Microbial Nitrogen Cycling
The oxidation of NH3 to NO2- and ultimately NO3- by chemoautotrophic ammonia- and nitrite-oxidizing microorganisms is a critical branch of the nitrogen cycle in soil, sedimentary, marine, freshwater and estuarine environments, where this process provides the key link between the mineralization of organic nitrogen and the subsequent loss of fixed nitrogen via denitrification and anammox. Much of our research is focused on exploring the diversity and structure of ammonia-oxidizing microbial communities, based on amoA genes encoding the alpha-subunit of the key nitrification enzyme, ammonia monooxygenase (AMO). Our work has revealed the widespread occurrence of the previously unrecognized group of ammonia-oxidizing archaea (AOA) in marine water columns and sediments. We are currently using molecular and biogeochemical approaches to explore the diversity, abundance, and activity of AOA and AOB in a number of ecosystems, including Monterey Bay, San Francisco Bay, Elkhorn Slough, and Riverton, WY, among others. Finally, we are using cultivation as well as metagenomic and metatranscriptomic approaches (see CSP Projects through the DOE Joint Genome Institute) to gain novel insights into AOA within both aquatic and terrestrial environments.
The dissimilatory reduction of nitrate and nitrite to gaseous products (NO, N2O, N2) under suboxic conditions, denitrification, is a major loss term for fixed nitrogen from ecosystems. This process removes up to 50% of external N inputs from estuarine and coastal sediments, and also leads to the production of potent greenhouse gases, NO and N2O. Despite the global importance of denitrifiers, the "key players" in most environments are simply not known. Functional genes encoding key metalloenzymes in the denitrification pathway have proven to be useful molecular markers for studying denitrifying communities. Our work has focused on characterizing the distribution, diversity, abundance, and activity of denitrifiers across physical/chemical gradients in many of the environments where we are also studying ammonia-oxidizers (e.g., Elkhorn Slough, San Francisco Bay, Riverton, etc.). By simultaneously examining these two key branches of the microbial N cycle, we hope to gain new insights into the relationships between functional diversity, environmental gradients, and biogeochemical function.