|Paper No. 151-1|
|Presentation Time: 1:30 PM-1:45 PM|
|THE KEY LARGO LIMESTONE REVISITED: PLEISTOCENE SHELF-EDGE FACIES, FLORIDA KEYS, USA|
MULTER, H.G., Fairleigh Dickinson University, 9855 State Route 961-F, Arkport, NY 14807-9606, firstname.lastname@example.org, GISCHLER, E., Geologisch-Paläontologisches Institut, J.W. Goethe-Universität, 60054 Frankfurt/Main, Germany, LUNDBERG, Joyce, Department of Geography, Carleton Univ, Ottawa, K1S5B6, Canada, SIMMONS, K.R., US Geol. Survey, Federal Center, Denver, CO 80225, and SHINN, Eugene A., Center for Coastal Geology, U. S. Geol Survey, 600 4th Street South, St. Petersburg, FL 33701|
The southern margin of the Pleistocene Florida Platform is well known from the coral-bearing Key Largo Limestone and the ooid-rich Miami Limestone that crop out along the island chain of the Florida Keys between Miami and Key West. These units were deposited during the last interglacial highstand of sea level ca. 125 yr BP (oxygen-isotope stage 5e). Based on sedimentological and chronological (U-series dating) investigations of 12 long and 57 short cores, the youngest of the well known Q units (Q1-Q5) of the Key Largo Limestone of south Florida was further subdivided into Q5e and post-Q5e. Individual units correspond to highstands of sea level, and units are, to a large part, separated from each other by subaerial exposure horizons reflecting sea level lowstands of the Pleistocene. Units Q1 and Q2 are characterized by abundant quartz and to a lesser extent by skeletal fragments of molluscs and foraminifera. We speculate that units Q1 and Q2 may have been deposited during the high sea levels of oxygen-isotope stage 11 between 420-360 ka. Abundant carbonate production and reef development occurred during deposition of unit Q3, presumably during isotope stage 9. The abundance of corals and coral boundstone decreases in unit Q4 (corresponding to isotope stage 7), which can be subdivided into a lower quartz-rich and an upper carbonate-rich succession. Unit Q5e (equivalent to isotope stage 5e), which forms the present day emergent Florida Keys, is again rich in massive corals (Montastrea annularis) and reefs. The seaward-dipping geometry of this unit and the scarcity of the Atlantic breakwater Acropora palmata support the contention that this Q5e platform margin had a ramp-type character. Shelf-margin reefs with Acropora palmata developed during deposition of post-Q5e units and correspond to highstands of sea level during isotope stages 5a and 5c. These deposits, which exhibit shelf margin wedge and offshore outlier reef geometries, act as Pleistocene foundations of the Holocene bank barrier reefs at the modern south Florida shelf edge.
2002 Denver Annual Meeting (October 27-30, 2002)
|Session No. 151|
Carbonate Stratigraphy, Diagenesis, and Geochemistry
Colorado Convention Center: A209
1:30 PM-5:30 PM, Tuesday, October 29, 2002
© Copyright 2002 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.