The Species Richness of Vascular Plants and Amphibia in Major Plant Communities in Temperate to Tropical Australia: Relationship with Annual Biomass Production
Table 1
Number of species of Amphibia in plant formations in south-eastern Australia, South Australia, south-western Australia, and Northern Territory. The Foliage Projective Covers of the combined overstorey and understorey strata in each plant community determine the Evaporative Coefficient ()—the ratio of actual to potential evapotranspiration per mm water available per month, a constant throughout the year, throughout the life cycle of the plant community, and between microhabitats in the same climatic area [5, 16, 26, 27, 40]. The annual shoot growth (dry weight per unit area of land) of each plant community has been estimated for each plant community [11], adjusted for soil nutrient status [16, 36].
Plant formation
Locality
Mean annual temperature (°C)
Annual precipitation (mm) (runoff†)
Evaporative coefficient () (per mm H2O)
Overstorey & understorey spp. per hectare
Annual shoot growth (t )
Vegetation survey
Amphibia (no. of spp. per plant formation)
Amphibian survey
South-eastern Australia (medium-nutrient soils*—clayey podsols, etc.)
*Relative to plant formations on medium-nutrient soils (Figure 4), annual shoot growth (dry weight measured in t ) in major plant formations on nutrient-poor soils is about 60 less, 50% less on extremely nutrient-poor soils, and 130 more on nutrient-rich soils [16, 36]. †Annual stream flows from the major drainage basins in Australia have been collated by the Australian Water Resources Council [92]. These estimates of runoff from the landscape show an exponential relationship to annual precipitation [16]. Runoff/Precipitation = (, ). Minimal runoff occurs from the deep lateritic earths of northern Australia (see the hydrological survey of the Weipa area in North Queensland, reported by Specht et al. in [93]).