Modern distribution of dinocysts from the North Pacific Ocean (37-64°N, 144°E-148°W) in relation to hydrographic conditions, sea-ice and productivity.
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PANGAEA
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Academy of Science Rise, Akademik M.A. Lavrentyev, Bering Sea, GE99/KOMEX_VI, GE99-10-2, GE99-12-3, GE99-30-2, GE99-31-3, GE99-38-3, INOPEX, KOMEX I, LV28, LV28-2-2, LV28-34-1, LV28-41-3, LV28-4-3, LV28-43-3, LV28-61-3, Marshal Gelovany, MIC, MiniCorer, MUC, MultiCorer, North Derugin Basin, North Pacific Ocean, North-West Kurile basin slope, Primary production of carbon, Primary production of carbon per area, yearly, Sakhalin shelf, Sample ID, Sea ice cover duration, Sea of Okhotsk, Sea surface salinity, August, Sea surface salinity, February, Sea surface salinity, summer, Sea surface salinity, winter, Sea surface temperature, August, Sea surface temperature, February, Sea surface temperature, summer, Sea surface temperature, winter, SO202/1, SO202/1_02-4, SO202/1_03-4, SO202/1_04-3, SO202/1_05-3, SO202/1_06-2, SO202/1_07-2, SO202/1_08-1, SO202/1_10-2, SO202/1_11-1, SO202/1_12-2, Sonne
Цитирование
Bonnet, Sophie; de Vernal, Anne; Gersonde, Rainer; Lembke-Jene, Lester (2012): Modern distribution of dinocysts from the North Pacific Ocean (37-64°N, 144°E-148°W) in relation to hydrographic conditions, sea-ice and productivity. Marine Micropaleontology, 84-85, 87-113, https://doi.org/10.1016/j.marmicro.2011.11.006