Data collected in three Californian estuaries indicate that hypersalin
e conditions exist during the dry summers typical of a Mediterranean c
limate. The generalised seasonal and longitudinal hydrographic structu
res are described and explained. It is argued that this seasonal hyper
salinity is common and that it represents a major class of estuaries.
The observed accumulation of salt indicates surprisingly long residenc
e times in small basins which have free exchange with the ocean. This
semi-isolation of the inner basin leads to a large build-up or severe
depletion of nutrients, pollutants and plankton in these systems. Of c
oncern are the trends to increase pollutant loading in the same system
s that are experiencing an increase in residence times owing to freshw
ater extraction in the watershed. (C) 1997 Academic Press Limited.