New Zealand Journal of Botany abstracts

---

Comparative palynomorph signals of vegetation change preserved in an adjacent peat swamp and estuary in North-West Nelson, New Zealand

R. K. Armour*
D. M. Kennedy^†

School of Earth Sciences
Victoria University of Wellington
P.O. Box 600
Wellington, New Zealand

*Present address: URS New Zealand Ltd,
P.O. Box 3367, Wellington, New Zealand.

 ^†Author for correspondence. David.Kennedy@vuw.ac.nz

Abstract  A history of vegetation for the mid–late Holocene was extracted from the southern margins of Whanganui Inlet and Mangarakau Swamp. These two sites represent very different pollen sinks with the estuary being dominated by fluvially transported material and the swamp by in situ pollen rain. They are, however, located very close to each other and therefore provide a unique study area to investigate how differing source environments affect pollen signals. A vegetation change from podocarps to beech forest is recorded in both settings at around 4000 years CalBP which is similar to that recorded at higher altitudes in the region. Robust palynomorphs were found in greater abundance in the inlet while the swamp contained a higher proportion of wetland species. Despite these differences both environments appeared to record a similar regional vegetation signal. This shows that estuarine environments, often characterised by material that has been transported, can provide accurate reconstructions of vegetation change.

Keywords  pollen; Whanganui Inlet; Holocene; coring; climate

B04047; Received 25 November 2004; accepted 5 April 2005; Online publication date 12 May 2005
New Zealand Journal of Botany, 2005, Vol. 43: 451–465
0028–825X/05/4302–0451 © The Royal Society of New Zealand 2005

PDF file of entire paper: Print-quality (2673K) | screen-quality (935K)

---

This year's abstracts | Journal home page | All abstracts | Publishing home page