Glacial‐age hydrography of the far northwest Pacific Ocean

Stable isotope data on benthic foraminifera from more than 30 cores on the northern Emperor Seamounts and in the Okhotsk Sea are synthesized in paleohydrographic profiles spanning the depth range 1000–4000 m. Holocene (core‐top) benthic foraminiferal δ 18 O and δ 13 C data are calibrated to modern hydrographic properties through measurements of δ 13 C of ΣCO 2 and δ 18 O of seawater. Cibicidoides stable isotope ratios are close to the δ 13 C and equilibrium δ 18 O of seawater, whereas Uvigerina δ 18 O and δ 13 C are variably offset from Cibicidoides . Glacial maximum δ 13 C of Cibicidoides displays a different vertical profile than that of the Holocene. When results are adjusted by +0.32‰ to account for the secular change in δ 13 C during the last glacial maximum, the data coincide with the modern seawater and foraminiferal curves deeper than ∼2 km. However, at shallower depths δ 13 C gradually increases by as much as 1‰ above the modern value. Furthermore, above 2 km the benthic δ 18 O decreases by ∼0.5‰. These results are consistent with a benthic front at ∼2 km in the North Pacific see Herguera et al ., 1992, but they differ from interpretations based on trace metal data which indicate a source of nutrient‐depleted deep water during glaciation. The isotopic data suggest that during glaciation there was a better ventilated watermass at intermediate depths in the far northwestern Pacific, it was relatively fresher than deep waters there, and deep waters were as nutrient‐rich as today.