Osmotic and ionic regulation in the western rock lobster Panulirus longipes (Milne-Edwards)

The western rock lobster, Panulirus longipes (Milne-Edwards) is poikilosmotic over its tolerated salinity range, 25–45 ‰. Blood sodium is accumulated while chloride concentration is reduced. Sodium and chloride vary directly with the external salinity, although maintaining their differences in the same proportions as at normal salinity (36.0 ‰). Calcium is accumulated, ranging from over 150% at salinity 20 ‰ to about 117% at salinity 45 ‰. Potassium concentration is equivalent to the external at normal salinity, but is increased with lowered and decreased with raised salinity. Magnesium is reduced to about one-third that of the external concentration over the salinity range 20–40 ‰, but regulation begins to break down at 45 ‰. Individual ions exhibit, therefore, a range of regulation types, from poikilosmotic to homoiosmotic.Equilibrium for sodium, chloride, and calcium is attained in 10 h at salinities of 25, 30, 40 and 45 ‰ respectively. Rate constants for this exchange are linearly related to salinity differential, and rapid osmotic adjustment is by high permeability, equal in both directions, probably mainly via the gills. Muscle appears to act as a salt pool for sodium, chloride, and potassium but not for magnesium and calcium. Salt-loading causes a slight salt diuresis, the salts being excreted, probably via the gills. Except for calcium, there is no excretion of salt into the gut, but there is evidence of an exchange of chloride with another anion. Magnesium excretion is slow, and in the absence of osmotic stress possibly occurs via the antennal glands. All the ions examined appear to be regulated independently.