol in promoting beta-AR kinase translocation to the plasma membrane. However, in the DDT1MF-2 cells, which contain alpha 1-adrenergic receptors coupled to phosphatidylinositol turnover, the alpha 1-agonist phenylephrine is ineffective. These results suggest that the first step in homologous desensitization of the beta-adrenergic receptor may be an agonist-promoted translocation of beta-AR kinase from cytosol to plasma membrane and that beta-AR kinase may represent a more general adenylate cyclase-coupled receptor kinase that participates in regulating the function of many such receptors.

Global Rates of Free Hydrogen (H2) Production by Serpentinization and other Abiogenic Processes within Young Ocean Crust

The main conclusion of this dissertation is that global H2 production within young ocean crust (<10 Mya) is higher than currently recognized, in part because current estimates of H2 production accompanying the serpentinization of peridotite may be too low (Chapter 2) and in part because a number of abiogenic H2-producing processes have heretofore gone unquantified (Chapter 3). The importance of free H2 to a range of geochemical processes makes the quantitative understanding of H2 production advanced in this dissertation pertinent to an array of open research questions across the geosciences (e.g. the origin and evolution of life and the oxidation of the Earth’s atmosphere and oceans).

The first component of this dissertation (Chapter 2) examines H2 produced within young ocean crust [e.g. near the mid-ocean ridge (MOR)] by serpentinization. In the presence of water, olivine-rich rocks (peridotites) undergo serpentinization (hydration) at temperatures of up to ~500°C but only produce H2 at temperatures up to ~350°C. A simple analytical model is presented that mechanistically ties the process to seafloor spreading and explicitly accounts for the importance of temperature in H2 formation. The model suggests that H2 production increases with the rate of seafloor spreading and the net thickness of serpentinized peridotite (S-P) in a column of lithosphere. The model is applied globally to the MOR using conservative estimates for the net thickness of lithospheric S-P, our least certain model input. Despite the large uncertainties surrounding the amount of serpentinized peridotite within oceanic crust, conservative model parameters suggest a magnitude of H2 production (~1012 moles H2/y) that is larger than the most widely cited previous estimates (~1011 although previous estimates range from 1010-1012 moles H2/y). Certain model relationships are also consistent with what has been established through field studies, for example that the highest H2 fluxes (moles H2/km2 seafloor) are produced near slower-spreading ridges (<20 mm/y). Other modeled relationships are new and represent testable predictions. Principal among these is that about half of the H2 produced globally is produced off-axis beneath faster-spreading seafloor (>20 mm/y), a region where only one measurement of H2 has been made thus far and is ripe for future investigation.

In the second part of this dissertation (Chapter 3), I construct the first budget for free H2 in young ocean crust that quantifies and compares all currently recognized H2 sources and H2 sinks. First global estimates of budget components are proposed in instances where previous estimate(s) could not be located provided that the literature on that specific budget component was not too sparse to do so. Results suggest that the nine known H2 sources, listed in order of quantitative importance, are: Crystallization (6x1012 moles H2/y or 61% of total H2 production), serpentinization (2x1012 moles H2/y or 21%), magmatic degassing (7x1011 moles H2/y or 7%), lava-seawater interaction (5x1011 moles H2/y or 5%), low-temperature alteration of basalt (5x1011 moles H2/y or 5%), high-temperature alteration of basalt (3x1010 moles H2/y or <1%), catalysis (3x108 moles H2/y or <<1%), radiolysis (2x108 moles H2/y or <<1%), and pyrite formation (3x106 moles H2/y or <<1%). Next we consider two well-known H2 sinks, H2 lost to the ocean and H2 occluded within rock minerals, and our analysis suggests that both are of similar size (both are 6x1011 moles H2/y). Budgeting results suggest a large difference between H2 sources (total production = 1x1013 moles H2/y) and H2 sinks (total losses = 1x1011 moles H2/y). Assuming this large difference represents H2 consumed by microbes (total consumption = 9x1011 moles H2/y), we explore rates of primary production by the chemosynthetic, sub-seafloor biosphere. Although the numbers presented require further examination and future modifications, the analysis suggests that the sub-seafloor H2 budget is similar to the sub-seafloor CH4 budget in the sense that globally significant quantities of both of these reduced gases are produced beneath the seafloor but never escape the seafloor due to microbial consumption.

The third and final component of this dissertation (Chapter 4) explores the self-organization of barchan sand dune fields. In nature, barchan dunes typically exist as members of larger dune fields that display striking, enigmatic structures that cannot be readily explained by examining the dynamics at the scale of single dunes, or by appealing to patterns in external forcing. To explore the possibility that observed structures emerge spontaneously as a collective result of many dunes interacting with each other, we built a numerical model that treats barchans as discrete entities that interact with one another according to simplified rules derived from theoretical and numerical work, and from field observations: Dunes exchange sand through the fluxes that leak from the downwind side of each dune and are captured on their upstream sides; when dunes become sufficiently large, small dunes are born on their downwind sides (“calving”); and when dunes collide directly enough, they merge. Results show that these relatively simple interactions provide potential explanations for a range of field-scale phenomena including isolated patches of dunes and heterogeneous arrangements of similarly sized dunes in denser fields. The results also suggest that (1) dune field characteristics depend on the sand flux fed into the upwind boundary, although (2) moving downwind, the system approaches a common attracting state in which the memory of the upwind conditions vanishes. This work supports the hypothesis that calving exerts a first order control on field-scale phenomena; it prevents individual dunes from growing without bound, as single-dune analyses suggest, and allows the formation of roughly realistic, persistent dune field patterns.

Legal Responsibilities When Hiring Migrant, Seasonal and H2-A Visa Workers

When farmers need to harvest a large amount of crops in a short period of time, migrant, seasonal, and H-2A Visa workers can often be the best solution to complete the job quickly and affordably. However, there are specific Federal and state legal duties and responsibilities for farmers who employ these types of workers and substantial criminal and civil penalties for failing to adhere to the law.