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21 April 2006 The bottom oxygen border of bioluminescence distribution in ocean
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Proceedings Volume 6160, Twelfth Joint International Symposium on Atmospheric and Ocean Optics/Atmospheric Physics; 61602O (2006) https://doi.org/10.1117/12.675900
Event: Twelfth Joint International Symposium on Atmospheric and Ocean Optics/Atmospheric Physics, 2005, Tomsk, Russian Federation
Abstract
From materials of forwarding researches follows, that the depth of deposition of the bottom border of bioluminescence plankton has not correlation with any of measurable hydrological parameters. As the reaction of bioluminescence is oxygen depended, it was logical to assume, that the situation of the bottom maximum of luminescence plankton is determined by concentration of oxygen. The data of vertical distribution of bioluminescence intensity of plankton and concentration of oxygen received in the Black Sea and near to east coast of America were investigated. Is established, that the deep maximum of bioluminescence of plankton is found out between isooxygen 0.35 and 0.20 ml/l. At concentration of oxygen in water is lower 0.10-0.20 ml/l the bioluminescence of plankton it is not found out.
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Valerii Zavoruev "The bottom oxygen border of bioluminescence distribution in ocean", Proc. SPIE 6160, Twelfth Joint International Symposium on Atmospheric and Ocean Optics/Atmospheric Physics, 61602O (21 April 2006); https://doi.org/10.1117/12.675900
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