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Bess
B. Ward Department Chair Professor of Geosciences (Biological Oceanograpy) Department of
Geosciences |
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Research (Project Summaries) Marine and global nitrogen cycle, molecular and immunological probes for marine bacteria and bacterial processes (especially nitrification and denitrification), microbal ecology, xenobiotic transformations by bacterial communities. Microbes control many of the important biogeochemical processes that occur in the oceans as well as on land. They contribute to the trace gas cycles that influence climate; they utilize and produce nutrients that are involved in eutrophication; and they are even capable of cleansing the environment by degrading a vast variety of chemical compounds, both naturally occurring and anthropogenically produced. My research focuses on the nitrogen cycle and the microorganisms involved in transformations of inorganic and organic nitrogen in the ocean and in sediment environments. This research makes use of technical approaches that range from molecular biological techniques to stable isotope biogeochemistry. The two main bacterial groups we study are the nitrifiers, autotrophs which oxidize ammonium to nitrite and nitrate, and the denitifiers, heterotrophs which can respire nitrate in the absence of oxygen. The linked activities of these two groups can be crucial in determining the chemical form and supply of nitrogen to planktonic communities and in determining the net nitrogen budget of ecosystems. We have used molecular methods for identification and analysis of bacteria in natural systems to study the distribution and diversity of nitrifying and denitrifying bacteria in marine environments. One ongoing project utilizes PCR and gene probe analysis to detect nitrifying bacteria in sediments and seawater, and to characterize the bacterial community across spatial and seasonal gradients. Our objective is to understand how the rates of nitrification may depend on the species composition of the nitrifying bacterial assemblage and its variation over time, space and environmental conditions. Another project uses genetic techniques to identify the kinds of microorganisms that are responsible for nitrate and ammonium assimilation in seawater. The field work for these two projects is carried out in Monterey Bay, California, and in estuarine environments on the California Coast. It has recently been recognized that trace metals such as iron and zinc are essential for plant and algal nutrition and that the availability of these metals may limit primary production. By contrast, very little is known about the trace metal requirements or toxicities for bacteria, which is the motivation behind another current project. Our study site is a permanently ice-covered lake in Antarctica which has two separate lobes; denitrification occurs in one lobe but not the other. We hypothesize that trace metal limitation or toxicity might explain this phenomenon. Trace metals are required for most of the redox chemistry of bacterial processes, and we are approaching this general area of research initially through study of the denitrifying enzymes. This research program (Project Summaries) is supported by field work on research cruises and expeditions as well as by laboratory based research, and is supported by a variety of federal and regional funding agencies.
Recent Extramural Projects
2003-2006 National Science Foundation: What limits denitrification and bacterial growth in Lake Bonney, Taylor Valley, Antarctica?Research Cruises and Expeditions (recent) 2000-present Several cruises per year in Chesapeake Bay/Atlantic Ocean |
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Updated 07/10/06 |
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