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Bacteria-phosphate interactions in Upper Klamath Lake sediments

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Title Bacteria-phosphate interactions in Upper Klamath Lake sediments
Names Harrison, Michael John (creator)
Morita, Richard (advisor)
Date Issued 1970-05-04 (iso8601)
Note Graduation date:1970
Abstract Interactions between sediment bacteria and available phosphate
necessary for algal production in a eutrophic lake were studied.
Twenty percent of the organisms isolated solubilized phosphate forms
such as CaHPO₄, Ca₃(PO₄)₂, FePO₄, Mg₃(PO₄)₂ and Al₂(PO₄)₂.
Solubilization of phosphates occurred under conditions of aerobic
growth.
Upon quantitative analysis, some isolates were capable of
solubilizing up to 87% of the inorganic phosphate.
Solubilization was
associated with carbohydrate metabolism and the production of organic
acids, which function as chelating agents.
Organic acids that
solubilize phosphates include lactic, acetic, glycolic, pyruvic, citric,
glyceric, glucuronic and gluconic acids.
Carbohydrates added to
sediment resulted in increased microbial activity and an increase in
the level of soluble phosphate.
Addition of precipitating ions (Ca⁺⁺ and Fe⁺⁺⁺) reduced the level of soluble phosphate in the sediment, but the soluble phosphate fraction could be increased by the stimulation of
microbial activity.
A. cyclic liberation of phosphate was associated with death during
cryptic growth.
Reversible liberation of phosphate was observed when
facultative and aerobic organisms were shifted from aerobic to an
anoxic environment.
Phosphate solubilization, liberation of phosphate
with cryptic growth, and the reversible uptake and liberation of
phosphate by microorganisms, with changes in aeration, may be of
significance in the exchange of phosphates between the water and the
sediment in Upper Klamath Lake.
Genre Thesis/Dissertation
Topic Upper Klamath Lake (Or.)
Identifier http://hdl.handle.net/1957/46227

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