GSA Poster 2013 Denver - Johnny Wimpee
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Transcript of GSA Poster 2013 Denver - Johnny Wimpee
Using Thecamoebian Populations to Evaluate Historical Water Quality in Todds Lake in Murfreesboro, Tennessee
Jesse C. Watts and Melissa Lobegeier Department of Geosciences, Middle Tennessee State University, Murfreesboro, TN, 37132
Abstract Study Area
Acknowledgments
Materials and methods
Figure 2: Map of sediment collection sites in Todds Lake.Rutherford Blvd. is the road that cuts across the lake(Map by: Google Earth)
Wetlands Estonoa
Oxbow Lake
Figure 1: View to the northwest of Todds Lake acrossRutherford Blvd.
Figure 4: A view of lily pads to the southeast toward the head waters of the lake
Wetlands Estonoa
Oxbow Lake
We wish to thank Kathryn Tackett, Kyle Wiseman, Amy Gilley,Amanda Brown, Emily Silveira, Johnny Wimpee and JoyceMiller.
Literature Cited
Results
Ogden, C.G., 1988, Fine structure of the shell wall in the soiltestate amoeba Cyclopyxis kahli (Rhizopoda), Journal ofProtozoology, 35, p. 537‐540.
Water quality is and will continue to be an importantenvironmental concern. Todds Lake is a smallfreshwater, artificial reservoir in Murfreesboro,Tennessee that was created in the 1930s by damminga wetland. Murfreesboro has experienced tremendousgrowth and rapid urbanization in the past decadewith the population of the city increasing 50.5% from2000 to 2010. Todds Lake is located in the StonesRiver Watershed and is fed by Black Fox Spring, whichtravels through several subdivisions receiving runofffrom lawns and driveways before ending in ToddsLake. The lake is also surrounded by urbandevelopment such as additional subdivisions, a stripmall and a gas station and may be receiving runofffrom those areas that could be negatively affecting thewater quality within the lake. Thecamoebians arebenthic testate amoebae that have been used inmultiple studies in North America and Europe asindicators of pollution and water quality in lacustrineenvironments. Analysis of thecamoebian populationsfrom sediment samples collected in Todds Lake inrecent years indicates that the lake is a stressedeutrophic environment with low diversityassemblages and abundant Centropyxis aculeataobserved in the samples. The shells of thecamoebianspreserve easily so these organisms can yield historicaldata on water quality. The fossilization potential ofthecamoebians gives them an advantage over otherfreshwater micro‐ and macroinvertebrates. This studywill compare populations of thecamoebians fromsediment samples in Todds Lake with those found insamples taken from a sediment core to determine ifthere have been changes in the ecological condition ofthe lake and wetland over the last century.
Surface sediment samples and short cores were takenby hand at various sites and the locations wererecorded with a GPS device. Each sample is sievedusing 45 and 500 µm sieves. This process removes thelarge organic matter from the sample and the mud isseparated from the thecamoebians. Once washed thesediment is preserved in isopropyl alcohol, andrefrigerated. Using a microscope and a fine tippedbrush, the thecamoebians are picked out of eachsample and then placed onto a numbered slide.
Two cores were collected. One was collected using asmall‐diameter coring device and the other wascollected using a universal coring device. Age datingusing Pb‐210 isotopic dating will be completed in thenext few months. The cores were sectioned in 1 cmslices and then washed in the same way as thesediment samples.
Figure 5: Histograms of the relative abundance of thecamoebians speciesin surface samples
Figure 3: Electron scanning microscope image of (1) Centropyxisaculeata “aculeata”, (2) Difflugia oblonga “tenuis”, (3) Difflugia corona, (4) Cyclopyxis kahli, (5) Difflugia oblonga “spinosa”, (6) Difflugia corona
Todds Lake appears to be more negatively impactedcloser to the busy Rutherford Boulevard. SampleKAT012, which is located closest to the road (Figs 1and 2), shows an increase in the relative abundance ofCentropyxis aculeata “aculeata” and Centropyxisaculeata “discoides” (Fig. 5). Centropyxids areenvironmental generalists that can tolerateintermediate to poor water quality environments.KAT001 and KAT003, located furthest fromRutherford Blvd., have absent to low relativeabundances of centropyxids, suggesting a relativeincrease in water quality further away from thedrainage coming from the road.
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Figure 6: Histograms of the relative abundance of thecamoebians species in coresamples
We found a high relative abundance of Cyclopyxis kahli inthe Todds Lake core samples. Cyclopxis kahli is known toinhabit soils as well as fresh water environments (Ogden,1988). The abundance of this species may show that soilerosion could have potentially introduced them into thelake.
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Figure 7: Calculated values for the Shannon Diversity Index (SDI), Pielou’sequitability index (j) values and Margalef’s richness index (d) values for the surface samples and core samples
The Shannon Diversity Indices for both the surface samplesand core samples are between 2.13 and 0.92. Surfacesamples further from Rutherford Blvd., KAT001 andKAT003, have higher SDI values than the sample closest tothe road, KAT012. This indicates that environmentalimpacts are greater closer to the road.
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