While Okhotsk‐1 displayed a relatively stable Δ 14 C record within the range of −8‰ to −23‰, Okhotsk‐2 showed an increasing trend from about −40‰ (at x = 7.60‰–31.31%) to about −20‰ (at x = 56.50‰–77.63%).
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Otolith radiocarbon signatures provide distinct migration history of walleye pollock around Hokkaido, Japan in the North-Western Pacific.
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