ALBERT

Notes: Abstract Precambrian granulites of the Aldan shield in southern Yakutia, USSR, form a massif of 200,000 km2 bounded by younger fold-belts to the south, west and east. The massif consists of several blocks that reflect a primary heterogeneity of composition and differences in structural and thermodynamic evolution of different parts of the area. According to structural and petrological data the massif can be divided into two megablocks: eastern Aldan and western Aldan. They are separated by a narrow meridional fold-belt. Structural evolution of this central zone was determined by the geodynamics of the mega-blocks and was completed in the late Archaean. Towards the south, this central zone is ‘transformed’into the relatively small Sutam block adjoining the Stanovoy fold-belt that bounds the Aldan shield on the south. The Sutam block is separated from the other structural units of the Aldan shield by a system of north trending grabens filled by post-Archaean sediments.The Aldan shield is composed of Archaean high-grade granulites, while the Stanovoy fold-belt, to the south, consists of highly foliated Proterozoic rocks metamorphosed under relatively lower-grade conditions. However, relics of the granulites are mapped within the fold-belt. They contain high-grade assemblages (e.g. Opx + Sil + Qz, Sap + Qz, Opx + Gr + Sil, etc.). One of the relics, the Tokskii block, which is only slightly touched by diaphthoresis, is located in the southeastern part of the Stanovoy fold-belt. Metamorphic conditions of the Tokskii block are compared with those of the Sutam block and a similar evolution of the units is revealed.Mineral assemblages and mineral compositions do not vary within each unit, but they change in a north-south direction. The Opx + Sil + Qz assemblage has been found only in Sutam and Tok, but not in eastern Aldan and western Aldan. The Sap + Qz assemblage has been found in the Tokskii block but has not yet been found in the Sutam block. The pyrope content in garnets, from metapelites of both blocks, is significantly higher than that from the Aldan (eastern and western blocks) rocks to the north. The most important assemblages from different units of the Aldan shield have been studied using the electron microprobe in order to unravel the metamorphic evolution of the granulites and thus to deduce the thermodynamic regime of this evolution. A geodynamic model for the Aldan shield is discussed in terms of Archaean island arc development.

Notes: The effect of sulfanilamide addition on the TBA numbers of meats cured with 0 - 200 ppm levels of sodium nitrite has been investigated. Results indicate that the TBA numbers of meats cured with 100 - 200 ppm level were always larger when sulfanilamide was present than in its absence. However, at low levels of 0 - 50 ppm sodium nitrite the TBA values were always lower in the presence of sulfanilamide. This effect is substantial and has apparently not been observed before. A possible explanation has been put forward. In all cases a distillation method was employed to evaluate TBA numbers.

Notes: Wheat starch was processed in a 19 mm diameter split-barrel laboratory extruder under varying conditions of barrel temperature (79–121oC), screw speed (50, 100 rpm) and moisture content (25, 30%). Final product and samples removed from along the barrel length were examined for changes in molecular size by dilute solution viscometry. Final products were also examined for paste viscosity and estimated degree of cook. A mathematical model was developed which relates the residence time of the starch in the barrel, the nominal shear stress acting on the starch and the degree of cook of the product to the extent of molecular degradation of the starch. Solution viscometry was found to be more rapid than gel permeation methods previously used to determine the extent of molecular changes.

Notes: A graft-versus-host reaction (GVHR) directed against DBA/2 non-H-2 antigens alone can be induced by grafting B10.D2 bone marrow and spleen cells intravenously to heavily irradiated, H-2d compatible (DBA/2 x B10.D2)F1 adult mice. Under the experimental conditions used, only 0-l0% of recipients survive, but the survival is greatly increased by donor alloimmunization, a few days prior to grafting, against host-specific (DBA/2) non-H-2 antigens and non-specific (foreign) H-2 antigens. The increased survival is mediated by alloimmunization-activated suppressor cells which can decrease the intensity of the immune reaction developed by normal B10.D2 cells both in vivo (GVHR) and in vitro (proliferative response measured in mixed lymphocyte culture, MLC). The present experiments were designed to explore the antigenic requirements for inducing suppression. The results showed that in GVHR the protective effect induced by donor alloimmunization against the specific non-H-2 antigens, which leads to 70-80% survival, is due primarily, if not entirely, to immunization against Mls2 antigens. Results of MLC experiments confirmed this conclusion, showing that immunization against Mlsa antigens is sufficient to account for the suppressive effect induced by the specific immunization. In addition, they indicated that the nonspecific protective effect induced by donor alloimmunization against foreign H-2 antigens, which leads to 20-30% survival, is due to immunization against antigens encoded by the K and/or I region(s) of the H-2 complex; immunization against D region encoded antigens alone has no effect.

Notes: Abstract The evolutionary relationship of the RuBisCO large subunit gene(s) (rbcL) of several prokaryotes was examined using the technique of heterologous DNA hybridization. Restriction fragments of cloned rbcL from Anacystis nidulans 6301, Chlamydomonas reinhardtii, Rhodospirillum rubrum, and maize were nick-translated and used as probes. The C. reinhardtii and maize probes hybridized with restriction fragment(s) only from cyanobacteria: Agmenellum quadruplicatum, Fremyella diplosiphon, and Mastigocladus laminosus. In addition, the A. nidulans probe hybridized with restriction fragment(s) from Alcaligenes eutrophus, Chromatium vinosum, Nitrobacter hamburgensis, Paracoccus denitrificans, Pseudomonas oxalaticus, Rhodomicrobium vannielii, Rhodopseudomonas capsulata, Rhodopseudomonas palustris, Rhodopseudomonas sphaeroides, Thiobacillus intermedius, Thiobacillus neapolitanus, and Thiothrix nivea. The elucidated fragment of Rhodopseudomonas species is presumably for the Form I RuBisCO LSU of these organisms. The R. rubrum probe hybridized only to a restriction fragment(s) from R. capsulata, R. palustris, R. sphaeroides, T. neapolitanus, and T. nivea. The fragment(s) of Rhodopseudomonas species is the Form II rbcL of these organisms. The restriction fragments of T. neapolitanus and T. nivea were also different from those elucidated by the A. nidulans probe, suggesting the presence of a second (different) rbcL in these organisms. Positive hybridization was not obtained using any of the probes with DNA from Beggiatoa alba, Chlorobium vibrioforme or Chloroflexus aurantiacus. It appears that all rbcL have evolved from a common ancestor. Our data are consistent with and supportive of the evolutionary scheme for RuBisCO proposed by Akazawa, Takabe, and Kobayashi [1].

Notes: The paper gives a detailed description of the technique for measuring azimuthal anisotropy which was suggested earlier by Vinnik, Kosarev & Makeyeva (1984) and used by Kind et al. (1985). The technique is based on the observations of long-period converted phases like SKS. Additionally, we describe a generalization of this approach which makes use of long-period S-waves of arbitrary polarization. Both modifications were applied to records of the GRF array in southern Germany. The results of this analysis, if combined with the data on Pn velocities (Bamford 1977), suggest that the direction of the fast velocity in the lithosphere of the region varies with depth.