2003-2004 USAP Field Season

Biology & Medicine

Dr. Polly Penhale
Program Manager

B-266-N

NSF/OPP 02-30499
Station: RV/IB Nathaniel B. Palmer
RPSC POC: Don Michaelson
Research Site(s): Ross Sea
Dates in Antarctica: Mid October to late November

Impact of solar radiation and nutrients on biogeochemical cycling of DMSP and DMS in the Ross Sea
Dr. David J. Kieber
State University of New York Syracuse
Chemistry Department
djkieber@syr.edu
http://www.esf.edu/chemistry/kieber/kieber.htm
 
Photo not available.
Deploying Team Members: John Bisgrove . David J. Kieber . Deirdre A. Toole . Emily M. White
Research Objectives: Areas of the Southern Ocean have spectacular blooms of phytoplankton during the austral spring and early summer. One of the dominant species, the haptophyte Phaeocystis antarctica, is a prolific producer of the organic sulfur compound dimethylsulfoniopropionate (DMSP), and Phaeocystis blooms are associated with some of the world's highest concentrations of DMSP and its volatile degradation product, dimethylsulfide (DMS). Sulfur, in the form of DMS, is transferred from the oceans to the atmosphere and can affect the chemistry of precipitation and influence cloud properties and, possibly, climate. DMSP and DMS are also quantitatively significant components of the carbon, sulfur, and energy flows in many marine food webs, although very little information is available on these processes in high-latitude systems.

We will study how solar radiation and iron cycling affect DMSP and DMS production by phytoplankton and the subsequent use of these labile forms of organic matter by the microbial food web. Four interrelated hypotheses will be tested in field-based experiments and in situ observations:

+ That solar radiation, including enhanced ultraviolet-B due to seasonal ozone depletion, plays an important role in determining the net ecosystem production of DMS in the Ross Sea;

+ That development of shallow mixed layers promotes the accumulation of DMS in surface waters, because of enhanced exposure of plankton communities to high doses of solar radiation;

+ That DMSP production and turnover represent a significant part of the carbon and sulfur flux through polar food webs; and

+ That bloom development and resulting nutrient depletion (e.g., iron) will result in high production of DMSP and high DMS concentrations and atmospheric fluxes.

Results from this study will greatly improve understanding of the underlying mechanisms controlling DMSP and DMS concentrations in polar waters, thereby improving our ability to predict DMS fluxes to the atmosphere from this important climatic region.

We actively engage high school, undergraduate, and graduate students in our research and are involved in formal programs that target underrepresented groups. The information gained from this research will also be used in teaching undergraduate and graduate courses and will enrich students’ experience.