Relationships between diatom assemblages and physicochemical factors w
ere examined in 63 saline lakes in western North America. Sodium was t
he overwhelmingly dominant cation in the lakes examined; lakes above 4
7-degrees latitude were dominated by SO4-2, and lakes below 47-degrees
were dominated by CO3-2 and Cl-1. This latitudinal gradient for anion
s was correlated with the distribution and community structure of diat
oms. Sixty-two taxa comprised > 85% of the total diatom relative abund
ance in the saline environments. There were strong negative correlatio
ns between specific conductance and diversity and species richness, ho
wever pH and major cations showed limited predictive value. Cluster an
alyses identified diatom assemblages along specific conductance and ma
jor anion gradients. Indices for specific conductance and major anions
were also developed for 62 diatom taxa. These diatom indices provide
useful information to interpret past and present physicochemical condi
tions in lacustrine ecosystems. Greatest diversity was found in habita
ts with ionic concentrations < seawater and ion composition similar to
marine environments. Principal components analyses comparing loadings
for major cations and anions, ionic concentration, and diatom communi
ty structure suggested that shallow saline lakes may have provided evo
lutionary pathways for speciation of marine pennate diatoms into athal
assic (nonmarine) environments.