Carotenes from Mutants of the Dinoflagellate, Crypthecodinium cohnii

SYNOPSIS.
The carotenoid compositions of 15 nitrosoguanidine-induced mutants of Crypthecodinium cohnii , a heterotrophic dinoflagellate, were determined by chromatographic and mass spectral analyses. Wild-type C. cohnii grown with irradiation of 250 W/cm² visible light at 27 C synthesizes β-carotene (33%) and γ-carotene (67%) amounting to 0.083 mg/g dry wt. There are 4 types of carotenoid-deficient mutants: (I) albinos which synthesize no C₄₀-carotonoids: (II) albinos blocked at the level of phytoene desaturation; (III) cream-colored cells which accumulate mainly §–carotene, with phytoene and/or β-zeacarotene also present; and (IV) light-orange strains which synthesize reduced amounts of β-carotene and γ-carotene.
Dark-grown wild-type cells produced 35% as much carotenoids as light-grown cells. Inhibition studies revealed that diphenylamine (3 γ) caused phytoene accumulation; nicotine at 0.9 mM blocked the final cyclization, to cause γ-carotene to accumulate in wild-type cells. Inhibition by adenine and guanine (1.5 mM) of carotenogenesis was demonstrated for the first time in any system. The effect of these purines was similar to that of diphenylamine addition: phytoene desaturation was largely inhibited.
The carotenogenic system in this dinoflagellate is similar to that of green algae and higher plants, and is under nuclear genetic control.     

Geochemical investigation of growth in selected Recent articulate brachiopods

Buening, N. & Carlson. S. J. 1992 07 15: Geochemical investigation of growth in selected Recent articulate brachiopods.
Growth increments have traditionally been used to determine age and growth rates of shelled organisms, particularly bivalves. Brachiopod growth increments and the time span they represent are rather poorly understood, however. Geochemical analyses of trace element concentrations preserved in skeletal calcite may provide an alternative method to determine the age of Recent brachiopods and to interpret their patterns of growth. Magnesium is a particularly important trace element in skeletal calcite because it is thought to vary with temperature, growth rate. and taxonomic affiliation. Electron microprobe analyses of Mg concentrations in the Recent articulate, temperate water brachiopods Terebratulina unguicula and Terebrotalia transversa , have revealed two distinct ontogenetic patterns of Mg concentration. The primary ontogenetic pattern is characterized by elevated and more variable levels of Mg concentration during early growth. followed by lower, more stable Mg concentrations during growth after sexual maturity. This pattern appears to be related to a predictable decrease in growth rate through ontopeny. Secondary peaks of Mg superimposed on this primary pattern may represent growth spurts related to annual cycles of productivity. Preliminary Fourier analyses of patterns of Mg concentration provide additional support for this hypothesis. Thus, a record of productivity characterized by annual peaks of Mg concentration may well allow us to age individual brachiopods by means other than size-frequency histograms. growth lines, and other less precise and accurate methods. Brachiopods, growth. biomineralization, calcification, Terebratali transversa, Terebratulina Unogicui.a, magnesium, Calcium, geochemical. ontogeny .     

Hierarchy,spatial configuration,and nutrient cycling in a desert stream

Abstract Recent studies of nutrient cycling in Sycamore Creek in Arizona, USA, suggest that a thorough understanding requires a spatially explicit, hierarchical approach. Physical configuration determines the path that water follows as it moves downstream. Water follows flowpaths through surface stream components, the hyporheic zone beneath the surface stream, and the parafluvial (sand bar) zone. Characteristic biogeochemical processes in these subsystems alter nitrogen (N) species in transport, in part as a function of available concentrations of N species. At several hierarchical levels, substrate materials are an important determinant of nitrogen dynamics in desert streams. Sand is present in bars of variable size and shape, each of which can be considered a unit, interacting with the surface stream. Groups of these stream-sandbar units form a higher level, the reach. At the next higher scale, sandy reaches (runs) alternate with riffles. Where flowpaths converge, rates of N transformation are high and, as a result, change in concentration is a non-linear function of flowpath length. Disturbance by flash floods alters sandbar configuration. Between floods, the interaction of subsurface and surface flowpaths shapes configuration in each, thus a self-organizing element of spatial structure exists. Sandy runs are dominated by subsurface processes and are likely to be net nitrifiers while riffles are dominated by surface flow and are nitrogen fixers. Whether a stream ecosystem retains nitrogen, or transports it to downstream recipient systems, or is a net emitter of gaseous forms of N, depends upon the dynamics of a spatial mosaic of interacting elements. An understanding of the net effect of this mosaic requires a spatially explicit, hierarchical, multi-scale approach.