Extraction and quantitation of astaxanthin from Phaffia rhodozyma

Summary The rapid, quantitative release of astaxanthin and other carotenoids from the yeast Phaffia rhodozyma is described. Hashed cells are ruptured with dimethylsulfoxide (DMSO) and carotenoids extracted into an organic solvent. Extraction and spectrophotometric quantitation of total carotenoids is rapid, reproducible and only small volumes (0.1–2 ml) of culture are required. HPLC analysis in normal phase silica gel column indicates that astaxanthin comprises 65–95% of the total pigmented carotenoids of P. rhodozyma.     

Secretion of the sweet-tasting plant protein thaumatin byBacillus subtilis

Summary With the -amylase promoter and ribosome binding site,Bacillis subtilis was used to express the sweet plant protein thaumatin II cDNA fused in the correct reading frame to the -amylase leader peptide. The r-thaumatin was purified from the medium on a S-Sepharose column and detected with western blots by sheep -thaumatin antibodies. The r-thaumatin and authentic thaumatin were the same size when reduced by 2-ME and the same size when not reduced.     

Secretion of the sweet-tasting plant protein thaumatin byStreptomyces lividans

Summary To produce and direct the export inStreptomyces lividans of the sweet plant protein thaumatin, thaumatin II cDNA was fused in the correct reading frame to the -galactosidase leader peptide, under the control of the -galactosidase promoter and ribosome binding site. The export of the recombinant thaumatin may allow the correct formation of the thaumatin disulfide bonds. The recombinant thaumatin was purified from the medium on an S-Sepharose column and detected with western blots by sheep -thaumatin antibodies. The recombinant thaumatin was the same size as authentic thaumatin and changed position on an acrylamide gel in response to reduction by 2-mercaptoethanol in the same manner.     

Lymphocyte entry into inflammatory tissues in vivo. Qualitative differences of high endothelial venule-like vessels in sponge matrix allografts vs isografts

Sponge matrix allografts and isografts become extensively encapsulated and neovascularized after s.c. implantation. Sponge allografts acquire alloantigen-reactive T lymphocytes, whereas sponge isografts fail to do so, even though these T cells are continuously circulating in the peripheral blood. We have investigated the possibility that the vascular endothelia regulates lymphocytic accumulation in sponge matrix implants. In normal lymph nodes, specialized high endothelial venules (HEV) regulate lymphocyte extravasation from the blood. We have now identified HEV-like vessels in sponge matrix allografts. These vessels are operationally defined as "HEV-like" in that they react with mAb MECA 325 which identifies murine HEV, and bind lymphocytes in ex vivo adhesion assays. In contrast, sponge isografts contain MECA 325 reactive vessels that are significantly smaller than those found in allografts. Further, vessels of sponge isografts do not readily bind lymphocytes in ex vivo adhesion assays. Immunohistologic analysis also revealed that the small MECA 325+ vessels present in sponge isografts are consistently found in close proximity to nerve bundles. Although this MECA 325 reactive vessel-nerve bundle association is also observed in sponge allografts, large MECA 325 reactive vessels are widely distributed in allografts. Our data suggest that small, poorly adhesive MECA 325 reactive vessels develop in sponge isografts and allografts, possibly under the influence of local nerve tissue. These vessels respond to regional alloimmune responses by developing into the larger HEV-like vessels capable of binding lymphocytes in sponge allografts. The value of this experimental system as an in vivo model to evaluate mechanisms involved in neovascularization and endothelial differentiation is discussed.     

Oligochaetes and water pollution in two deep Norwegian lakes

Analyses of the oligochaete fauna of two of the deepest lakes in Scandinavia — the Norwegian lakes Mjösa (450 m) and Tyrifjorden (295 m), revealed a totally different species composition in the deep profundal compared with the upper profundal - in contact with the nutrient-enriched epilimnion. In both lakes a pronounced thermal stratification develops in the summer, thus the epilimnion receiving gross organic pollution behaves differently from the profundal. The lakes are each effectively divided into two bodies of water with limited water exchange between them, i.e. one major oligotrophic body and one minor more nutrient-rich. Since the 1950s both lakes have been exposed to heavy pollution of various kinds. In Lake Mjösa in 1975 and 1976 unpleasant algal blooms of the blue-green alga Oscillatoria bornetii fa. tenuis occurred. Bottom samples obtained at the same time revealed that the deep central bottoms of the lake were totally dominated by oligotrophic oligochaete indicators, i.e. by Stylodrilus heringianus and Spirosperma ferox, while the fauna of the upper profundal in the vicinity of domestic and agricultural sewage outfalls, wood processing industries, etc. was dominated by Limnodrilus hoffmeisteri and Tubifex tubifex in great abundance, indicating enriched conditions. Several other species indicative of eutrophy, were absent, most of them belonging to the genus Potamothrix. A fairly similar situation exists in Lake Tyrifjorden, where, for instance, in the shallow bay of Steinsfjorden — heavily eutrophied by agricultural wastes — blooms of blue-green algae have caused problems from time to time. The same oligochaete communities as in Lake Mjösa distinguish the central oligotrophic bottoms from the regionally more enriched upper profundal. The likely reasons for an intact profundal oligochaete fauna are great volumes of oxygen-rich hypolimnic water of low temperature and a high bottom/lake surface area ratio.     

Micro‐ and nano‐scale mineralogical characterization of Fe(II)‐oxidizing bacterial stalks

Neutrophilic, microaerobic Fe(II)‐oxidizing bacteria (FeOB) from marine and freshwater environments are known to generate twisted ribbon‐like organo‐mineral stalks. These structures, which are extracellularly precipitated, are susceptible to chemical influences in the environment once synthesized. In this paper, we characterize the minerals associated with freshwater FeOB stalks in order to evaluate key organo‐mineral mechanisms involved in biomineral formation. Micro‐Raman spectroscopy and Field Emission Scanning Electron Microscopy revealed that FeOB isolated from drinking water wells in Sweden produced stalks with ferrihydrite, lepidocrocite and goethite as main mineral components. Based on our observations made by micro‐Raman Spectroscopy, field emission scanning electron microscopy and scanning transmission electron microscope combined with electron energy‐loss spectroscopy, we propose a model that describes the crystal‐growth mechanism, the Fe‐oxidation state, and the mineralogical state of the stalks, as well as the biogenic contribution to these features. Our study suggests that the main crystal‐growth mechanism in stalks includes nanoparticle aggregation and dissolution/re‐precipitation reactions, which are dominant near the organic exopolymeric material produced by the microorganism and in the peripheral region of the stalk, respectively.