2017
DOI: 10.1021/acs.est.7b03713
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Photochemical Alteration of Dissolved Organic Sulfur from Sulfidic Porewater

Abstract: Sulfidic sediments are a source of dissolved organic sulfur (DOS) to the ocean but the fate of sedimentary DOS in the oxic, sunlit water column is unknown. We hypothesized that photodegradation after discharge from the dark sedimentary environment results in DOS molecular transformation and decomposition. To test this hypothesis, sulfidic porewater from a saltmarsh was exposed to potential abiotic transformations of dissolved organic matter (DOM) in the water column. We quantitatively investigated DOM transfor… Show more

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Cited by 47 publications
(68 citation statements)
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References 73 publications
(210 reference statements)
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“…It also highlights the fact that sulfurization reactions in SBB pore waters are not limited to CHO formulas and also involve a wide variety of compounds including nitrogen-containing DOM compounds. This latter point agrees with laboratory sulfurization experiments which show that abiotic sulfur incorporation reactions are non-selective and occur with a wide variety of DOM compounds including DON compounds (Pohlabeln et al, 2017;Gomez-Saez et al, 2017).…”
Section: Reactant Dom Formulassupporting
confidence: 89%
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“…It also highlights the fact that sulfurization reactions in SBB pore waters are not limited to CHO formulas and also involve a wide variety of compounds including nitrogen-containing DOM compounds. This latter point agrees with laboratory sulfurization experiments which show that abiotic sulfur incorporation reactions are non-selective and occur with a wide variety of DOM compounds including DON compounds (Pohlabeln et al, 2017;Gomez-Saez et al, 2017).…”
Section: Reactant Dom Formulassupporting
confidence: 89%
“…Our results and those of others (Gomez-Saez et al, 2016;Poulin et al, 2017;Gomez-Saez et al, 2017) reveal high sulfurization reactivity of many of the CHO and DON formulas that fall in the CRAM region on a van Krevelen diagram, and this group of formulas could be responsible for the formation of a major fraction of organosulfur compounds in anoxic and sulfidic sediments. If these DOS products are precursors of sulfur-containing protokerogen, they may play a key role in enhancing organic preservation in sulfidic sediments.…”
Section: Discussionsupporting
confidence: 77%
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“…All CHNO components had a mass < 500 Da and were related to small molecules, with oxygen-poor and relatively aliphatic character ( Figure S4). The photo transformation of S-containing components was investigated by [80] and [84]. In contrast to these two studies, the abundance of CHOS was much smaller in our sample ( Figures S5 and S6).…”
Section: Average Photo-chemical Dom Quality Changementioning
confidence: 58%
“…We speculate that the higher mineralized fractions in these waters may be due to specific enriched DOM that is not found in typical lacustrine environments, 22 as confirmed by the low 262 DOC/DOS ratios of the porewaters compared to the other samples (Table S2). Water circulation 263 within the wetland brings the S-enriched DOS from the sediments to the surface, 22,23 where 264 oxidative transformations can occur 11,23 . Thus, we reason that the Prairie Pothole surface waters are more reactive than common surface waters due to a higher content of organic sulfur, but less reactive than the corresponding porewaters due to a lower fraction of reduced sulfur species.…”
mentioning
confidence: 99%