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.     

Localized energization of the mitochondrial inner membrane by ATP.

Studies were made to determine whether the energy-dependent binding of ethidium to the mitochondrial inner membrane reflects the membrane potential or the energization of localized regions of the membrane. The number of binding sites of ethidium in mitochondria energized with ATP was 72 nmol/mg protein and decreased with increase in the amount of the ATPase system (F1 . F0) inactivated by oligomycin. These findings clearly show that the energy-dependent binding of ethidium to the mitochondrial inner membrane energized with ATP does not reflect the membrane potential, in good accord with the previous conclusion (Higuti, T., Yokota, M., Arakaki, N., Hattori, A. and Tani, I. (1978) Biochim. Biophys. Acta 503, 211-222), but that ethidium binds to localized regions of the energized membrane that are directly affected by ATPase (F1), reflecting the localized energization of the membrane by ATP.     

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.     

The structure of triple-stranded G-2C polynucleotide helices.

The thermal stability of a new polynucleotide complex has been used to establish the hydrogen-bonding structure of three-stranded C-G·CH⁺ helices. In the Hoogsteen structure, the 8NH₂ group of 8NH₂GMP can form a third hydrogen bond to the CH⁺ strand, but in the alternative structure, the 8NH₂ group can form no interbase hydrogen bonds. For the new complex, 8NH₂GMP·2 poly(C), a transition temperature of 80°C is observed under conditions in which the corresponding complex formed with 5′-GMP has a T_m of 20°C. We conclude from this 60° elevation of transition temperature that a third hydrogen bond is formed by the 8NH₂ group and that the structure must have Hoogsteen bonding. In order to be compatible with this structure in regular helices formed by U,C copolymers, A·2U bonding would also have to have a Hoogsteen structure.     

The physiological significance of the xanthurenic acid-insulin comples.

The xanthurenic acid-insulin complex was found to have similar immunological properties to native Zn-insulin. This complex showed less hormonal activity on glucose metabolism in adipose tissue than native An-insulin, but its activity was increased by addition of Zn2+ ions.     

Ribonucleic acid polymerase of germinating Bacillus cereus T.

It appears that a de novo synthesis of the deoxyribonucleic acid-dependent ribonucleic acid-polymerase in Bacillus cereus T takes place fairly late in outgrowth, at the onset of the vegetative cycle. Therefore, the ribonucleic acid-polymerase used by germinating spores is the one carried on from sporulating cells. However, the sporal enzyme is less soluble that the vegetative one, and its "core" is bound to two extra peptides. This complexing to other molecules could play a role in the regulation of gene expression during germination.     

Two new iridoid glucosides from Ixora chinensis

From leaves and twigs of Ixora chinensis, two new iridoid glucosides, ixoroside (1) and ixoside (7,8-dehydroforsythide) (2) along with known geniposidic acid (3) have been isolated and their structures have been established.     

Experimental Approach Reveals the Role of alx1 in the Evolution of the Echinoderm Larval Skeleton

Over the course of evolution, the acquisition of novel structures has ultimately led to wide variation in morphology among extant multicellular organisms. Thus, the origins of genetic systems for new morphological structures are a subject of great interest in evolutionary biology. The larval skeleton is a novel structure acquired in some echinoderm lineages via the activation of the adult skeletogenic machinery. Previously, VEGF signaling was suggested to have played an important role in the acquisition of the larval skeleton. In the present study, we compared expression patterns of Alx genes among echinoderm classes to further explore the factors involved in the acquisition of a larval skeleton. We found that the alx1 gene, originally described as crucial for sea urchin skeletogenesis, may have also played an essential role in the evolution of the larval skeleton. Unlike those echinoderms that have a larval skeleton, we found that alx1 of starfish was barely expressed in early larvae that have no skeleton. When alx1 overexpression was induced via injection of alx1 mRNA into starfish eggs, the expression patterns of certain genes, including those possibly involved in skeletogenesis, were altered. This suggested that a portion of the skeletogenic program was induced solely by alx1. However, we observed no obvious external phenotype or skeleton. We concluded that alx1 was necessary but not sufficient for the acquisition of the larval skeleton, which, in fact, requires several genetic events. Based on these results, we discuss how the larval expression of alx1 contributed to the acquisition of the larval skeleton in the putative ancestral lineage of echinoderms.