Eurypterid–evaporite occurrences in the Appalachian basin were examined.
In a single eurypterid assemblage survey, 2% of specimens contained cross-cutting evaporites.
In a regional survey, 37% of eurypterid-bearing intervals contained salt hoppers.
A depositional model explains the frequent eurypterid–salt hopper associations.
Results refute the traditional view that eurypterids were halotolerant organisms.