2006 Philadelphia Annual Meeting (22–25 October 2006)
Paper No. 130-9
Presentation Time: 10:25 AM-10:40 AM

THE MARTYRDOM OF ST. LUCIE: THE IMPORTANCE OF A BASELINE FAUNAL ASSESSMENT

HAYEK, Lee-Ann C., Chief Mathematical Statistician, Smithsonian Institution, National Museum of Natural History, MRC-121, Washington, DC 20560-0121, hayekl@si.edu and BUZAS, Martin A., Department of Paleobiology, Smithsonian Institution, National Museum of Natural History, MRC-121, Washington, DC 20560-0121, buzasm@si.edu

St. Lucie, the southernmost inlet of the Indian River Lagoon, is affected by a variety of stresses including dumping from Lake Okeechobee, the second-largest freshwater lake in the U. S., through a system of canals. In 2005 a particularly large discharge of fresh pollutant-saturated water resulted in losses of seagrass, bivalves, and diseased and dying fish. A program to monitor the macrofauna and assess its future is now underway. A comparison with the past, of course, is only possible if a baseline exists. Unlike the macrofauna, in 1975/76, such a baseline was established for the foraminifera. Thirty years later in 2005, the same area was re-sampled for foraminifera. In 1975/76 the mean density was 280 per 20 ml of sediment. In 2005, we observed a mean of 46 per 20 ml of sediment, a decline of 83%. In 1975/76 we observed 62 species while in 2005 we observed 13, a decline of 79%. The most abundant species constituted 42% of the fauna in 1975/76; in 2005 it had risen to 76%, a dramatic increase in dominance. The dramatic difference between the baseline and the present is plotted on a biodiversity gram (BDG) which depicts the canonical ensemble of species richness, compound diversity and evenness against the number of individuals on a single diagram.

2006 Philadelphia Annual Meeting (22–25 October 2006)
General Information for this Meeting
Session No. 130
Quaternary Micropaleontology: Quantifying Environmental Change
Pennsylvania Convention Center: 204 C
8:00 AM-12:00 PM, Tuesday, 24 October 2006

Geological Society of America Abstracts with Programs, Vol. 38, No. 7, p. 323

© Copyright 2006 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.