Phosphorus is most commonly found in its fully oxidized state (P+5) of phosphate and phosphate esters, which are incorporated into biomolecules such as nucleotides, nucleic acids, and phospholipids. Phosphite, a reduced form of phosphorus (P+3), is found in rivers, lakes, sediments, and oceans, and is of suspected biological origin. However, there is no conclusive evidence of phosphite production in axenic culture, nor any clear mechanistic pathway for phosphite biosynthesis. Given that the phosphate/phosphite redox couple heavily favors oxidation (-690 mV vs. NHE), phosphite has been proposed to be a downstream product in the biosynthesis or degradation of phosphonates, molecules containing a direct phosphorus-carbon bond. This hypothesis forms the basis of my investigations, which primarily aimed to detail biogenic phosphite production in a phosphonate synthesizing organism using an array of optimized analytical techniques for phosphite detection.I developed an enzymatic, fluorometric assay for phosphite sensing. The method is reliant on the activity of a NAD+-dependent phosphite dehydrogenase, which through a series of electron transfer reactions, reduces resazurin to the highly fluorescent resorufin. Through the use of a thermostable variant of phosphite dehydrogenase, novel sample preparation methods, and phosphite standard additions, stable fluorescence readout can be read in 20 minutes with a 3 M limit of detection. The assay’s limit of detection and phosphite recovery were assessed in a wide array of biologically- and environmentally-relevant matrices to determine the sensor’s robustness. The sensor, along with 1H-coupled and 1H-decoupled 31P-NMR, were employed to observe phosphite production in Streptomyces viridochromogenes, a gram-positive soil bacterium. Through phosphonate feeding experiments in cell culture and soluble cell lysate, as well as the recombinant expression and purification of CTP-phosphonoformate nucleotidyltransferase (PhpF), phosphite was determined to be the decomposition product of activated phosphonate phosphonoformate-CMP. This work challenged the preexisting assumption that phosphite was a decomposition product of phosphonoformate at biologically-relevant temperatures and pHs. Finally, phosphite was investigated as a mobile, selective P-source for toluene-degrading inoculant Pseudomonas veronii in a synthetic soil community (SynCom) as a means of enhancing bioremediation efficiency. A phosphite-oxidizing (ptxD+) mutant of Pseudomonas veronii was constructed that can use phosphite as a sole P source. Soil microcosms with all iterations of the presence or absence of inoculant, SynCom, toluene, and phosphite were propagated, and were monitored for community composition with 16S rRNA gene amplicon sequencing and toluene degradation rates using GC-MS. Phosphite was determined to enhance inoculant abundance most prominently in toluene-free soil microcosm, likely due to the growth substrate being carbon limited.
These investigations provide new insights into the role of phosphite in the biogeochemical P cycle, elucidating both a biological production mechanism of phosphite as well as its bioavailability in soil microbial communities.