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Species-Level Variability in Extracellular Production Rates of Reactive Oxygen Species by Diatoms
Robin J Schneider1, Kelly L Roe2, Colleen M Hansel3
1Department of Chemistry, St. John's University New York, NY, USA.
Frontiers in Chemistry
|April 12, 2016
Summary
Marine diatoms produce reactive oxygen species (ROS) like hydrogen peroxide (H2O2) and superoxide (O2-) through diverse pathways, influenced by light. These ROS play a role in marine carbon and metal cycling.
Area of Science:
- Marine biology
- Biogeochemistry
- Environmental science
Background:
- Reactive oxygen species (ROS), including hydrogen peroxide (H2O2) and superoxide (O2-), are biologically produced and degraded in marine systems.
- ROS are known to influence the cycling of critical elements like trace metals and carbon in oceans.
Purpose of the Study:
- To quantify extracellular production rates of H2O2 and O2- by five marine diatom species.
- To investigate the influence of light on ROS production in diatoms.
- To examine the capacity of diatoms to degrade H2O2 and O2-.
Main Methods:
- Extracellular ROS production was measured using chemiluminescence probes on filtered diatom cultures.
- ROS production was assessed in both the presence and absence of light.
- Degradation of H2O2 and O2- was evaluated by measuring recovery rates in live and killed diatom cultures.
Main Results:
- Significant variation in O2- and H2O2 production rates (up to 7.3 × 10(-16) and 3.4 × 10(-16) mol cell(-1) h(-1), respectively) was observed among diatom species.
- Light enhanced O2- production in some species, suggesting a passive photochemical pathway on cell surfaces.
- Diatom species exhibited distinct ROS production and decay mechanisms, with significant differences between live and killed cells, indicating active cellular processes.
Conclusions:
- Diatom species display diverse and species-specific extracellular ROS production and decay pathways.
- Light conditions significantly impact ROS production, with evidence of passive photochemical ROS generation.
- Active cellular processes are crucial for ROS decay, but passive mechanisms also contribute, particularly for O2-.
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