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- Chapter contents
- Abstract
- Introduction
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Background
- Scientific objectives
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Summary of expedition results
- References
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Figures
- F1. Location map.
- F2. Surface water circulation and topography.
- F3. Subsurface water circulation and topography.
- F4. Temperature, salinity, dissolved oxygen, and drilling transect.
- F5. Sedimentation rates.
- F6. Location map, Site U1340.
- F7. Location map, Sites U1343–U1345.
- F8. Location map, Site U1339.
- F9. Age-depth plot, Hole U1340A.
- F10. Age-depth plot, Site U1341.
- F11. Age-depth plot, Site U1342.
- F12. Age-depth plot, Site U1339.
- F13. Age-depth plot, Site U1343.
- F14. Age-depth plot, Site U1344.
- F15. Age-depth plot, Site U1345.
- F16. Lithostratigraphic summary.
- F17. Shipboard analyses, Site U1340.
- F18. Shipboard analyses, Site U1341.
- F19. Shipboard analyses, Site U1342.
- F20. Shipboard analyses, Site U1339.
- F21. Shipboard analyses, Site U1343.
- F22. Shipboard analyses, Site U1344.
- F23. Shipboard analyses, Site U1345.
- F24. Potassium content.
- F25. NRM/MS.
- F26. Sea ice coverage.
- F27. Biological productivity and temperature.
- F28. Deep infaunal benthic foraminifers related to low dissolved-oxygen content.
- F29. Eggerella bradyi, Martinottiella communis, Cycladophora davisiana.
- F30. Dissolved chemical concentrations.
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Tables
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PDF file
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doi:10.2204/iodp.proc.323.101.2011
Scientific objectives
The objectives of Expedition 323 are as follows:
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To elucidate a detailed evolutionary history of climate and surface-ocean conditions since the earliest Pliocene in the Bering Sea, where amplified high-resolution changes of climatic signals are recorded;
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To shed light on temporal changes in the origin and intensity of NPIW and possibly deeper watermass formation in the Bering Sea;
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To characterize the history of continental glaciation, river discharges, and sea ice formation in order to investigate the link between continental and oceanic conditions of the Bering Sea and adjacent land areas;
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To investigate linkages, through comparison to pelagic records, between the ocean/climate processes that occur in the more sensitive marginal sea environment of the Bering Sea and those that occur in the North Pacific and/or globally. This objective includes evaluating how the ocean/climate history of the Bering Strait gateway region may have affected North Pacific and global conditions; and
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To constrain global models of subseafloor biomass and microbial respiration by quantifying subseafloor cell abundance and pore water chemistry in an extremely high productivity region of the ocean. We also aim to determine how subseafloor community composition is influenced by high productivity in the overlying water column.
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