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Sediments of Lake ErieThis project is no longer current. Please see the Research Programs page for a list of current research projects. Collaborators Executive SummarySediment-water exchange is important in the cycling and fate of many constituents in the Great Lakes. Since Lake Erie is the most shallow of the Great Lakes, understanding and quantifying the lakes coupling with inventories of chemicals in the exchangeable sediments will be critical in any attempt to build ecosystem simulation/forecasting models. Each of the components of this project contributes to that end. Program PlansThere are several sub-projects under this title:
Program AccomplishmentsPaleo-proxies: Cores from the same location collected in 1983 and 1991 have been analyzed for geochronology, stable isotopes, carbon, and nutrient concentrations. Analyses of these same constituents plus selected lipid biomarkers are nearly completed on a new core. The core collected in September 2003 provides data on the effects of the relatively warm temperatures of the 1990s. Data are being processed and will result in a manuscript. Eastern Basin Reference Site Cores (EBRS-03): Most analyses are completed. A manuscript is in draft form. Literature review: Literature has been accumulated but the search has not yet been exhaustive. We recovered 3 independent data sets of radionuclide analyses of accumulation rates/inventories. These, (Edgington, 1976 Cs rates + inventories, Robbins 1982 Cs inventories, Edgington and Klump 1991 Cs and 210 Pb rates) combined with the Kemp et al sediment accumulation rates (below) based on pollen and Canadian surveillance data, will allow us to synthesize the data accumulation rates in the lake for modeling and recent accumulations of carbon and nutrients.
Net Mass Accumulation Rate Lake Erie Trapping: Canadian Centre for Inland Waters (CCIW web site) trap samples (May - Oct, 2004) are being analyzed in conjunction with GLERL trap samples from Sep 2004 - Oct 2005 at the center of the central basin and the deep hole in the eastern basin. Mass, nutrient and carbon fluxes are being measured. Two posters were presented at the 2006 Lake Erie Millennium network conference (see below). These data will be incorporated into the sediment accumulation manuscript.
Mass fluxes at the Lake Erie central and eastern basins. Lake Erie workshop: As a major step in developing this Lake Erie program, GLERL hosted a large (over 50 attendees), international workshop on March 4-5, 2004 to identify and discuss three important Lake Erie issues that GLERL scientists thought were within the existing capabilities of the laboratory: anoxia and hypoxia, harmful algal blooms (HABs), and coupling physics with fish forecasts. This workshop also provided an opportunity:
Several areas of potential and immediate collaboration were identified and mechanisms to implement them were initiated. A final report is available: http://www.glerl.noaa.gov/ifyle/workshops/workshop200403.html Posters Eadie, Brian J., Nathan Hawley, Murray Charlton, Ram Yerubundi, Margaret
Lansing and Thomas Johengen. 2006."Rates of Delivery of Organic Carbon
and Nutrients to the Hypoxic Region of Lake Erie" Lake Erie Millennium
Network Conference, Windsor, ON, 28 February - 2 March 2006. Klump, J.V., K. Weckerly, D. Edgington, P. Anderson, D. Szmania, J. Waples,
and B.j. Eadie. 2006. "Historical Sedimentation Rate Determinations in
Lake Erie." Lake Erie Millennium Network Conference, Windsor, ON, 28 February
- 2 March 2006. PresentationsMeyers, P.A., C.K. Knowlton, B.J. Eadie, and J.A. Robbins. Interpreting recent paleolimnology from Lake Erie cores. AGU, San Francisco, Dec 2003. Knowlton, C., Meyers, P.A., B.J. Eadie, and J.A. Robbins. Oxygen, Carbon, and Nitrogen Isotopic Evidence of Environmental Changes in Eastern Lake Erie Over the Past Century. AGU, San Francisco, Dec 2003 ReferencesKemp, A.L.W., A. MacInnis, and N.S. Harper. 1977. Sedimentation rates for a revised sediment budget for Lake Erie. J. Great Lakes Res. 3(3-4):221-233. |
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