|2011 GSA Annual Meeting in Minneapolis (9–12 October 2011)|
|Paper No. 194-4|
|Presentation Time: 2:30 PM-2:45 PM|
TWO HUNDRED YEARS OF COASTAL CHANGE IN THE MOBILE BAY ESTUARY, NORTHERN GULF OF MEXICO
OSTERMAN, Lisa E., St. Petersburg Coastal and Marine Science Center, U.S. Geological Survey, 600 Fourth St. South FL, St. Petersburg, FL 33701, firstname.lastname@example.org and SMITH, Christopher G., St. Petersburg Coastal and Marine Science Center, U.S. Geological Survey, 600 Fourth Street South, St. Petersburg, FL 33701|
In an effort to document how the environmental and sedimentological regimes have evolved in the face of natural and anthropogenic pressures, foraminifers and sediment geochemistry of Mobile Bay, Alabama (USA) were analyzed. Twelve surface-sediment grab samples collected throughout the bay for three seasons show seasonal and spatial variability in the foraminifers; agglutinated species dominate the modern microfauna throughout most of the bay. Living foraminiferal densities are greatest in the southern bay and the more industrial western bay. Similarly, organic matter increases in a southerly or seaward direction, indicating a portion of riverine and/or deltaic organic matter bypasses the pro-delta region and deposits in the southern portion of the bay. Higher organic matter and salinities favor the greater living benthic foraminiferal densities observed in the southern portion of the bay. Living foraminiferal densities and associated assemblage composition indicate two biofacies (upper and lower bay), which are used to help reconstruct longer-term environmental change in Mobile Bay.
Study of seven box cores, with 210Pb-derived chronologies, show that significant environmental changes occurred in the middle of the last century. Lower-density calcareous foraminiferal assemblages at depth are replaced in the near-surface sediment by higher-density agglutinated assemblages indicative of eutrophic conditions. This complete faunal turnover and introduction of more severe eutrophic conditions began impacting the microfauna between 1950 and 1960, around the same time that many of the oyster reefs in the northwestern portion of the bay became unharvestable. Increases in the sediment mass-accumulation rates and geochemical evidence from bulk stable carbon and nitrogen isotopes support increased terrestrial, freshwater, and sediment input over the same interval. These biological and physical changes all indicate significant anthropogenic forcing. Although the data set is not complete, patterns have been identified in the data that indicate a significant change in Mobile Bay salinity, structure, and environmental health over the last century.
2011 GSA Annual Meeting in Minneapolis (9–12 October 2011)
General Information for this Meeting
|Session No. 194|
Minneapolis Convention Center: Room L100FG
1:30 PM-5:30 PM, Tuesday, 11 October 2011
Geological Society of America Abstracts with Programs, Vol. 43, No. 5, p. 479
© Copyright 2011 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.