The concentration of dissolved oxygen (O2) in the ocean determines the structure and function of marine ecosystems. Loss of dissolved oxygen in the ocean favors chemolithoautotrophic metabolism that causes a decrease in nitrogen and production of the greenhouse gases nitrous oxide (N2O) and methane (CH4). Protists are important members of aquatic microbial communities. Through grazing on prokaryotic and other eukaryotic prey, they modify or remineralize organic matter and regenerate nutrients. They also can affect the quantity, activity and physiological state of their prey. Thus, through direct and indirect effects, protists help determine the metabolic potential of microbial communities. Bacterial grazing in marine environments is principally performed by flagellated protists and ciliates. We are interested in looking at the diversity and role of protists in low oxygen to sulfidic marine water columns. Our current study sites include the Eastern Mediterranean deep hypersaline anoxic basins, the Cariaco Basin, Venezuela, and Saanich Inlet.
Saanich Inlet is a seasonally anoxic fjord and an example of a marine oxygen minimum zone (OMZ). OMZs are becoming areas of growing interest for several reasons. First, studies have indicated that climate change induced formation and intensification of OMZs is increasing worldwide. Second, OMZs influence carbon sequestration and cycling as well as the cycling of nitrogen in the world’s oceans. OMZs support enigmatic communities of microorganisms that regulate global cycles of nutrients and gases. Together with our collaborators we are examining the response in microbial eukaryotes (protists) to changing oxygen concentrations using 18S small subunit ribosomal RNA (SSU rRNA) and metatranscriptomic, as well as microscopy-based approaches. OMZs and permanently anoxic water columns select for unique assemblages of protists, including many novel lineages.
MultimediaMovie of representative cell of novel ciliate class CARH
Credit: William Orsi