Last glacial–Holocene water structure in the southwestern Okhotsk Sea inferred from radiolarian assemblages

In order to reconstruct paleoceanographic conditions in the southwestern (SW) Okhotsk Sea, radiolarian assemblages were analyzed from 10 surface sediments and 5 sediment cores obtained from various water depths, ranging between 461 and 1348 m. We also measured geochemical components such as biogenic opal, calcium carbonate, total organic carbon, total sulfur and total nitrogen for one sediment core. These data imply that the complicated water structure in the SW Okhotsk Sea changed with time from the last glacial to Holocene. The glacial surface water was characterized by low primary production in the summer and expanded sea-ice coverage in the winter. During this time, the ventilation might have reached deeper than during the Holocene. During the major deglacial period including the melt-water pulses 1A and 1B, the deep-sea oxygen content had declined with less ventilation and/or more oxygen consumption with organic matter supply into the deeper depths. The intermediate layer has been well ventilated and has supplied large amount of organic matter during the last 20 kyrs, especially in the early-mid Holocene, however such condition ceased during 3 to 2 ka. The warm Pacific deep water has been present since 9 ka. The influence of warmer surface water such as the Soya Warm Current (SWC) increased in the coastal area during 7 to 4 ka and since 2 ka till present. Neritic-derived productivity might be extended at 2.2–1.8 ka and since 1.2 ka till present.