期刊
AQUATIC SCIENCES
卷 80, 期 2, 页码 -出版社
SPRINGER BASEL AG
DOI: 10.1007/s00027-018-0564-5
关键词
Phosphorus cycle; Dissolved organic phosphorus; Nutrient cycling; Colloidal phosphorus; Plankton
资金
- National Science and Engineering Research Council of Canada
Phosphorus (P) in lake water is commonly partitioned into particulate P and dissolved P by membrane filtration, and dissolved P is then fractionated into soluble reactive P (SRP, reactive with molybdate) and dissolved unreactive or organic P (DOP). Much of what is known about DOP is derived from radiotracer studies using gel chromatography, and summarized by a kinetic model (Lean, Science 179: 678-680, 1973a; Lean, J Fish Res Board Can 30: 1525-1536, 1973b). Since this work, several relevant discoveries have been made on the role of enzymes, viruses and zooplankton in regenerating dissolved P, and the role of filtration damage in generating dissolved P in filtrates. Herein we present the results of new radiotracer experiments on the fate of DOP in lake water filtrates, consistent with the hypothesis that some of the high molecular weight organic P breaks down spontaneously to smaller molecules, which in turn break down to PO43-. We use inhibitors, including competitive inhibitors of phosphatases and a commercial product (RNA-later (R)) to support the hypothesis that the larger molecules include nucleic acids, and that the smaller molecules are substrates for alkaline phosphatase. We also find that colloidal P (i.e., P > 5000 MW according to gel filtration) includes some virus-sized material that can be collected on 0.02 or 0.03 mu m filters. Finally, we provide a new model of the cycling of epilimnetic P that is consistent with these and earlier observations.
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