First documentation of tidal-channel sponge biostromes (upper Pleistocene, southeastern Florida)

• Published in: Geology (Boulder) 2007-05, Vol.35 (5), p.475-478
• Main Authors: Cunningham, Kevin J, Rigby, J. Keith, Wacker, Michael A, Curran, H. Allen
• Format: Article
• Language: English
• Subjects: Atlantic Coastal Plain; biogenic structures; biostromes; Cenozoic; coastal environment; Coral reefs; cores; Dade County Florida; Demospongea; Florida; Geology; geometry; growth; high-energy environment; intertidal environment; Invertebrata; Marine; Marine biology; marine environment; Miami Limestone; Miami-Dade County Florida; Ocean currents; paleoecology; Pleistocene; Porifera; Quaternary; Quaternary geology; reef builders; sed rocks, sediments; Sedimentary petrology; sedimentary structures; shallow-water environment; shore features; size; southeastern Florida; Studies; tidal channels; trophic analysis; tropical environment; United States; upper Pleistocene
• ISSN: 0091-7613; 1943-2682
• DOI: 10.1130/G23402A.1

Sponges are not a common principal component of Cenozoic reefs and are more typically dominant in deep-water and/or cold-water localities. Here we report the discovery of extensive upper Pleistocene shallow-marine, tropical sponge biostromes from the Miami Limestone of southeastern Florida built by a new ceractinomorph demosponge. These upright, barrel- to vase-shaped sponges occur in monospecific aggregations constructed within the tidal channels of an oolitic tidal-bar belt similar to modern examples on the Great Bahama Bank. The biostromes appear to have a ribbon-like geometry, with densely spaced sponges populating a paleochannel along a 3.5 km extent in the most lengthy biostrome. These are very large (as high as 2 m and 1.8 m in diameter), particularly well-preserved calcified sponges with walls as hard as concrete. Quartz grains are the most common particles agglutinated in the structure of the sponge walls. Where exposed, sediment fill between the sponges is commonly a highly burrowed or cross-bedded ooid-bearing grainstone and, locally, quartz sand. It is postulated that the dense, localized distribution of these particular sponges was due to a slight edge over competitors for food or energy supply and space in a stressed environment of tidal-influenced salinity and nutrient changes, strong currents, and frequently shifting submarine sand dunes. To our knowledge, this represents the first documentation of sponge biostromes composed of very large upright sponges within high-energy tidal channels between ooid shoals. The remarkably well-preserved accumulations provide an alternative example of sponge reefs for comparative paleoenvironmental studies.