Palynology, vegetation and climate of the Waikato lowlands, North Island, New Zealand, sincec.18,000 years ago

Abstract

The vegetational and climatic history of the Waikato lowlands during the last c. 18,000 years is inferred from the palynology of sediment cores from Lakes Rotomanuka, Rotokauri, and Okoroire. Intra- and inter-lake correlations were aided by multiple tephra layers interbedded with the lake sediments. The detailed chronological resolution given by these tephra sequences shows that late glacialpost glacial vegetational and climatic changes were nearly simultaneous throughout the Waikato lowlands.