Lefebvre Jean-Pierre, Dolique F., Gratiot Nicolas. (2004). Geomorphic evolution of a coastal mudflat under oceanic influences : an example from the dynamic shoreline of French Guiana. Marine Geology, 208, p. 191-205. ISSN 0025-3227.
Titre du document
Geomorphic evolution of a coastal mudflat under oceanic influences : an example from the dynamic shoreline of French Guiana
Année de publication
2004
Type de document
Article
Auteurs
Lefebvre Jean-Pierre, Dolique F., Gratiot Nicolas
Source
Marine Geology, 2004,
208, p. 191-205 ISSN 0025-3227
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
