24 research outputs found

    Activation of wheat embryo calcium-regulated protein kinase by unsaturated fatty acids in the presence and absence of calcium

    Get PDF
    AbstractUnsaturated fatty acids (oleic, linoleic and arachidonic acids) markedly activate extensively purified wheat embryo Ca2+-regulated protein kinase in the absence of Ca2+ or at very low free Ca2+ levels (<0.4 μM). While oleic and linoleic acids also activate in the presence of Ca2+ (10−6−10−4 M), arachidonic acid inhibits at free Ca2+ greater than 10−5 M. Phosphatidylserine does not substantially activate in the absence of Ca2+ or the presence of high Ca2+. Stearic and arachidic acids are less effective than the unsaturated fatty acids as activators in the absence of Ca2+. This type of plant protein kinase may be regulated in vivo independently of Ca2+ through release of unsaturated fatty acids

    Convergence of Infinite Linear Systems

    No full text

    Understanding the fate of iron in a modern temperate estuary: Leirarvogur, Iceland

    No full text
    Fluvial dissolved Fe concentrations decrease upon mixing with seawater, resulting in the formation of Fe-floccules. However, a clear understanding of the fate of these floccules has yet to be established. Assessing how tidal processes affect the formation of Fe-colloids in the Leirárvogur estuary, SW Iceland, is an important step in understanding the formation and potential deposition of estuarine Fe-rich minerals within this estuarine system. The Leirárvogur estuary drains predominately Fe-rich basalt, increasing the likelihood of detecting changes in Fe-phases. Fluvial waters and local lake waters that drain into the estuary were compared and the effects of seasonal changes were considered, in an attempt to understand how varying end-members and external factors play a role in Fe-rich mineral formation. Aqueous and colloidal Fe concentrations were found to be greater towards the head of the Leirárvogur estuary, suggesting that potential Fe-rich minerals and complexes are forming at sites of fluvial input. Increasing suspended colloidal Fe towards the estuary mouth suggests that Fe-colloids are readily transported seaward
    corecore