Lal. Debruyn et Aj. Conacher, THE BIOTURBATION ACTIVITY OF ANTS IN AGRICULTURAL AND NATURALLY VEGETATED HABITATS IN SEMIARID ENVIRONMENTS, Australian Journal of Soil Research, 32(3), 1994, pp. 555-570
The effect of ant activity on bioturbation rates was assessed in the c
entral wheatbelt of Western Australia in naturally vegetated and farml
and sites, by bimonthly measurements of soil fauna activity and period
ic measurements of ant nest dimensions. The percentage soil surface af
fected by soil fauna (%SSASF) was on average 0.5%, with the lowest act
ivity in cropped areas and the highest %SSASF recorded in pasture site
s (>2%). Overall %SSASF was greater on yellow sand in comparison with
grey sandy loam. The estimated bioturbation rates of ant communities i
n naturally vegetated and farmland habitats on both soils ranged from
10 to 37 g m-2 yr-1. On average, the amount of soil excavated by ants
to build a nest was 20 to 25 g. Aphaenogaster sp. D49 was identified a
s a significant contributor to soil turnover based on the frequency of
excavation, nest density and mass of soil removed to build the nest (
134 g). Aphaenogaster sp. D49 brought to the soil surface 465 g m-2 yr
-1 on grey sandy loam and 223 g m-2 yr-1 on yellow sand. The activity
period for the majority of ant nests was around 3 months, but some spe
cies such as Rhytidoponera spp. and Meranoplus spp. had nests active f
or up to 2 years. While other ant species such as Iridomyrmex sp. D13
have a high turnover of nests (<3 months). There was no clear seasonal
trend in the number of active nest openings, although they appeared t
o be greatest in May, and lowest in January. Ant nest density was high
er in yellow sand than in grey sandy loam, regardless of land use. Par
ticle size distribution of ant spoils (soil brought to the surface dur
ing nest construction) and ant-affected soil at 26 cm was compared to
the control soil at comparable depths, and found to be similar. Three
instances where the ant spoil had a higher proportion of clay-sized pa
rticles in comparison with the control soil, and this was attributed t
o ants excavating into the clay subsoil or being size-selective in the
material they excavated. The control soil had a texture-contrast betw
een 2 and 26 cm, while all the ant nests examined had similiar texture
between these two depths. This supports the hypothesis that ant activ
ity homogenizes the soil texture profile.