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22. Long-term variations in Iceland–Scotland overflow strength during the Holocene
23. Persistent export of 231Pa from the deep central Arctic Ocean over the past 35,000 years
24. Transient stratification as the cause of the North Pacific productivity spike during deglaciation
25. 231Pa/230Th evidence for a weakened but persistent Atlantic meridional overturning circulation during Heinrich Stadial 1
26. Advection and scavenging controls of Pa/Th in the northern NE Atlantic
27. Oceanographic dynamics and the end of the last interglacial in the subpolar North Atlantic
28. Silicon isotopes indicate enhanced carbon export efficiency in the North Atlantic during deglaciation
29. What do benthic δ13C and δ18O data tell us about Atlantic circulation during Heinrich Stadial 1?
30. Large deglacial shifts of the Pacific Intertropical Convergence Zone
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