Seasonal and Spatial Variation of Particulate Cadmium and Phosphorous along Line P in the Northeast Pacific

Line P is a transect along 50°N in the subarctic North Pacific that stretches from Sanich Inlet out to Ocean Station PAPA (OSP). Between February 1996 and March the following year, size fraction suspended particulate matter was collected (<1 μm, 1-51 μm and >51 μm) using the Multiple Unit Large Volume Filtration System (MULVFS) technique. Over the course of 4 cruises, 17 MULFS casts were taken. Using this large dataset, we examine the seasonal and spatial variability of cadmium content of particles. Throughout this one year time span, the particulate Cd uptake relative to P varied by a factor of two at individual sites during different seasons and by a factor of three at different sites during the same season.

Typically, the Cd:P content of phytoplankton increases going from Sanich Inlet out toward station PAPA. While Sanich Inlet is an iron and zinc replete coastal environment, OSP is located in an HNLC region with low dissolved Fe and Zn concentrations. We compared the Cd:P profiles along the Line P transect to that of other divalent metals, specifically Zn, Mn, Co, Ba and Fe. While Fe:P, Mn:P and Co:P are highest in the coastal environment, Cd:P is higher in the open ocean environment. Cd:P peaks in the open ocean station below the mixed layer. We also compare the relationship between oxygen and Cd content in particles. The reason for Cd uptake by marine organisms is still not fully understood; by examining particles in a well-studied region with seasonal, nutrient, environmental and other divalent metal concentrations in particles, we can better understand the causes for variability.