| Summary: | The subarctic Pacific Ocean, which is linked to both polar and tropical climates, is an area of high marine productivity and sensitive to ocean-atmosphere CO 2 flux, however, the mechanisms underlying the drivers of its productivity dynamics or patterns remain elusive. Using biogenic barium, opal, and terrgenous input in sediment core since the past 230 kyr, we present a continuous high resolution nutrient availability dynamic for the subarctic Pacific Ocean and assess possible changes to sea ice and glacial North Pacific Intermediate Water on nutrient upwelling in the region. We suggest that export production in this region is controlled by the freshwater discharge associated with moisture and heat from low-latitude and the iceberg discharge from Kamchatka glaciations under a weak Aleutian Low. These findings indicate that both high- and low-latitude climate systems forced the evolution of marine environment and primary productivity in the high-latitude North Pacific.
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