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In many places on the present shoreface, offshore bar or beach sands with a sharp-basal contact overlie thin-bedded fine sands and muds. Ancient analogues are commonly interpreted as lowstand shoreface deposits lying on an erosional surface cut into the shelf during a relative sea-level fall. New observations may challenge this interpretation by providing evidence that such sequences develop during...
An overall estimate of the relationship between the changes in the nearshore morphology, the evolution of the sedimentary budget, the beach morphodynamics and the variation of grain-size characteristics along the beach barrier of Thau Lagoon, Languedoc, France, was attempted by synthesizing the data from different surveys: a basic survey of two separate grids of 11 closely-spaced (50 m) transverse...
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