B. Vidondo et al., PHYSICOCHEMICAL CHARACTERISTICS OF A PERMANENT SPANISH HYPERSALINE LAKE - LA-SALADA-DE-CHIPRANA (NE SPAIN), Hydrobiologia, 267(1-3), 1993, pp. 113-125
La Salada de Chiprana Lake, located in the Ebro River basin, northeast
ern Spain, is the only permanent and deep water hypersaline ecosystem
in all of western Europe. With a total surface of 31 ha and a maximum
depth of 5.6 m, it has several basins bounded by elongated sandstone-b
odies or ribbons which are paleochannels of Miocene age. Its salinity
varied from 30 to 73 g l-1 during the 1989 hydrological cycle and the
most abundant ions were magnesium and sulphate. Depth-time distributio
ns of major physico-chemical variables demonstrated that the lake was
stratified in two distinctive layers during most of the year. The chem
ocline disappeared only in October, with the complete overturn of the
water column. In the deep water, three conditions occurred which allow
ed development of green sulphur bacteria populations: (1) oxygen deple
tion, (2) presence of hydrogen sulphide and (3) presence of light. Ben
thic microbial mats covered the sediments of shallow shores of moderat
e slope.