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  • Other Sources  (2)
  • Bentham Science  (1)
  • Wiley  (1)
  • American Physical Society
  • 1
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    Bentham Science
    In:  Protein & Peptide Letters, 23 (11). pp. 1013-1023.
    Publication Date: 2019-07-10
    Description: Prostaglandin H synthase (PGHS) catalyzes the biosynthesis of PGG2 and PGH2, the precursor of all prostanoids, from arachidonic acid (AA). PGHS exhibits two enzymatic activities following a branched-chain radical mechanism: 1) a peroxidase activity (POX) that utilizes hydroperoxide through heme redox cycles to generate the critical Tyr385 tyrosyl radical for coupling both enzyme activities; 2) the cyclooxygenase (COX) activity inserting two oxygen molecules into AA to generate endoperoxide/hydroperoxide PGG2 through a series of radical intermediates. Upon the generation of Tyr385 radical, COX catalysis is initiated, with C13 pro-S hydrogen abstraction from AA by Tyr385 radical to generate arachidonyl substrate radical. Oxygen provides a large driving force for the subsequent fast steps leading to the formation of PGG2, including radical redistributions, ring formations, and rearrangements. On the other hand, if the supply of oxygen is severed, equilibrium between arachidonyl radical and tyrosyl radical(s) biases largely towards the latter. In this study, we demonstrate that such equilibrium is shifted by many factors, including temperature, chemical structures of fatty acid substrates and limited supply of oxygen. We also, for the first time, reveal that this equilibrium is significantly affected by co-substrates of POX. The presence of efficient POX co-substrates, which reduces heme to its ferric state, apparently biases the equilibrium towards arachidonyl radical. Therefore a dynamic interplay exists between the two activities of PGHS.
    Type: Article , PeerReviewed
    Format: text
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  • 2
    Publication Date: 2023-02-08
    Description: Key Points: • Antarctic meltwater forcing induces an overall global cooling but regional warming in East Asia • Antarctic meltwater forcing can shift the Intertropical Convergence Zone northward and suppress convection over the Western North Pacific • Suppressed convection in the Western North Pacific is responsible for the regional warming of East Asia via atmospheric teleconnection. In recent decades, Antarctic ice sheet/shelf melting has been accelerated, releasing freshwater into the Southern Ocean. It has been suggested that the meltwater flux could lead to cooling in the Southern Hemisphere, which would retard global warming and further induce a northward shift of the Intertropical Convergence Zone (ITCZ). In this study, we use experimental ensemble climate simulations to show that Antarctic meltwater forcing has distinct regional climate impacts over the globe, leading in particular to regional warming in East Asia, which offsets the global cooling effect by the meltwater forcing. It is suggested that Antarctic meltwater forcing leads to a negative precipitation anomaly in the Western North Pacific (WNP) via cooling in the tropics and the northward shift of the ITCZ. This suppressed convection in WNP induces an anticyclonic flow over the North Pacific, which leads to regional warming in East Asia. This hypothesis is supported by analyses of interensemble spread and long-term control simulations.
    Type: Article , PeerReviewed , info:eu-repo/semantics/article
    Format: text
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