ABSTRACT. In studies of sessile organisms on intertidal boulders on 2 rock platforms near Sydney, Australia, the green alga Ulva lactuca and the tubeworm Galeolaria caespitosa were usually more abundant on one shore (Cape Banks). A likely explanation for this pattern was the difference in rocktype between the 2 shores -boulders were sandstone at one shore (Cape Banks) and shale or latente at the other (Long Reef). Experiments showed this explanation to b e correct, though not complete, for U. lactuca but incorrect for G. caespitosa. Further, a common spirorbid, normally equally abundant on both shores, settled and/or survived better on shale/ laterite. These results illustrate the dangers of drawing conclusions about processes based simply on observations of patterns.