Figure 2.
Changes in coastal-food productivity on a typical high Pacific island between AD 1200 and AD 1400 were forced by a sea-level fall driven by cooling during the AD 1300 event Refer to the image caption for details.

Changes in coastal-food productivity on a typical high Pacific island between AD 1200 and AD 1400 were forced by a sea-level fall driven by cooling during the AD 1300 event

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