Research Article| July 01, 1993 Lime-mud layers in high-energy tidal channels: A record of hurricane deposition Eugene A. Shinn; Eugene A. Shinn 1U.S. Geological Survey Coastal Center, 600 4th Street South, St. Petersburg, Florida 33701 Florida 33701 Search for other works by this author on: GSW Google Scholar Randolph P. Steinen; Randolph P. Steinen 2Department of Geology, University of Connecticut, Storrs, Connecticut 06268 Search for other works by this author on: GSW Google Scholar Robert F. Dill; Robert F. Dill 3GeoMarine Inc., San Diego, California 92106 Search for other works by this author on: GSW Google Scholar Richard Major Richard Major 4Bureau of Economic Geology, University of Texas, Austin, Texas 78713 Search for other works by this author on: GSW Google Scholar Geology (1993) 21 (7): 603–606. https://doi.org/10.1130/0091-7613(1993)021<0603:LMLIHE>2.3.CO;2 Article history first online: 02 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Eugene A. Shinn, Randolph P. Steinen, Robert F. Dill, Richard Major; Lime-mud layers in high-energy tidal channels: A record of hurricane deposition. Geology 1993;; 21 (7): 603–606. doi: https://doi.org/10.1130/0091-7613(1993)021<0603:LMLIHE>2.3.CO;2 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Abstract During or immediately following the transit of Hurricane Andrew (August 23-24, 1992) across the northern part of the Great Bahama Bank, thin laminated beds of carbonate mud were deposited in high-energy subtidal channels (4 m depth) through the ooid shoals of south Cat Cay and Joulters Cays. During our reconnaissance seven weeks later, we observed lime-mud beds exposed in the troughs of submarine oolite dunes and ripples. The mud layers were underlain and locally covered by ooid sand. The mud beds were lenticular and up to 5 cm thick. Their bases cast the underlying rippled surface. The layers were composed of soft silt- and sand-sized pellets and peloids and in some areas contained freshly preserved Thalassia blades and other organic debris along planes of lamination. The beds had a gelatinous consistency and locally had been penetrated by burrowers and plants. Layers of lime mud had also settled on bioturbated, plant-stabilized flats and in lagoonal settings but were quickly reworked and made unrecognizable by the burrowing of organisms. Thicker, more cohesive (and therefore older) mud beds and angular mud fragments associated with ooids from Joulters Cays have similar characteristics but lack fresh plant fragments. We infer that these older beds were similarly deposited and thus record the passage of previous hurricanes or tropical storms. Storm layers are preserved within channel sediments because migrating ooids prevent attack by the burrowing activity off organisms. This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not have access to this content, please speak to your institutional administrator if you feel you should have access.