Fig. 5From: A 2700-year record of ENSO and PDO variability from the Californian margin based on coccolithophore assemblages and calcificationComparison between the mass of coccoliths of E. huxleyi, G. ericsonii, and G. muellerae (Top) and Pacific Decadal Oscillation (PDO) index (Mantua and Hare 2002). Red bands highlight periods of high PDOBack to article page