Palaeobotanical Evidence for Changes in the Tertiary Climates of New Zealand - Tuatara: Volume 16, Issue 1, April 1968

Content Partner: Victoria University of Wellington. by D. R. McQueen1, D. C. Mildenhall2 and C. J. E. Bell1 Tertiary Climatic changes are inferred from changes in the plant micro-fossils described by Couper (1960). Critical forms are: the Nothofagus ‘fusca’ group for temperate conditions, the Nothof...

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Hauptverfasser: D. R. McQueen, D. C. Mildenhall, C. J. E. Bell
Format: Buch
Sprache:eng
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Zusammenfassung:Content Partner: Victoria University of Wellington. by D. R. McQueen1, D. C. Mildenhall2 and C. J. E. Bell1 Tertiary Climatic changes are inferred from changes in the plant micro-fossils described by Couper (1960). Critical forms are: the Nothofagus ‘fusca’ group for temperate conditions, the Nothofagus ‘brassi’ group for warm temperate or equivalent subtropical montane conditions, and some other...