A potential photo-protective, antioxidant function for DMSO in marine phytoplankton

The marine compound dimethyl sulfoxide (DMSO) is ubiquitous in the world's surface ocean, constituting one of the largest sources of reduced organic sulfur in seawater. DMSO cycling has been linked to the formation of the climate-active gas dimethyl sulfide (DMS) through a reductive pathway, but the underlying physiological role of DMSO reduction, and the environmental controls on this pathway, remain unresolved. Here we present evidence that DMSO reduction to DMS serves an antioxidant role in phytoplankton through a secondary electron-scavenging pathway that can dissipate excess light-harvested energy, and potentially mitigate the formation of reactive oxygen species (ROS). Results from isotopic tracer experiments demonstrate significant increases in DMSO reduction rates in low-light acclimated natural phytoplankton assemblages exposed to high irradiance. Increased DMSO reduction rates were negatively correlated with non-photochemical quenching, while treatment with the photosynthetic electron transport inhibitor DCMU significantly decreased DMSO reduction, indicating a link to photosynthetically-derived electrons. Our results show that photic stress drives enhanced DMSO reduction in marine phytoplankton, linking DMS production to irradiance and vertical mixing through an electron scavenging mechanism that could serve an antioxidant role.

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Publication Details

Journal
PLoS ONE
Published
2025-02-06
DOI
https://doi.org/10.1371/journal.pone.0317951
Citations
2
Primary Topic
Atmospheric chemistry and aerosols
Type
article
Field-Weighted Citation Impact
2.60

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article

A potential photo-protective, antioxidant function for DMSO in marine phytoplankton

Philippe D. Tortell, Brandon J. McNabb
2 citations
PLoS ONE
Atmospheric chemistry and aerosols
2.60
article

A potential photo-protective, antioxidant function for DMSO in marine phytoplankton

Philippe D. Tortell, Brandon J. McNabb
article en
2 citations

Abstract

The marine compound dimethyl sulfoxide (DMSO) is ubiquitous in the world's surface ocean, constituting one of the largest sources of reduced organic sulfur in seawater. DMSO cycling has been linked to the formation of the climate-active gas dimethyl sulfide (DMS) through a reductive pathway, but the underlying physiological role of DMSO reduction, and the environmental controls on this pathway, remain unresolved. Here we present evidence that DMSO reduction to DMS serves an antioxidant role in phytoplankton through a secondary electron-scavenging pathway that can dissipate excess light-harvested energy, and potentially mitigate the formation of reactive oxygen species (ROS). Results from isotopic tracer experiments demonstrate significant increases in DMSO reduction rates in low-light acclimated natural phytoplankton assemblages exposed to high irradiance. Increased DMSO reduction rates were negatively correlated with non-photochemical quenching, while treatment with the photosynthetic electron transport inhibitor DCMU significantly decreased DMSO reduction, indicating a link to photosynthetically-derived electrons. Our results show that photic stress drives enhanced DMSO reduction in marine phytoplankton, linking DMS production to irradiance and vertical mixing through an electron scavenging mechanism that could serve an antioxidant role.

PLoS ONEVol. 20(2)
University of British Columbia (CA)
Natural Sciences and Engineering Research Council of Canada
Life below water
Openalex Percentile: Top 14%
Atmospheric chemistry and aerosols
2.60
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