Assessing the ability of zonal δ18O contrast in benthic foraminifera to reconstruct deglacial evolution of Atlantic Meriodonal Overturning Circulation

However, whether the deglacial zonal delta O-18(c) contrast can represent the AMOC change is still unclear. delta O-18(c) contrast across the Florida Straits has been hypothesized as a proxy for the AMOC evolution during the last deglaciation, but the strength of Florida Current could also be influenced by wind forcing.

Here we examine the ability of the zonal delta O-18(c) contrast to reconstruct AMOC in a deglacial model simulation. The model simulation suggests that the deglacial variation of the Florida Current strength is dominated by AMOC, with the wind effect on the variation of the Florida Current being negligible. Furthermore, the delta O-18(c) contrast across the western boundary along the entire Atlantic and the basin-wide delta O-18(c) contrast in the North Atlantic in the upper ocean can also be used to reconstruct AMOC.