Bw. Hayward et al., FORAMINIFERAL ASSOCIATIONS IN WANGANUI BIGHT AND QUEEN-CHARLOTTE SOUND, NEW-ZEALAND, New Zealand Journal of Marine and Freshwater Research, 31(3), 1997, pp. 337-365
Eight benthic foraminiferal associations are recognised in Wanganui Ei
ght and Queen Charlotte Sound, New Zealand, based on cluster analysis
of census data from 52 sediment samples. Distribution of the four asso
ciations in Wanganui Eight correlates with increasing water depth: Elp
hidium charlottense/Haynesina depressula/Patellinella inconspicua asso
ciation (17-27 m); Patellinella inconspicua/Quinqueloculina suborbicul
aris association (20-42 m); Cassidulina carinata/Miliolinella subrotun
data association (42-66 m); and Cassidulina carinata/Bulimina submargi
nata (72-109 m). The four associations in Queen Charlotte Sound are: Q
uinqueloculina seminula/Elphidium advenum/Haynesina depressula in sand
y shallows (0.5-7 m); Epistominella vitrea/Haynesina depressula in sha
llows of the outer Sound (4-12 m); Elphidium vellai/Haynesina depressu
la in the mouth of the Sound (9-25 m); and Nonionella flemingi/Notouot
alia finlayi in a muddy, sheltered basin (25-42 m). The most important
physical factors influencing benthic foraminiferal distribution patte
rns in these two areas appear to be the characteristics of the water (
e.g., temperature, turbidity, salinity) and factors that vary with wat
er depth (e.g., wave and current energy, substrate, light penetration
food availability). Species diversity (alpha, H) and the relative abun
dance of planktic foraminiferal tests are mostly greater in the open s
ea conditions of Wanganui Eight than in Queen Charlotte Sound. In Wang
anui Eight both generally increase with increasing depth, although the
re is a local diversity peak at 70-80 m depth.