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A Vegetation History of the Far North of New Zealand during the Late Otira (Last) Glaciation

Published online by Cambridge University Press:  20 January 2017

Rewi Newnham
Affiliation:
Department of Geography, University of Otago, Dunedin, New Zealand
John Ogden
Affiliation:
Department of Botany, University of Auckland, Auckland, New Zealand
Dallas Mildenhall
Affiliation:
DSIR Geology and Geophysics, Lower Hutt, New Zealand

Abstract

During the latter part of the last (Otira) glaciation the forest cover of New Zealand was much reduced. It has frequently been postulated, however, that diverse mixed forest communities survived in the far north of North Island. Pollen diagrams and radiocarbon dates from two last glacial and postglacial (Aranuian) sits on the Aupouri Peninsula in the far north of New Zealand are compared with other published palynological and plant macrofossil evidence from the region. Mixed kauri/podocarp/angiosperm forest was present at times during the late Otiran (and Aranuian) and no evidence was found for substantial loss of forest. However, radiocarbon samples from one site, at least, seem to have been contaminated with young carbon; this introduces uncertainty into the chronology established at that site. Possibly nondeposition or erosion has obscured part or all of the late Otiran record at all the sites studied so that very much reduced forest cover at that time cannot be ruled out.

Type
Articles
Copyright
University of Washington

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References

Brown, L. J., and Wilson, D. D. (1988). Stratigraphy of the late Quaternary deposits of the northern Canterbury Plains, New Zealand. New Zealand Journal of Geology and Geophysics 31, 305335.Google Scholar
Burrows, C. J. (1988). Late Otiran and early Aranuian radiocarbon dates from South Island localities. New Zealand Natural Sciences 15, 2536.Google Scholar
Clayton-Greene, K. A. (1978). Aspects of the distribution of certain indigenous woody species in the Waikato District, New Zealand. Journal of the Royal Society of New Zealand 8, 283291.Google Scholar
Dawson, J. W. (1985). Metrosideros bartlettii (Myrtaceae) a new species from North Cape, New Zealand. New Zealand Journal of Botany 23, 607610.Google Scholar
Dick, R. S. (1950). “The Plant Geography of the “Far North” New Zealand.” Unpublished MS thesis, University of Auckland.Google Scholar
Dieffenbach, E. (1843). “Travels in New Zealand,” Vol. 1. John Murray, London.Google Scholar
Dodson, J. R. Enright, N. J., and McLean, R. F. (1988). A late Quaternary vegetation history for far northern New Zealand. Journal of Biogeography 15, 647656.CrossRefGoogle Scholar
Enright, N. J. McLean, R. F., and Dodson, J. R. (1988). Late Ho-locene development of two wetlands in the Te Paki region, far northern New Zealand. Journal of the Royal Society of New Zealand 18, 369382.Google Scholar
Faegri, K., and Iversen, J. (1964). “Textbook of Pollen Analysis” (1st, Ed.). Blackwell, London.Google Scholar
Gardner, R. O., and Bartlett, J. K. (1980). Forest flora of the North Cape region. Tane 26, 223234.Google Scholar
Goh, K. M. Tonkin, P. J., and Raftner, T. A. (1978). Implications of improved radiocarbon dates of Timaru peats on Quaternary loess stratigraphy. New Zealand Journal of Geology and Geophysics 21, 463466.Google Scholar
Goldie, P. J. (1975). “The Quaternary Geology of an Area North of Houhora.” Unpublished MS thesis, University of Auckland.Google Scholar
Harkness, D. D. (1975). The role of the archaeologist in C-14 measurement. In “Radiocarbon: Calibration and Prehistory” (Watkins, T., Ed.), pp. 128135. Edinburgh Univ. Press, Edinburgh.Google Scholar
Hicks, D. L. (1975). “Geomorphic Development of the Southern Aup-ouri and Karikari Peninsulas with Special Reference to Sand Dunes.” Unpublished MS thesis, University of Auckland.Google Scholar
Hogg, A. G. (1982). Radiocarbon dating at the University of Waikato, New Zealand. Department of Earth Sciences, University of Waikato Occasional Report, 8, 52.Google Scholar
Leitch, E. C. (1966). “The Geology of the North Cape Area, Northernmost New Zealand.” Unpublished MS thesis, University of Auckland.Google Scholar
Macphail, M. K., and McQueen, D. R. (1983). The value of New Zealand pollen and spores as indicators of Cenozoic vegetation and climates. Tuatara 26, 3759.Google Scholar
McGlone, M. S. (1982). Modern pollen rain, Egmont National Park, New Zealand. New Zealand Journal of Botany 20, 253262.Google Scholar
McGlone, M. S. (1988). New Zealand. In “Vegetation History” (Huntley, B. and Webb, T. III, Eds.), pp. 557599. Kluwer Academic.Google Scholar
McGlone, M. S., and Moar, N. T. (1977). The Ascarina decline and post-glacial climatic change. New Zealand Journal of Botany 15, 485489.Google Scholar
Mclntyre, D. J. (1963). Pollen morphology of the New Zealand species of Myrtaceae. Transactions of the Royal Society of New Zealand Botany 2, 83170.Google Scholar
McLean, R. F. Enright, N. J. Mitchell, N. D., and Braggins, J. E. (1985). “Wetlands and Heathlands of the Te Paki Region.” Report to the New Zealand Department of Lands and Survey. Geography Department, University of Auckland.Google Scholar
Mildenhall, D. C. (1973). Vegetational changes in the New Zealand Quaternary based on pollen studies, with brief comments on the Pliocene background. In “The New Zealand Quaternary—An Introduction” (Mansergh, G. D., (Ed.). INQUA IX International Con-gress, 1973, Christchurch, pp. 2032.Google Scholar
Mildenhall, D. C. (1974). “Report on a Series of Palynological Samples from Great Exhibition Bay, Te Kao Bay, and other Quaternary Localities on Sheet N4.” Palynological Section Report, New Zealand Geological Survey, D.S.I.R., Lower Hutt, September, 1974.Google Scholar
Mildenhall, D. C. (1985). Quaternary palynology: North Kaipara Barrier. New Zealand Journal of Geology and Geophysics 28, 121127.Google Scholar
Millener, P. R. (1981). The Quaternary avifauna of the North Island of New Zealand. Unpublished Ph.D. thesis, University of Auckland.Google Scholar
Mitchell, N. D. (1984). “The Forest Remnants of Te Paki.” Unpublished report, Botany Department, University of Auckland.Google Scholar
Moir, R. W. Colleen, B., and Thompson, C. S. (1986). The climate and weather of Northland. New Zealand Meteorological Service Miscellaneous Publication 115(2).Google Scholar
Newnham, R. M. (1990). “Late Quaternary Palynological Investiga-tions into the History of Vegetation and Climate in Northern New Zealand.” Unpublished Ph.D. thesis, University of Auckland.Google Scholar
Newnham, R. M. (in press). A 30,000 year pollen, vegetation, and climate record from Otakairangi, Northland, New Zealand. Journal of Biogeography. Google Scholar
Newnham, R. M. Lowe, D. J., and 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, 127150.Google Scholar
Newnham, R. M., and Lowe, D. J. (1991). Holocene vegetation and volcanic activity, Auckland Isthmus, New Zealand. Journal of Quaternary Science 6, 177193.CrossRefGoogle Scholar
Ogden, J. (1985). An introduction to plant demography with particular reference to New Zealand trees. New Zealand Journal of Botany 3, 751772.Google Scholar
Ogden, J. Newnham, R. M. Palmer, J. G. Serra, R. G., and Mitchell, N. D. (1993). Climatic implications of macro- and micro-fossil assemblages from late Pleistocene deposits in northern New Zealand. Quaternary Research 39, 107119.Google Scholar
Pocknall, D. T. (1978). Relative pollen representation in relation to vegetation composition, Westland, New Zealand. New Zealand Journal of Botany 16, 379386.Google Scholar
Polach, H. (1976). Radiocarbon dating as a research tool archaeology— hopes and limitations. In “The Proceedings of a Symposium on Scientific Methods of Research in the Study of Ancient Chinese Bronzes and Southeast Asian Metal and Other Archaeological Artifacts” (Barnard, N., Ed.). National Gallery of Victoria, Melbourne.Google Scholar
Ricketts, B. D. (1979). Petrology and provenance of Pleistocene deposits in the south Parengarenga—Te Kao district, northern New Zealand. New Zealand Journal of Geology and Geophysics 22, 2127.Google Scholar
Wardle, P. (1963). Evolution and distribution of the New Zealand flora as affected by Quaternary climates. New Zealand Journal of Botany 1, 317.Google Scholar
Wardle, P. (1964). Facets of the distribution of forest vegetation in New Zealand. New Zealand Journal of Botany 2, 352366.Google Scholar
Wardle, P. (1988). Effects of glacial climates on floristic distribution in New Zealand. 1. A review of the evidence. New Zealand Journal of Botany 26, 541555 Google Scholar