Crayfish have a long evolutionary history in temperate fresh water (FW
). Ion regulation is challenged by low external concentrations of Na,
Cl, and Ca (<1 mM). In intermolt the primary concern is Na and Cl bala
nce; around ecdysis the emphasis switches to Ca regulation as the cuti
cle is decalcified/calcified. Compared with marine crustaceans, interm
olt crayfish maintain a reduced extracellular (EC) osmolality and have
lower permeability to both ions and water. Hyperregulation involves a
ctive branchial uptake of Na and Cl and the unique ability to produce
a hypotonic urine. Ion uptake involves apical electroneutral ion excha
nge (Na+ for H+; Cl- for HCO3-; counterions provided from CO2 via carb
onic anhydrase) followed by active basolateral transport of Na via the
Na pump, with Cl following passively. Reabsorption of 95% of filtered
electrolytes at the antennal gland (kidney) involves similar subcellu
lar mechanisms in a morphologically differentiated region of the dista
l tubule. Intermolt crayfish exhibit negative Ca balance (passive effl
ux unopposed by uptake) tolerable in view of the large cuticular CaCO3
reserve. In premolt, cuticular Ca is reabsorbed. A small amount is st
ored as gastroliths, the remainder is lost via branchial excretion and
in the discarded exuviae. At ecdysis, FW uptake generates the physica
l force for shedding, leaving the crayfish with dilute hemolymph and a
Ca deficiency. Levels of EC Na and Cl are restored by intensive postm
olt branchial uptake. Mineralization of the soft exoskeleton involves
remobilization of stored Ca and branchial uptake of Ca and HCO3. Trans
epithelial Ca transport involves Ca2+ ATPase and Ca2+/Na+ exchange. Th
e importance of external electrolytes and pH in postmolt ion regulatio
n is explored, as are some allometric considerations.