Conservation and release of osmolytes by yeasts during hypo-osmotic stress

In response to fluctuations in environmental osmolarity, yeast cells adjust their intracellular solute concentrations in order to maintain a constant turgor pressure and ensure continuation of cellular activity. In this study, the effect of hypo-osmotic stress on osmolyte content of osmotolerant yeasts Zygosaccharomyces rouxii and Pichia sorbitophila and the less tolerant Saccharomyes cerevisiae was investigated. All these yeasts released glycerol upon hypo-osmotic shock. However, Z. rouxii also released arabitol, whereas P. sorbitophila released erythritol in addition to arabitol and glycerol. Osmolyte release was very rapid and specific and was neither affected by reduced temperatures nor inhibited by the channel blocker gadolinium or the protonophore carbonyl cyanide m-chlorophenyl hydrazone. Extracellular osmolyte levels increased drastically suggesting that osmolytes were not metabolised but mainly released upon exposure to hypotonic conditions. The export process is well controlled, and the amount of osmolyte released was proportional to the shock intensity. Osmolyte release occurred with little cell lysis and thus the survival as well as the subsequent growth of yeast cells was largely unaffected after hypo-osmotic shock. The kinetics and patterns of osmolyte export suggest the involvement of channel proteins, but the molecular nature of this export pathway in yeasts, with exception of S. cerevisiae, remains to be established.     

Seasonal stable isotope variations of the modern Amazonian freshwater bivalve Anodontites trapesialis

In a floodplain lake of the Amazon River near the city of Iquitos, northeastern Peru, a one-year monitoring experiment was conducted during which water samples and living bivalves (Anodontites trapesialis) were collected with the aim to investigate seasonal δ¹⁸O variation in and fractionation between bivalve aragonite and host water. Both host water and molluscan growth increments show more than 8‰ seasonal variation in δ¹⁸O. In the floodplain lake under study the δ¹⁸O variation of the water is controlled by contrasting dry and wet season evaporation-precipitation regimes. Molluscan δ¹⁸O appears to be in equilibrium with the host water. Although an approximately 4.0‰ offset occurs, δ¹³C records of water and bivalves are in good agreement, suggesting that both δ¹⁸O and δ¹³C of the shells of freshwater bivalve A. trapesialis are good recorders of (palaeo-)environmental conditions. The δ¹³C of Dissolved Inorganic Carbon (DIC) is governed by plant growth and/or by changes in aquatic chemistry, affecting the DIC pool.     

Different effects of rat interferon alpha, beta and gamma on rat hepatic stellate cell proliferation and activation

Background  

Liver fibrosis is the common sequel of chronic liver diseases. Recent studies have identified hepatic stellate cells as the primary cell type mediating hepatic fibrogenesis. It has been demonstrated that hepatic stellate cells undergo a process of activation during the development of liver fibrosis. During the activation process, hepatic stellate cells acquire myofibroblast-like phenotype featuring the expression of smooth muscle alpha actin. Interferons have been employed for the treatment of viral hepatitis. However, it is unclear what is the effect of interferons on the prevention and treatment of liver fibrosis. Moreover, it is not clear whether there are any differences among interferon alpha, interferon beta, and interferon gamma in the treatment of liver fibrosis. Therefore, our objective in current study is to investigate the effects of rat interferon-α, interferon-β, and interferon-γ on the proliferation and activation of rat hepatic stellate cells.