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  • 1980-1984  (3)
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Year
  • 1
    Electronic Resource
    Electronic Resource
    Oxford [u.a.] : International Union of Crystallography (IUCr)
    Acta crystallographica 39 (1983), S. 134-136 
    ISSN: 1600-5759
    Source: Crystallography Journals Online : IUCR Backfile Archive 1948-2001
    Topics: Chemistry and Pharmacology , Geosciences , Physics
    Type of Medium: Electronic Resource
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  • 2
    ISSN: 1432-1793
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract During a cruise to the eastern Canadian Arctic (Northern Baffin Bay) in the summer of 1980, we took advantage of the 24-h photoperiod to conduct a 32-h time course experiment of 14C accumulation under natural solar radiation. The degree of non-linearity in the time course was judged against a time-dependent curve of radioactivity constructed by cumulatively adding the amount of 14C taken up in sequential short (2 h) incubations of plankton held in a replicate bottle but left unlabelled until removed for assay. Departure from linearity was due first to decreasing rates of 14C incorporation into polysaccharides and then into lipids. There was a close correspondence between 14C incorporation into proteins in the 32-h incubation and in the sequence of short incubations. These observations are consistent with patterns in utilization of photosynthetic end-products established from laboratory studies of unicellular algal cultures. Based on parallel or independent control experiments, it was judged that complicating factors such as diel light changes, nitrogenous nutrient exhaustion, bottle size effects or inhibitory conterminants in NaH14CO3 stock solutions would not seriously affect our interpretation that non-linearity resulted from catabolic loss of radiocarbon.
    Type of Medium: Electronic Resource
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  • 3
    ISSN: 1432-2056
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Summary Marine microbial plankton from eastern Canadian Arctic waters have the remarkable ability of rapidly accumulating nutrients (amino acids, glucose, phosphate) at mesobiotic temperatures (≈30°C) after an acclimation period of a few hours. Curves of the nutrient uptake response to temperature established before and after an 8 h acclimation period at 30°C showed that maximum uptake rates attained much higher values and were established at much higher temperatures after the acclimation period. This enhancement was inhibited by chloramphenicol (but not cycloheximide) and occurred even when the possibility of bacterial enhancement due to animal and plant death was reduced by prior removal of organisms using a screen of 1 μm nominal pore diameter. The enhancement at high temperatures was evidenced only in heterotrophic but not in photosynthetic activities and was concominant with large increases in the apparent activity of microbial DNA synthesis and bacterial cell density. The enhancement may have been due to a rapid and opportunistic growth of presumed non-psychrophilic members of the bacterioplankton.
    Type of Medium: Electronic Resource
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