USGS - science for a changing world

FISC - St. Petersburg

Coastal & Marine Geology Program > Center for Coastal & Watershed Studies > Professional Paper 1751

Systematic Mapping of Bedrock and Habitats along the Florida Reef Tract—Central Key Largo to Halfmoon Shoal (Gulf of Mexico)

USGS Professional Paper 1751

by Barbara H. Lidz, Christopher D. Reich, and Eugene A. Shinn

Introduction:
Table of Contents
Project Overview
Project Objective
Geologic Setting
Primary Datasets
Primary Products - Overview Maps & Evolution Overview:
Bedrock Surface map.
Introduction
Depth to Pleistocene Bedrock Surface
Reef & Sediment Thickness
Benthic Ecosystems & Environments
Sedimentary Grains in 1989
Summary Illustration Index Map
Evolution Overview
Tile-by-Tile Analysis
Satellite image of the Florida Keys showing location of tiles.
Organization of Report
Tiles: 1, 2, 3, 4,
5, 6, 7/8, 9/10,
11
Summary
Acknowledg-
ments
References
Disclaimer
Related
Publications

Tile 6

Eastern Sambo: Eastern Sambo and Maryland Shoal flank Pelican Shoal (Fig. 91B). A single, moderately well developed outlier-reef tract is positioned at the seaward terrace edge off Eastern Sambo (Fig. 89, line 2) and Maryland Shoal (Fig. 95) but is absent off Pelican Shoal (Fig. 94A). Instead, a low-relief, bedrock dune-ridge type of accretion is present in the same location off Pelican Shoal. The low-relief feature is clearly part of the outlier-reef tract but a part that simply never experienced Pleistocene coral growth, as is judged from the smoothly rounded seismic reflection. Compare its smoothness (Fig. 94A) with the jaggedness of reflections over areas of known Holocene shelf-edge coral reefs (for example, Fig. 95). There is no seismic evidence that outlier reefs ever grew off Pelican Shoal. Lidz (2004) referred to the Pelican Shoal feature as a poorly developed reef or paleoshoreline beach-dune ridge. If the Pelican Shoal terrace feature does represent a beach-dune ridge, its presence would support the hypothesis (Lidz et al., 1997a) that beach-dune ridges served as nuclei for outlier-reef development. Confirmation of the origination of this feature would require coring.

Coastal & Marine Geology Program > Center for Coastal & Watershed Studies > Professional Paper 1751

Accessibility FOIA Privacy Policies and Notices

Take Pride in America logo USA.gov logo U.S. Department of the Interior | U.S. Geological Survey
URL: [disc] /pubs/pp/2007/1751/professional-paper/tile6/eastern-sambo.html
Page Contact Information: Feedback
Page Last Modified: December 01, 2016 @ 04:14 PM (JSS)