Benthic populations of inland lakes are commonly discussed in terms of organisms per square meter of bottom surface, often with reference to changes occurring during some period of time. However, the vertical distribution of animals within the sediments has been neglected to a great extent in North America. Lenz (1931) and Berg (1938) have contributed to our knowledge of this aspect of faunal distribution in European lakes. Moore (1939) and Cole (1949) have reported on the vertical distribution of the microbenthos in bottom deposits of certain lakes of this continent, but little information has been published concerning the stratification of macrobenthic forms, particularly the profundal organisms. APPARATUS AND METHODS Thirty benthic collections, each composed of three vertical core samples, were taken from profundal depths in Douglas Lake, Cheboygan County, Michigan, from August 4 to August 26, 1950. Eight collections were made in the upper profundal zone at a water depth of 16 meters, and twenty-two collections were taken from a depth of 19.5 meters. Both stations were in the South Fish Tail Bay depression along a transect extending lakeward from a permanent marker on the west shore. In addition to the 90 profundal core samples, 8 cores were taken at sublittoral and littoral depths for comparative purposes. All benthic collections were made with a small vertical core sampler, described in another paper (Cole, 1949). An inserted transparent plastic ttube served to collect the core of sediment and its biota. This tube was removed from the sampler, transported to the laboratory in a wooden rack, and the included mud was removed in sections for examination. The sectioning was accomplished, after the water overlying the core had been siphoned off, by pushing a rubber piston up the tube from the bottom. A rod, calibrated in centimeters, was used to push the piston, and hence the mud core, up through and above the upper edge of the tube. A tight-fitting, waterproof bowl encircled the tube, and served to catch watery sediment which spilled over the top. An ordinary glass slide was used to scrape the mud from the top of the tube, and a rubber syringe was employed in washing the outside of the tube and in removing the sediment from the bowl. The three cores, comprising one collection, were sectioned in succession and their corresponding strata consolidated in finger bowls. The upper 10 cm. of each core was sectioned at one cm. intervals and screened with a metal sieve of 80 meshes to the inch. The second 10 cm. was sectioned at 2 cm. intervals and screened 1 This investigation was made possible by a grant from the Research Fund, University of Louisville.