Effect of Ozone on the Activities of Reactive Oxygen Scavenging Enzymes in Rbc of Ozone Exposed Japanese Charr (Salvelinus Leucomaenis)

The effect of ozone exposure on the activities of reactive oxygen scavenging enzymes (SOD†, catalase, GSH-Px) in RBC of Japanese charr (Salvelinus leucomaenis) was examined. Ozone (0, 0.4 and 0.7 ppm as initial concentrations) was exposed to Japanese charr for 30 min, which definitely caused serious membrane damage to RBC of fish. Ozone exposure at 0.4 and 0.7 ppm decreased activities of both catalase and GSH-Px by 80 to 57+ of the control. On the other hand, the activities of SOD remained unaffected even by 0.7 ppm ozone exposure. A hypothesis on the RBC membrane damage and participation of SOD and heme-iron was proposed.     

N-terminally extended form of C-type natriuretic peptide (CNP-53) identified in porcine brain

C-type natriuretic peptide of 22 residues (CNP-22) is very recently identified in porcine brain as a third member of the mammalian natriuretic peptide family (1). Using a radioimmunoassay system newly established for CNP-22, we searched for CNP-related peptides in porcine brain. In addition to CNP-22, one major form of immunoreactive CNP was detected in porcine brain extracts, being isolated by immunoaffinity chromatography and reverse phase high performance liquid chromatography. By microsequence analysis, the peptide was deduced to be a 53-amino acid peptide carrying a CNP-22 sequence at the C-terminus, and was designated C-type natriuretic peptide-53 (CNP-53). CNP-53 was found to be a major molecular form of CNP in porcine brain.     

Isolation of NPY-25 (neuropeptide Y[12-36]), a potent inhibitor of calmodulin, from porcine brain

In the present purification of low molecular weight fractions (Mr: 2000-4000) containing basic peptides, twenty nmol of novel calmodulin binding peptide, possessing a potent affinity for calmodulin, was isolated from 18 kg of porcine brain. By analysis with gas phase sequencer, the sequence was determined to be APAEDLARYYSALRHYINLITRQRY. Carboxy terminus of the peptide was determined to be Tyr-NH2. The peptide was a carboxy terminal pentacosanepeptide of neuropeptide Y and was termed NPY-25. NPY-25 competitively inhibited the activation of cAMP-phosphodiesterase through CaM binding in a Ca++ dependent fashion, but did not inhibit the basal activity of cAMP phosphodiesterase. NPY-25 elicited a more potent activity than did neuropeptide Y. IC50 values of NPY-25 and Neuropeptide Y were 0.06 microM and 0.54 microM respectively.     

Evaluation of the timing to reduce the initial dose of antithyroid drugs in patients with Graves' disease.

The present study was undertaken to evaluate whether the normalization of the serum TSH level in a supersensitive assay during the initial treatment with antithyroid drugs (ATD) is a useful indicator for the reduction of the initial dose of ATD in 50 patients with hyperthyroidism due to Graves' disease. The initial dose of ATD was continued until the achievement of the euthyroid state, and was then reduced either before the serum TSH level was in the normal range in 9 of 29 patients treated with methimazole (MMI) (group MMI-1) and 8 of 21 treated with propylthiouracil (PTU) (PTU-1), or after the serum TSH level was in/above the normal range in 20 of 29 treated with MMI (MMI-2) and 13 of 21 treated with PTU (PTU-2). Although there were no significant differences in age, sex, thyroid function, prevalence of autoantibodies, goiter size, duration of the disease or the initial and modified doses of ATD, the mean durations of the administration of the initial dose of ATD in MMI-2 and PTU-2 were significantly longer than those in MMI-1 and PTU-1, respectively. As a result, 4 (44%) in group MMI-1, 20 (100%) in MMI-2, 2 (25%) in PTU-1 and 7 (54%) in PTU-2 developed low free T4 levels, and 1 (11%) in MMI-1, 15 (75%) in MMI-2 and 3 (23%) in PTU-2 developed low free T3 levels. Serum TSH levels increased over the normal range in 3 (33%) in MMI-1, 18 (90%) in MMI-2 and 5 (39%) in PTU-2.(ABSTRACT TRUNCATED AT 250 WORDS)     

Structure of cloned delta-globin genes from a normal subject and a patient with delta-thalassemia; sequence polymorphisms found in the delta-globin gene region of Japanese individuals.

The delta-globin genes of a normal Japanese and a Japanese patient with homozygous delta-thalassemia were cloned, and the nucleotide sequence of a region including the gene was determined. Comparison of the nucleotide sequences of these two individuals with that of pH delta 1, delta-globin clone from the gene library constructed by Maniatis et al., showed differences in the large intervening sequence (IVS 2), at positions 137, 151, 186, 188, 291, 292 and 540 as one base substitutions, at 339 and 823 as one base additions, at 548 as a one base deletion, and a 9 bp duplication between positions 651 and 659, and differences in the 3'-flanking sequence at 51 and 98 nucleotides 3' to the AATAAA sequence. However, in the region studied, no differences was observed in the nucleotide sequences of the normal subject and the patient with delta-thalassemia. Therefore, these differences may represent polymorphisms of the delta-globin gene present in Japanese individuals. These data suggest that IVS 2 is more divergent than other regions, and that a DNA region(s) other than the globin gene may affect expression of the gene.     

Late quaternary dynamics of pollen influx at mineral lake,Washington

Pollen influx analysis at Mineral Lake, Washington, indicates that immediately south of the Puget Lobe of the Fraser Glaciation, tundra was a characteristic vegetation until 16,300 years ago. Invasion ofPinus contorta began 17,500 years B.P., and boreal climax conifers (Abies, Picea andTsuga mertensiana), 16,300, but was temporarily interrupted by the Vashon advance (14,500–14,000 yr B.P.).Pseudotsuga menziesii began to grow in population 10,750 years ago, and woodland was established within a time span of 1,000 years. Modern lowland coniferous forests began to form 7,000 years ago. Logistic analysis of pollen abundance changes show that the intrinsic growth rate,r (yr⁻¹), of pioneer species (e.g. 0.024–0.026 inPteridium aquilinum) is higher than that of climax species (e.g. 0.003 inThuja plicata).P. menziesii, a subclimax species, shows an intermediater value (0.013) between these two ecologically different taxa. The absoluter value ofP. contorta (−0.011) is only slightly lower than that ofP. menziesii, although their replacement began almost simultaneously. Thus competition between these species was intense before the inflection point ofPinus curve 10,100 years ago. At this time, forest gaps became abundantly available forPseudotsuga, as indicated by a peak of the diagnostic factor (the reciprocal of the pollen influx).     

The concentrations and thermodynamic activities of cations in intact Bryopsis chloroplasts

The internal cation levels of chloroplasts isolated from a green sea alga, Bryopsis maxima, were studied. Atomic absorption spectroscopy, combined with the determination of the sorbitol-impermeable and water-permeable spaces, revealed that chloroplasts contain an extremely high concentration of K⁺ and high levels of Na⁺, Mg²⁺ and Ca²⁺. A method was developed to estimate the thermodynamic activities of monovalent and divalent cations present in chloroplasts. pH changes induced by the addition of an ionophore (plus an H⁺ carrier), which makes the outer limiting membranes of chloroplasts permeable to both a cation and H⁺, were determined. Provided that the external pH was set equal to the internal pH, the internal concentration of the cation was estimated by determining the external cation concentration which gave rise to no electrochemical potential difference of the cation and hence no pH change on addition of the ionophore. The internal pH was determined by measuring distributions of radioactive methylamine and 5,5-dimethyloxazolidine-2,4-dione between the chloroplast and medium (Heldt, H.W., Werdan, K., Milovancev, M. and Geller, G. (1973) Biochim. Biophys. Acta 314, 224–241). The internal pH was also estimated by measuring pH changes caused by the disruption of the outer limiting membrane with Triton X-100. The results indicate that a significant part of the monovalent cations and most of the divalent cations are attracted into a diffuse layer adjacent to the negatively charged surfaces of membranes and proteins, or form complexes with organic and inorganic compounds present in the intact chloroplasts.     

Nitrate and nitrite in interstitial waters of eelgrass beds in relation to the rhizosphere

The distribution of nitrate and nitrite in the interstitial water of the sediment of eelgrass (Zostera marina) bed of Izembek Lagoon, Alaska, were investigated. Their concentrations were relatively high (0 to 9.8 μg-at.N·1^?1, average 4.8 for nitrate; 0 to 4.0 μ-at.N·1^?1, average 1.9 for nitrite) although the sediments were anoxic and contained hydrogen sulphide. The rates of bacterial denitrification measured by ¹⁵N tracer technique ranged from 0.49×10^?10 to 1.2 × 10^?9 g-atN·g^?1·h^?1. When a steady state is maintained, the loss of nitrate and nitrite must be balanced by their production by bacterial nitrification. Experimentally determined rate of nitrification in the sediment was of the same order. A model experiment demonstrated that oxygen is transported from leaves to rhizomes and roots of eelgrass and released into the sediment. The oxygen is used for nitrification in the rhizosphere in anoxic sediments.     

Denitrification and Ammonia Formation in Anaerobic Coastal Sediments

Simultaneous determinations of nitrogen gas production, ammonia, and particulate organic nitrogen formation in the coastal sediments of Mangoku-Ura, Simoda Bay, and Tokyo Bay were made by using the ¹⁵N-label tracer method. The rate of nitrogen gas production in the sediment surface layer was about 10⁻² μg atom of N per g per h, irrespective of the location of the sediments examined. [¹⁵N]ammonia and -particulate organic nitrogen accounted for 20 to 70% of the three products, and after several hours of incubation, the major fraction of nondenitrified ¹⁵N in Mangoku-Ura and Simoda Bay sediments was recovered as ammonia. In Tokyo Bay sediments, particulate organic nitrogen was produced at a greater rate than was ammonia. The reduction rate data suggest that the pathway of nitrate reduction to ammonia is important in coastal sediments.