The purpose of the project is to use benthic foraminifera to investigate the condition of the ecosystem of Possession Sound, Everett, WA, part of Puget Sound. Puget Sound is a polluted water system due to the ports, oil refineries, paper mills, agricultural runoff, and previously, a smelter. Possession Sound itself is home to private properties, a naval station, ports, marinas, and an asphalt plant on the waterfront. Foraminifera are marine protists with calcareous or agglutinated shells (tests) that are readily preserved in sediments. Because they are sensitive to environmental conditions such as bottom water pH, organic and metal pollutants, and change in temperature, they can be indicators of environmental conditions at the sediment/water interface. Calcareous foraminifera exposed to water with decreasing pH have increasing levels of test dissolution, however, agglutinated species don’t dissolve. For this study, sediment samples were collected by the Washington State Department of Ecology; and sub-samples were sent to the Burke Museum. Thirty samples were processed; each was washed through a 63 screen, floated in trichloroethylene to remove the heavier sediment, then picked for around 300 foraminifera/sample. Foraminifera were identified for analysis of their assemblages, condition, and signs of dissolution. These signs are chalkiness, pitting, holes in the shells, and removal of shell layers. The hypotheses are as follows. Dissolution will have increased over time as Puget Sound water quality has decreased in recent years. Worse water quality will result in fewer calcareous species. Foraminifera will be fewer in number since 1997, with a higher proportion being agglutinated species. Results of this investigation will deliver insight into benthic conditions of Puget Sound, specifically Possession Sound, but could also provide useful information for people who rely on Puget Sound’s benthic conditions, such as the oyster and crab industry.