An Integrated View of Organic Biomarker‐Based Sea Surface Temperature Changes in the Subarctic Pacific Since the Last Ice Age

Abstract

A prevailing view for abrupt millennial-scale climate fluctuations during the last deglaciation in the Northern Hemisphere is tightly linked to changes in the Atlantic meridional overturning circulation (AMOC) (McManus et al., 2004). Evidence suggests that perturbations in the North Pacific can also have a significant impact on regional and global climate fluctuations by altering the poleward transport of heat and moisture (Praetorius