DETERMINANTS OF THE SELECTIVE PHAGOCYTOSIS OF CARCINOGENIC PARTICULATE NICKEL COMPOUNDS

Certain inorganic nickel compounds such as crystalline NiS and Ni(,3)S(,2) are potent inducers of carcinogenesis and in vitro cell transformation, while several closely-related compounds such as amorphous NiS are essentially devoid of genotoxic activity. The phenomenon of selectivity of phagocytosis among such particulate nickel compounds has been hypothesized to account for their widely varying toxicological potency, yet the determinants of this selectivity have not been well characterized. Extracellular medium composition, particle dissolution, and particle surface charge were examined as potential determinants of selective phagocytosis for the carcinogenic crystalline and noncarcinogenic amorphous modifications of NiS. Selectivity and avidity of uptake of crystalline NiS by CHO cells was not dependent upon serum: phagocytosis of crystalline, but not amorphous NiS proceeded readily in a minimal salts/glucose medium at 37(DEGREES)C. The evolution of phagocytosis-inhibiting Ni(II) from the surface of amorphous NiS particles did not demonstrably contribute to the lower uptake of these noncarcinogenic particles despite their somewhat greater dissolution rate than the readily phagocytosed crystalline NiS particles. Significant differences in surface charge were noted between crystalline and amorphous NiS, the former being more negative in charge in distilled water suspension. Exposure of amorphous NiS particles to the vigorously reducing environment of a LiAlH(,4) solution under an inert atmosphere resulted in the particles' acquisition of a more negative surface charge. Amorphous NiS particles thus treated were phagocytosed by CHO cells to an extent similar to that of untreated crystalline NiS particles and likewise were shown to induce morphological transformation of primary Syrian hamster embryo cells with a similar potency. The potentiation of uptake characteristic of LiAlH(,4)-treated amorphous NiS was lost gradually upon storage of particles in ambient oxygenated atmosphere and was lost rapidly by apparent particle surface oxidation in aerated distilled water suspensions aged for up to 7 days. Concomitant with this loss of uptake there occurred a loss of negative surface charge. These results suggest the predominant role of particle surface charge rather than adsorbed serum components or particle dissolution as a determinant of selective phagocytosis among particulate nickel compounds. ^

Description and chemical composition of ferromanganese encrustations and deposits in the Atlantic Ocean from R/V Atlantis II cruises 20, 42, 60, 85; R/V Chain cruise 35; R/V Knorr cruise 61 and RRS Shackleton cruise 75/1 stations

Chemical and mineralogical compositions of ferromanganese oxide coatings on rocks dredged from the New England Seamounts, the Sierra Leone Rise and the Mid-Atlantic Ridge near the Equator have been determined in an investigation of regional differences in Atlantic ferromanganese deposits. Most encrustations are clearly of hydrogenous origin, consisting mainly of todorokite and delta MnO2, but several recovered from the equatorial fracture zones may be hydrothermal accumulations. Differences in the chemistry of the water column and in growth rates of the ferromanganese coatings may be important in producing this regional contrast in composition. Fine-scale changes in element abundances within the encrustations indicate that the nature of the substrate has little influence on compositional variations.

Chemical composition of iron-manganese and phosphate rocks from aseismic ridges of the Indian Ocean and from the continental slope of the Southeast Africa

Study of chemical composition of 26 samples collected at depths from 400 to 1400 m on vertex surfaces of the Southeast Indian Ridge, Mascarene Ridge, Madagascar Ridge, and Mozambique Ridge, as well as on the upper part of the Southeast Africa continental slope showed that the samples represent three groups of rocks: 1) low phosphate or phosphate-free ferromanganese rocks, 2) phosphate ferromanganese rocks 3) phosphorites and phosphatized limestones.

Compilation of measurements from two interdisciplinary STAR-shaped surveys in the North Sea: The ZISCH - Dataset

The measurements were obtained during two North Sea wide STAR-shaped cruises during summer 1986 and winter 1987, which were performed to investigate the circulation induced transport and biologically induced pollutant transfer within the interdisciplinary research in the project "ZISCH - Zirkulation und Schadstoffumsatz in der Nordsee / Circulation and Contaminant Fluxes in the North Sea (1984-1989)". The inventory presents parameters measured on hydrodynamics, nutrient dynamics, ecosystem dynamics and pollutant dynamics in the pelagic and benthic realm. The research program had the objective of quantifying fluxes of major budgets, especially contaminants in the North Sea. In spring 1986, following the phytoplankton spring bloom, and in late winter 1987, at minimum primary production activity, the North Sea ecosystem was investigated on a station net covering the whole North Sea. The station net was shaped like a star. Sampling started in the centre, followed by the northwest section and moving counter clockwise around the North Sea following the residual currents. By this strategy, a time series was measured in the central North Sea and more synoptic data sets were obtained in the individual sections. Generally advection processes have to be considered when comparing the data from different stations. The entire sampling period lasted for more than six weeks in each cruise. Thus, a time-lag should be considered especially when comparing the data from the eastern and the western part of the central and northern North Sea, where samples were taken at the beginning and at the end of the campaign. The ZISCH investigations represented a qualitatively and quantitatively new approach to North Sea research in several respects. (1) The first simultaneous blanket coverage of all important biological, chemical and physical parameters in the entire North Sea ecosystem; (2) the first simultaneous measurements of major contaminants (metals and organohaline compounds) in the different ecosystem compartments; (3) simultaneous determinations of atmospheric inputs of momentum, energy and matter as important ecosystem boundary conditions; (4) performance of the complex measurement program during two seasons, namely the spring plankton bloom and the subsequent winter period of minimal biological activity; and (5) support of data analysis and interpretation by oceanographic and meteorological numerical models on the same scales.

(Table 2) Layer-by-layer chemical composition of barite crusts from the Atlantis II Deep of the Red Sea rift zone

Results of studies of hydrothermal sulfide-sulfate rocks occurring in the Atlantis II Deep of the Red Sea are reported in the paper.