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Ann Pearson

Publications and source records attributed to Ann Pearson.

2 recordsLinked to original sources

Nitrifying microorganisms linked to biotransformation of perfluoroalkyl sulfonamido precursors from legacy aqueous film forming foams

Drinking water supplies across the United States have been contaminated by firefighting and fire-training activities that use aqueous film-forming foams (AFFF) containing per- and polyfluoroalkyl substances (PFAS). Much of the AFFF is manufactured using electrochemical fluorination by 3M. Precursors with six perfluorinated carbons (C6) and non-fluorinated amine substituents make up approximately one-third of the PFAS in 3M AFFF. C6 precursors can be transformed through nitrification (microbial oxidation) of amine moieties into perfluorohexane sulfonate (PFHxS), a compound of regulatory concern. Here, we report biotransformation of the most abundant C6 sulfonamido precursors in 3M AFFF with available commercial standards (FHxSA, PFHxSAm, and PFHxSAmS) in microcosms representative of the groundwater/surface water boundary. Results show rapid (<1 day) biosorption to living cells by precursors but slow biotransformation into PFHxS (1–100 pM day –1 ). The transformation pathway includes one or two nitrification steps and is supported by the detection of key intermediates using high-resolution mass spectrometry. Increasing nitrate concentrations and total abundance of nitrifying taxa occur in parallel with precursor biotransformation. Together, these data provide multiple lines of evidence supporting microbially limited biotransformation of C6 sulfonamido precursors involving ammonia-oxidizing archaea ( Nitrososphaeria ) and nitrite-oxidizing bacteria ( Nitrospina ). Further elucidation of interrelationships between precursor biotransformation and nitrogen cycling in ecosystems would help inform site remediation efforts.

Environmental Science and Technology

Paleoenvironmental implications of taxonomic variation among δ 15 N values of chloropigments

Natural variations in the ratios of nitrogen isotopes in biomass reflect variations in nutrient sources utilized for growth. In order to use &delta; 15 N values of chloropigments of photosynthetic organisms to determine the corresponding &delta; 15 N values of biomass &ndash; and by extension, surface waters &ndash; the isotopic offset between chlorophyll and biomass must be constrained. Here we examine this offset in various geologically-relevant taxa, grown using nutrient sources that may approximate ocean conditions at different times in Earth&rsquo;s history. Phytoplankton in this study include cyanobacteria (diazotrophic and non-diazotrophic), eukaryotic algae (red and green), and anoxygenic photosynthetic bacteria (Proteobacteria), as well as environmental samples from sulfidic lake water. Cultures were grown using N 2 , NO 3 &minus; , and NH 4 + as nitrogen sources, and were examined under different light regimes and growth conditions. We find surprisingly high variability in the isotopic difference (&delta; 15 N biomass &minus; &delta; 15 N chloropigment ) for prokaryotes, with average values for species ranging from &minus;12.2&permil; to +11.7&permil;. We define this difference as &epsilon; por , a term that encompasses diagenetic porphyrins and chlorins, as well as chlorophyll. Negative values of &epsilon; por reflect chloropigments that are 15 N-enriched relative to biomass. Notably, this enrichment appears to occur only in cyanobacteria. The average value of &epsilon; por for freshwater cyanobacterial species is &minus;9.8 &plusmn; 1.8&permil;, while for marine cyanobacteria it is &minus;0.9 &plusmn; 1.3&permil;. These isotopic effects group environmentally but not phylogenetically, e.g., &epsilon; por values for freshwater Chroococcales resemble those of freshwater Nostocales but differ from those of marine Chroococcales. Our measured values of &epsilon; por for eukaryotic algae (range = 4.7&ndash;8.7&permil;) are similar to previous reports for pure cultures. For all taxa studied, values of &epsilon; por do not depend on the type of nitrogen substrate used for growth. The observed environmental control of &epsilon; por suggests that values of &epsilon; por could be useful for determining the fractional burial of eukaryotic vs. cyanobacterial organic matter in the sedimentary record.

Geochimica et Cosmochimica Acta