Physical and biological controls on the formation of carbonate and siliciclastic bedforms on the north-east Brazilian shelf VIVIANE TESTA* and DANIEL W. J. BOSENCE   *CPGG ± Universidade Federal da Bahia, Campus Universita Ârio Ondina, Salvador, Bahia, 40170±290 Brazil (E-mail: vtesta@pppg.ufba.br)  Department of Geology, Royal Holloway University of London, Egham, Surrey, TW20 0EX, UK ABSTRACT The continental shelf of the State of Rio Grande do Norte, Brazil, is an open shelf area located 5°S and 35°W. It is in¯uenced by strong oceanic and wind- driven currents, fair weather, 1á5-m-high waves and a mesotidal regime. This work focuses on the character and the controls on the development of suites of carbonate and siliciclastic bedforms, based on Landsat TM image analysis and extensive ground-truth (diving) investigations. Large-scale bedforms consist of: (i) bioclastic (mainly coralline algae and Halimeda) sand ribbons (5±10 km long, 50±600 m wide) parallel to the shoreline; and (ii) very large transverse siliciclastic dunes (3á4 km long on average, 840 m spacing and 3±8 m high), with troughs that grade rapidly into carbonate sands and gravels. Wave ripples are superposed on all large-scale bedforms, and indicate an onshore shelf sediment transport normal to the main sediment transport direction. The occurrence of these large-scale bedforms is primarily determined by the north- westerly ¯owing residual oceanic and tidal currents, resulting mainly in coast- parallel transport. Models of shelf bedform formation predict sand ribbons to occur in higher energy settings rather than in large dunes. However, in the study area, sand ribbons occur in an area of coarse, low-density and easily transportable bioclastic sands and gravels compared with the very large transverse dunes in an offshore area that is composed of denser medium- grained siliciclastic sands. It suggests that the availability of different sediment types is likely to exert an in¯uence on the nature of the bedforms generated. The offshore sand supply is time limited and originates from sea ¯oor erosion of sandstones of former sea-level lowstands. The trough areas of both sand ribbons and very large transverse dunes comprise coarse calcareous algal gravels that support benthic communities of variable maturity. Diverse mature communities result in sediment stabilization through branching algal growth and binding that is thought to modify the morphology of dunes and sand ribbons. The occurrence and the nature of the bedforms is controlled by their hydrodynamic setting, by grain composition that re¯ects the geological history of the area and by the carbonate-producing benthic marine communities that inhabit the trough areas. Keywords Bedforms, carbonate shelf, current-dominated, north-east Brazil, sand ribbons. INTRODUCTION Considerable work has been undertaken on the ¯ow dynamics and formation of siliciclastic bedforms on shallow marine shelves (Allen, 1968, 1985; MacCave, 1971; McLean, 1981; Stride, 1982; see also Ashley, 1990). Similar structures are also formed on shallow carbonate shelves (e.g. Farrow et al., 1979; Hine et al., 1981; Wilson, 1986; Shinn et al., 1990), but these have not been Sedimentology (1999) 46, 279±301 Ó 1999 International Association of Sedimentologists 279