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Collecting Samples My first point of collection along the North West Arm was near the main sewage outlet at Point Pleasant Park, on a foggy evening in April. I combed the shores for two hours (at low tide) and found only four periwinkles. However, the abundance of periwinkle shells indicated that the population must have been more pervasive at other times. I returned the following day at high tide and found no presence of periwinkles, and even the broken shells had been washed out to sea. On both occasions I collected water samples in sterile containers, which I later tested for pH level, turbidity, and the level of chlorine present. I returned to this area on a sunny day when the amount of bacteria in the water is known to be lower. I found few traces of periwinkles at either high or low tide. On a bright May evening one week later, I examined the beach near a secondary sewage outlet along Jubilee Road; this is also the location of a popular recreation area, the Saint Mary's Boat Club. At first, the only traces of periwinkles were scattered shell remains on the beach. After further investigation, however, I found 12 common periwinkles along a 30-meter stretch of beach. Along the same stretch of beach were several pounds of dehydrated black seaweed and an abundance of garbage. The 12 periwinkles were all found suctioned to the bottom of a large igneous rock two meters from the waterline. I collected three of these periwinkles, as well as one stalk of green seaweed, 0.5 kilos of igneous rock, 0.25 kilos of sand, and two liters of North West Arm water. I then arranged the contents in a 20-liter tank. I returned later in the week, during inclement weather, to collect another sample of water. This was to document the changes in concentrations of fecal bacteria, metals, and PCBs to give a more accurate picture of the Arm's environment. |
North West Arm
Click to enlarge Graves Island ![]() Periwinkle specimens were collected from sites in the contaminated North West Arm as well as from sites at Graves Island, a relatively pristine environment. The environments around the polluted habitat and the control habitat are essentially geologically identical. Both collection points are situated along bays on the eastern coast of Nova Scotia bordering the Atlantic Ocean. The underlying rock is from the Mefima Group, and the primary deposits are slate, schist, and migmatite, which formed approximately 450 million years ago. The thin layer of topsoil in the surrounding area is the result of glaciation that occurred 10,000 years ago. The soil along the shore is formed from decomposed lichens. As a result of similar soil conditions, both environments support the same species of trees. Examples include the black spruce, white spruce, red maple, red oak, and white pine. After surveying both areas, I found that concentrations of these species within a 10-meter by 10-meter enclosure were essentially the same. In both environments, coniferous trees were more dominant than deciduous. |














