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Keyword [Bering]
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1. Distribution Of Chlorofluorocarbon And Its Tracer Study Of Water Masses In The Arctic Ocean, Bering Sea And The Southern South China Sea
2. Study On The Change Of Polynyas In The Bering Sea And Corresponding Ocean Process
3. Study On The Diversity Of Cytophaga-Flavobacteria Cluster In Typical Areas Of The China Seas And The Bering Sea
4. A Dipole Pattern Between The Sea Of Okhotsk And The Bering Sea And Its Influence On The Atmosphere Circulation
5. Effects Of Pacific Inflow On Arctic Sea Ice
6. Pylogenetic Analysis Of Bacterioplankton And Bacteria In Surface Sediments From The Northern Bering Sea
7. Contents And Distribution Of PCBs And Heavy Metals In Surface Sediments From Bering Sea, Chukchi Sea And Canada Basin
8. Research On Oil And Gas Reservoir Formation Law Of PuTaoHua Oil Bering Layer In PuXi Area
9. Meiofaunal Communities In The Study Area Of The Bering Sea And Chukchi Sea In Summer
10. Community Structure And Secondary Productivity Of Macrozoobenthos In The Bering Sea And Their Correlation With Environmental Factors
11. Hydrograpic Structure And Inter-Annual Variations Of Bering Sea And Chukchi In Summer
12. Comparative Study Of Sediment Cores From The Chukchi And Bering Basins And Its Paleoceanographic Implications During Late Quaternary
13. The Distribution Of The Sand Of Putaohua Oil Bering Layer In Taidong Area And The Control Action To Accumulation
14. Research On Diversity And Community Structure Of Picoplankton And Nanoplankton In The Arctic Ocean During Summer Seasons
15. 210Po-210Pb Disequilibria In Polar Seas In Summer
16. The Characteristic Analyses And Influencing Factors Of Bering Sea Water Mass
17. Study On The Spatiotemporal Variation Of Dimethyl Sulfide In The Bering Sea
18. Sources Of Terrestrial Organic Carbon In Surface Sediments Across The Bering And Chukchi Seas In The Arctic,Insights From Lignin Phenols
19. The Water Exchange In Bering Strait And Its Effects On Arctic Sea Ice
20. Variation Of Marine Productivity In The Bering Sea Shelf Under Global Warming And Its Implication For The Formation Of Source Rocks
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