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The cause(s) for the declines in marine mammal populations in the North Pacific and Bering Sea over the past 30 yr are unknown, despite progress in understanding the present ecology of this system. Explanations that attribute the declines to long-term decreases in marine productivity and/or short-term shifts in oceanographic conditions have been offered, but few studies have explored the issue from an explicitly historical perspective. Here we present a high-resolution, 52 yr time series of δ 13 C and δ 15 N values for teeth of juvenile male northern fur seal Callorhinus ursinus collected from a single colony on Saint Paul Island, Alaska in the eastern Bering Sea. Mean annual δ 13 C declined by ~1.1‰ from 1948 to 2000, while long-term mean annual δ 15 N did not significantly change. The relatively small but significant long-term decrease in δ 13 C most likely reflects anthro- pogenically-driven changes in surface ocean carbon reservoirs and not a decline in primary produc- tivity in the North Pacific and Bering Sea system. To assess short-term shifts in the time series, we de- trended the δ 13 C data; the δ 15 N time series did not require a correction. The corrected δ 13 C and uncorrected δ 15 N values showed low amplitude oscillations with a frequency of ~20 to 25 yr that are roughly in phase through time. The relative timing of these oscillations suggest they may be driven by shifts in the Pacific Decadal Oscillation (PDO); however, the frequency of cycles in our time series is approximately half as long as the frequency of the PDO. Finally, mean δ 13 C and δ 15 N values sug- gest that juvenile males modify their migration patterns by Age 3 (GL3, the third year of growth). Specifically, they remain in high-latitude waters year-round (southern Bering Sea and/or western Gulf of Alaska).

Historic decline in primary productivity in western Gulf of Alaska and eastern Bering Sea: isotopic analysis of northern fur seal teeth