Biogeochemistry of Dissolved Organic Matter


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Project Overview

Dissolved organic matter (DOM) is a significant chemical component in aquatic systems because it acts as an important carbon source for microorganisms, absorbs harmful radiation in sunlight, is able to complex metals, and can participate in important biogeochemical redox reactions. We are studying the biogeochemical cycling of DOM in a small coastal Antarctic pond, Pony Lake, located on Cape Royds, Ross Island. Because there are no higher plants present at this site all of the DOM in this lake is microbially derived from photoautotrophic, heterotrophic, and mixotrophic organisms. Thus, Pony Lake is an ideal site to study the effect of photolysis, redox changes, and microbial processes on the composition and character of the DOM pool. Finally, Pony Lake’s abundant levels of DOM (50-100 mg/L as C) and proximity to the laboratory resources at McMurdo Station, makes it an ideal site to collect an International Humic Substances Society (IHSS) fulvic acid standard. Unlike other IHSS standards, this standard will not contain DOM components derived from higher land plants.

What's  New

  •  Soon to be reported
Key Milestones
  •  Soon to be reported.
     

Project Support

This material is based upon work supported by the National Science Foundation under Grant No. 0338121.  Any opinions, findings and conclusions or recommendations expressed in this material are those of the author(s) and do not necessarily reflect the views of the National Science Foundation (NSF).

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 Copyright 2004.
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Last updated: 05/28/05.