Journal of the Royal Society of New Zealand abstracts
Stratigraphy, landsnail faunas, and paleoenvironmental history of coastal
dunefields at Te Werahi, northernmost New Zealand
F. J. Brook*
*Department of Conservation, P. O. Box 842, Whangarei, New Zealand
During Quaternary time, the history of the Te Werahi area included episodes of
dunefield formation alternating with periods of extensive erosion of sand
cover. Dune units of last interglacial age and older crop out as isolated
erosional remnants within and adjacent to an extensive Holocene dunefield. The
latter had begun to form by at least 4000 years BP, and dune mobilisation
continued until about 1800 years BP, possibly with increased dune movement
after 3000 years BP. A smaller Holocene dunefield on Motuopao Island also
formed before about 1800 years BP. After 1800 years BP, the Te Werahi and
Motuopao dunefields entered a stable phase that persisted until about 450 years
BP, followed by dune remobilisation and erosion that has continued to the
present day.
Analysis of fossil landsnail faunas indicates that forest was widespread in
the Te Werahi area in mid Holocene time, was mostly over-run by dunes by about
1900 years BP, and then locally re-established on the dunefield between about
1800 and 800 years BP. That dune forest was destroyed between 800 and 550 years
BP, probably as a result of anthropic firing following Polynesian settlement,
and has not subsequently re-established. Vegetation disturbance on the Te
Werahi dunefield since at least 4000 years BP has resulted in cumulative
extinctions and impoverishment of native landsnail faunas, especially during
major extinction pulses before 1900 years BP and between 800 and 550 years
BP.
Keywords landsnails; coastal dunes; islands; Holocene;
Pleistocene; biogeography; diversity; extinction; vegetation history; northern
New Zealand
(c) Journal of The Royal Society of New Zealand,
Volume 29, Number 4, December 1999, pp 361-393
PDF file of entire paper: medium quality (2175K); (scanned from paper original: notes about this process)
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