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Palynology, vegetation and climate of the Waikato lowlands, North Island, New Zealand, since c. 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 glacial-post glacial vegetational and climatic changes were nearly simultaneous throughout the Waikato lowlands.
Type
Journal Article
Type of thesis
Series
Citation
Newnham, R.M., Lowe, D.J. & Green, J.D. (1989). Palynology, vegetation and climate of the Waikato lowlands, North Island, New Zealand, since c. 18,000 years ago. Journal of the Royal Society of New Zealand, 19(2), 127-150.
Date
1989
Publisher
Royal Society of New Zealand
Degree
Supervisors
Rights
This article has been published in the journal: Journal of the Royal Society of New Zealand. © 1989 Journal the of Royal Society of New Zealand. Used with permission.