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- W2034453848 abstract "The modern North Pacific is the terminus for deep-water circulation. While no deep-water mass is formed today, the region is the source of North Pacific Intermediate Water (300–800 m) formed primarily in the Sea of Okhotsk . However, the source and strength of intermediate-water in the glacial North Pacific was likely different from the present intermediate-water. Here we present microfossil evidence of Late Quaternary ventilation changes associated with changes in intermediate-water. Intermediate-water ventilation decreased drastically at the glacial termination when it switched to the modern circulation system. The ventilation change appears to have been widespread and synchronous in the North Pacific. Glacial microfossil assemblages indicate that there was relatively strong ventilation of intermediate-water, which seems to have been cold and well-oxygenated as if produced by brine rejection during the formation of sea ice. On the basis of the glacial distribution of microfossils in the North Pacific, we suggest that intermediate-water was derived from the Bering Sea during the glacials, rather than the Sea of Okhotsk." @default.
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- W2034453848 date "2003-06-01" @default.
- W2034453848 modified "2023-10-16" @default.
- W2034453848 title "Last Glacial–Holocene change in intermediate-water ventilation in the Northwestern Pacific" @default.
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- W2034453848 doi "https://doi.org/10.1016/s0277-3791(03)00082-9" @default.
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