Geomorphic evolution of a coastal mudflat under oceanic influences: an example from the dynamic shoreline of French Guiana Jean Pierre Lefebvre a, * , Franck Dolique b , Nicolas Gratiot a a Laboratoire d’Ecologie Littorale, UR Elisa (UR053) IRD Guyane, BP 165, Rte de Montabo, Cayenne, Guyane Franc ¸aise 97323, French Guiana b Laboratoire Ge ´odal, Universite ´ du Littoral, De ´partement de Ge ´ographie, 2, chausse ´e des darses, Dunkerque 59140, France Received 17 June 2002; accepted 14 April 2004 Abstract The dynamics of the shoreline in French Guiana are characterized mainly by the northwestward migration of nearshore mudbanks. The passage of these features is responsible for significant geomorphic changes at the shoreline, such as the creation and erosion of extensive mudflats and the deviation of estuarine river mouths. Indeed, the hydrodynamic perturbation of the mean alongshore coastal currents generated by river discharge and tidal outflow from these estuaries can result in the immobilization of parts of a migrating mudbank, leading to the creation of a mudflat. Due to the general northwestward direction of coastal oceanic dynamics in this area, such mudflat development always occurs southeast (updrift) of the river mouths and consequently contributes to their northwestward diversion, forming a mudcape. Erosional processes on the marine side of mudcapes often result in a secondary outlet channel that gradually replaces the former main channel. In order to quantify the rate of these geomorphic changes, monitoring of an estuarine area was carried out at different time scales: on a decadal basis, from 1951 to 2001, with airborne sensing data, and over a shorter period covering a complete interbank situation (i.e., between the passage of two successive mudbanks), from 1999 to 2002, by means of field surveys and airborne digital videography. This short-term morphological monitoring was conducted from the early stage of mudflat consolidation and mangrove colonization to the arrival of the following mudbank at the edge of the study area. Various modes of erosion and the diversity of the eroded topography were highlighted by the study. Other aspects brought out by the work are the rate of mangrove colonization and its influence on the erosion processes, the influence of the tide on geomorphic processes, and the role of pioneer fluid mud deposits, related to the proximity of the next mudbank, on the dynamics of the mudflat system. D 2004 Elsevier B.V. All rights reserved. Keywords: estuarine mudcape; mudbank; littoral fringe; fluid mud layer 1. Introduction The coastline of French Guiana is part of the longest muddy coastline in the world fronting the open ocean (Fig. 1). This 1600 km mud belt extends from the mouth of the Amazon to the Orinoco River on the northeast coast of South America. The along- shore sediment flux along this coast is strongly regulated by the supply of mud from the Amazon River. This mud supply is reworked seasonally and interannually on the Amazon shelf of Brazil (Amas- 0025-3227/$ - see front matter D 2004 Elsevier B.V. All rights reserved. doi:10.1016/j.margeo.2004.04.008 * Corresponding author. E-mail address: j-p.lefebvre@wanadoo.fr (J.P. Lefebvre). www.elsevier.com/locate/margeo Marine Geology 208 (2004) 191 – 205