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GCAGS Transactions

Abstract


Gulf Coast Association of Geological Societies Transactions
Vol. 38 (1988), Pages 579-579

Abstract: Environmental Sedimentology of the Pontchartrain-Maurepas Estuarine Complex

George C. Flowers (1), Andrew W. Durfee (1), Wayne C. Isphording (2)

ABSTRACT

The Pontchartrain Basin is the site of one of the largest estuarine complexes in the southeastern United States. It is well known that the same geographic factors that make southeastern Louisiana an important metropolitan and industrial region have also led to disruption of the estuarine environment. Pollution, development, flood abatement, and dredging have all impacted the estuary. Besides affecting the biota and water quality, the impact of these environmental pressures is reflected in the bottom sediments of the lakes.

As part of an ongoing study of northern Gulf of Mexico estuaries, over 120 bottom sediment samples were collected from the Pontchartrain-Maurepas estuarine complex in late 1987. Comparison of sediment maps generated in the present study with studies based on samples collected in 1931, 1972, 1973, and 1978 indicates that the distribution of sediment types has not changed greatly over the past 56 years. A notable exception is the south shore in the vicinity of outfall canals and the Inner Harbor Navigation Canal where sandy sediment is accumulating. Other "textural islands" of sediment with elevated sand content, discovered by the 1931 sampling of Lake Pontchartrain, persist to the present day.

Lake Maurepas sediments have a significantly lower level of carbonate than Lake Pontchartrain sediments. In Lake Pontchartrain the carbonate content increases from east to west with the highest values occurring along the south shore. The generally elevated carbonate content of the sediments probably reflects the impact of shell dredging on the estuarine complex. The anomalously high carbonate content of a few samples along the south shore, however, is probably due to the concentration of shell by wave action rather than shell dredging which is prohibited in the near shore areas of the lake.

Of the two lakes, Lake Pontchartrain has been impacted most by heavy metals carried in effluent, particularly along the south shore due to the numerous outfall canals. Comparison of metal levels in the lake with values determined for Mississippi Sound indicates that Pb and Cr are elevated in lake Pontchartrain. As frequently observed in estuarine sediments, the heavy metal content of affected sediments increases with increasing clay content. Therefore, sediment samples taken at the mouths of outfall canals can produce erroneous estimates of the impact of effluent due to the elevated sand content. The sandy sediments in the vicinity of outfall canals are the result of winnowing during periods of high discharge storm drainage.

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ACKNOWLEDGMENTS AND ASSOCIATED FOOTNOTES

(1) Department of Geology, Tulane University, New Orleans, LA 70118

(2) Department of Geology and Geography, University of South Alabama, Mobile, AL 36688

Copyright © 1999 by The Gulf Coast Association of Geological Societies