Reactive oxygen species affect the potential for mineralization processes in permeable intertidal flats.

Intertidal permeable sediments are crucial sites of organic matter remineralization. These sediments likely have a large capacity to produce reactive oxygen species (ROS) because of shifting oxic-anoxic interfaces and intense iron-sulfur cycling. Here, we show that high concentrations of the ROS hydrogen peroxide are present in intertidal sediments using microsensors, and chemiluminescent analysis on extracted porewater. We furthermore investigate the effect of ROS on potential rates of microbial degradation processes in intertidal surface sediments after transient oxygenation, using slurries that transitioned from oxic to anoxic conditions. Enzymatic removal of ROS strongly increases rates of aerobic respiration, sulfate reduction and hydrogen accumulation. We conclude that ROS are formed in sediments, and subsequently moderate microbial mineralization process rates. Although sulfate reduction is completely inhibited in the oxic period, it resumes immediately upon anoxia. This study demonstrates the strong effects of ROS and transient oxygenation on the biogeochemistry of intertidal sediments.

Microbial community composition of sediments influenced by intensive mariculture activity.

Marine aquaculture is a major industry that supports the economy in many countries, including the Philippines. However, excess feeds and fish waste generated by mariculture activities contribute an immense nutrient load to the environment that can affect the underlying sediment. To better understand these impacts, we compared the physicochemical characteristics and microbial community composition of sediments taken at a fish cage and an off cage site in Bolinao, Philippines. Sediments and pore water at the fish cage site showed evidence of greater organic enrichment relative to the off cage site. Under these conditions, we found lower relative abundance of dissimilatory sulfate reductase and nitrite reductase genes, suggesting shifts in prevalent nutrient cycling processes. This is further supported by 16S rRNA gene sequencing that revealed differences in the community composition between sites. Fish cage sediments favored the growth of taxa that thrive in anaerobic, organic carbon-enriched environments, such as members of class Anaerolineae, which can potentially serve as bioindicators of eutrophication in sediments. This study demonstrates that intensive mariculture activity can cause eutrophic sediment conditions that influence microbial community structure and function.