Kjm. Dickinson et Af. Mark, Interpreting ecological patterns in an intact estuary, South-west New Zealand World Heritage Area, J BIOGEOGR, 26(4), 1999, pp. 913-932
Vegetation pattern, soil attributes, and salinity regimes along with severa
l other environmental factors were studied in a small (11 ha) but unmodifie
d estuary in south Westland, New Zealand. Part of an unmodified 40 km(2) ca
tchment within the South-west New Zealand World Heritage Area, the Hapuka E
stuary, formed behind a 5-km long barrier beach, provides considerable ecol
ogical value as well as baseline, conservation advocacy and educative poten
tials both in a national and international context. Seventy-four quadrats w
ere sampled randomly along five transects at right angles to the main Hapuk
a River. Eight plant communities comprising 141 native and thirteen exotic
vascular species, were differentiated using multivariate analyses, from bar
e mud (mean elevation 1.23 +/- 0.24 m above Mean Low Water Spring (MLWS)),
saltmarsh and shrubland associations through to the adjacent podocarp-broad
leaved rain forest (4.53 +/- 0.74 m above MLWS). Bulk density of the upper
10 cm of substrate varied from a maximum of 1.15 g cm(-3) in the lowest ele
vation association to a minimum of 0.15 g cm(-3) in the rain forest. pH sho
wed a similar trend with values of 6.97 and 4.31, respectively. The reverse
pattern was evident with organic matter, with the highest content (53% ODW
t) in the rain forest substrate. The water which irrigates the saltmarsh at
high tide reaches 15-19 parts per thousand salinity on calm days but may b
e much less saline when moderate to strong southerly winds counter the tida
l influence. Northerly winds, or a southern outlet through the barrier beac
h, intermittently evident in the past, are likely to enhance salinity of th
e tidal waters across the saltmarsh.
Ordination of the vegetation samples indicated a very strong gradient assoc
iated with Axis 1 (eigenvalue=0.872) and Axis 2 (eigenvalue=0.461). Vector
fitting of nine measured environmental factors indicated a strong positive
correlation with Axis 1 of the ordination, of soil pH, sodium and conductiv
ity, and negative correlations with elevation, soil water, organic matter a
nd potassium contents.