Structure and Role of the Five Glycopeptides of Human IgM Immunoglobulins

Carbohydrate is attached at five sites in the constant sequence region of the µ heavy chain of human IgM. The oligosaccharides are of two kinds, simple and complex and affect the conformation and properties of macroglobulins.     

Difference in the distribution and speciation of cellular nickel between nickel‐tolerant and non‐tolerant Nicotiana tabacum L. cv. BY‐2 cells

To evaluate Ni dynamics at the subcellular level, the distribution and speciation of Ni were determined in wild‐type (WT) and Ni‐tolerant (NIT) tobacco BY‐2 cell lines. When exposed to low but toxic levels of Ni, NIT cells were found to contain 2.5‐fold more Ni (14% of whole‐cell Ni values) in their cell walls than WT cells (6% of whole‐cell Ni values). In addition to higher levels of Ni in the apoplast, a higher proportion (94%) of symplastic Ni was localized in the vacuoles of NIT cells than in the vacuoles of WT cells (81%). The concentration of cytosolic Ni in the NIT cells was significantly lower (18 nmol g^?1 FW) than that in the WT cells (85 nmol g^?1 FW). In silico simulation showed that 95% of vacuolar Ni was in the form of Ni‐citrate complexes, and that free Ni²⁺ was virtually absent in the NIT cells. On the other hand, the amount of free metal ions was markedly increased in WT cells because free citrate was depleted by chelation of Ni. A protoplast viability assay using BCECF‐AM further demonstrated that the main mechanism that confers strong Ni tolerance was present in the symplast as opposed to the cell wall.     

Photoperiodic induction of diapause in the silkworm, Bombyx mori: location of the photoreceptor using a chemiluminescent paint

ABSTRACT. To locate the photoreceptor involved in the photoperiodic induction of diapause in Bombyx mori L., covering of larval head with black paint or local illumination using chemiluminescent paint was carried out. A silkworm race showing a response of long-day type during the larval stage was employed. The results demonstrated that the photoreceptor is located in the head but is extraocular. The optical properties of the larval body suggest that during the first and second stadia light is admitted through the translucent clypeus of the head, but during later stadia enters over the entire larval body including the head, and that it reaches the cerebral lobe where a photoreceptor is possibly located.     

ONTOGENY OF CHICKEN HEMOGLOBIN. III. IMMUNOLOGICAL STUDY OF THE HETEROGENEITY OF HEMOGLOBIN IN DEVELOPMENT

By applying the double diffusion technique of Ouchterlony and the immunoelectrophoresis, sequence in the appearance of antigens reactive with antisera against HbCOs from 5-day embryos and adult chickens, and the major component of adult HbCO in the course of chicken development has been studied.
Antigenic components reacting to antiserum against HbCO from 5-day embryos have been detected throughout development. Three globin-like components specific to early embryos are detectable in embryos to 2 days of incubation. Two Hb components are detectable in embryos from 3 to 5 days of incubation; one is apparently specific to embryos, while the other seems to be somewhat different from adult Hb. After 6 days of incubation only one adult Hb component is detectable.
Antigenic components reacting to antiserum against HbCO from adults have also been detectable throughout embryonic life. One globin-like component specific to early embryos can be found in embryos to 2 days of incubation. One or two Hb components which are probably specific to embryos can be detected in embryos from 3 to 5 days of incubation. After 6 days of incubation one adult Hb component is detectable, while one globin-like component specific to adults can be found after 15 days of incubation. Further, the other globin-like component is detectable after 3 days of incubation.
Antigenic components reacting to antiserum against the major component of adult HbCO have been detected throughout development; one which seems to be somewhat different from either adult Hb components can be found in embryos from 2 to 5 days of incubation, while the other which is identical with the major component of adult Hb is detectable after 6 days of incubation.     

Molecular characterization of microbial communities in fault-bordered aquifers in the Miocene formation of northernmost Japan

We investigated the diversity and distribution of archaeal and bacterial 16S rRNA gene sequences in deep aquifers of mid‐ to late Miocene hard shale located in the northernmost region of the Japanese archipelago. A major fault in the north‐west–south‐east (NW–SE) direction runs across the studied area. We collected three groundwater samples from boreholes on the south‐west (SW) side of the fault at depths of 296, 374 and 625 m below ground level (m.b.g.l.) and one sample from the north‐east (NE) side of the fault at a depth of 458 m.b.g.l. The groundwater samples were observed to be neutral and weakly saline. The total microbial counts after staining with acridine orange were in the order 10⁵?10⁶ cells mL^?1 and 10³ cells mL^?1 in the aquifers to the SW and to the NE of the fault, respectively. A total of 407 archaeal and bacterial 16S rRNA gene sequences (204 and 203 sequences, respectively) were determined for clone libraries constructed from all groundwater samples. Phylogenetic analyses showed that the libraries constructed from the SW aquifers were generally coherent but considerably different from those constructed from the NE aquifer. All of the archaeal clone libraries from the SW aquifers were predominated by a single sequence closely related to the archaeon Methanoculleus chikugoensis, and the corresponding bacterial libraries were mostly predominated by the sequences related to Bacteroidetes, Firmicutes and δ‐Proteobacteria. In contrast, the libraries from the NE aquifer were dominated by uncultured environmental archaeal clones with no methanogen sequences and by β‐proteobacterial clones with no sequences related to Bacteroidetes and δ‐Proteobacteria. Hence, the possible coexistence of methanogens and sulphate reducers in Horonobe deep borehole (HDB) on the SW side is suggested, particularly in HDB‐6 (374 m.b.g.l.). Moreover, these organisms might play an important geochemical role in the groundwater obtained from the aquifers.