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Arsenobetaine‐decomposing Ability of Marine Microorganisms Occurring in Particles Collected at Depths of 1100 and 3500 Meters
Author(s) -
Hanaoka Ken'ichi,
Kaise Toshikazu,
Kai Norihisa,
Kawasaki Yasuhiro,
Miyasita Hideaki,
Kakimoto Kenji,
Tagawa Shoji
Publication year - 1997
Publication title -
applied organometallic chemistry
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.53
H-Index - 71
eISSN - 1099-0739
pISSN - 0268-2605
DOI - 10.1002/(sici)1099-0739(199704)11:4<265::aid-aoc579>3.0.co;2-w
Subject(s) - arsenobetaine , photic zone , chemistry , environmental chemistry , microorganism , arsenic , degradation (telecommunications) , deep sea , inorganic arsenic , mineralogy , oceanography , phytoplankton , organic chemistry , bacteria , geology , paleontology , nutrient , telecommunications , computer science
The arsenobetaine‐decomposing ability of microorganisms occurring in sinking particles, which play a main role in the vertical transport of organic substances produced in the photic zone, was investigated. The microorganisms in particles collected in the deep sea, 1100 and 3500 m in depth, clearly showed decomposing ability. With the particles from 1100 m, the degradation products were the same as those produced by microorganisms occurring in sources in the photic zone, i.e. trimethylarsine oxide (TMAO), dimethylarsinic acid (DMA) and inorganic arsenic(V). At 3500 m, the degradation activity was diminished, smalls amount of DMA and TMAO being produced. These results suggest that arsenobetaine contained in the animals starts to degrade immediately after the death of the animals and their transformation to particles. The degradation of arsenobetaine to inorganic arsenic in our tentative arsenic cycle in marine ecosystems (inorganic arsenic to inorganic arsenic via the biosynthesis of arsenobetaine) may apply to the deep sea as well as to the photic zone. © 1997 by John Wiley & Sons, Ltd.