The appropriation of an Aboriginal landscape in northern New South Wales

The attachment of Australian Aboriginal people to land has not only been amply documented by anthropologists since the late 19^th century, it is also one of their own enduring tropes of differentiation from non‐Aboriginal and “official” Australian state society. In the face of widespread and concerted alteration of the pre‐settlement landscape engendered by industrial and commercial development, Aboriginal people seek to reclaim or reappropriate remnants of a pristine environment untransformed by modern development. Alteration of the landscape, as far as Aboriginal people are concerned, also goes hand in hand with the progressive decimation of Aboriginal populations in the 19^th and early 20^th centuries through violence and disease. Contemporary Aboriginal communities seek to protect the sites of violent death, believed heavily populated with the frustrated spirits of the deceased, from disturbance, particularly by non‐Aboriginal people. In this chapter I discuss some of the anthropological implications of seeing landscape as a terrain of intercultural conjunction in such a bifold society in northern New South Wales, and what levels of transformation are and are not acknowledged by a marginal, minority indigenous population seeking to insulate their historical landscape from development.     

The ecology of the Australian gecko Heteronotia binoei in northern New South Wales

A two year study was carried out on Heteronotia binoei (Gray) in the Pilliga Scrub by means of visits of six days' duration in each month of the year. Animals were individually marked by toe-clipping and a mark-recapture programme was carried out throughout the study.
In the Pilliga Scrub Heteronotia lives below bark or boards on the ground or below the bark at the base of dead trees or stumps.
The mark-recapture programme provided extensive data on the population, its movements, growth, tail loss and regeneration. Samples were collected for analysis of intestinal contents. The above data together with observations of behaviour provided a well corroborated picture of the biology of this small gekkonid lizard.     

Occurrence of the mayfly family Teloganodidae in northern New South Wales

Teloganodid mayfly nymphs, previously known in Australia only from south-eastern Queensland, have now been recorded from numerous localities in the coastal drainages of northern New South Wales (NSW) from the Barrington Tops district to the Richmond River system. The nymphs seem to be restricted to riffles in forest streams and occur over a wide altitudinal range with records up to 940 m. They appear identical to those of Austremerella picta Riek, but rearing to the adult is needed to be certain that they represent the same species. The apparent restriction of Australian Teloganodidae to southern Queensland and northern NSW poses a biogeographical puzzle.     

New prosauropod material from South Wales

New prosauropod material from a cave filling of Upper Triassic/Lower Jurassic age in Pant-y-ffynnon Quarry, South Wales, is described. The Panl-y-ffynnon fauna also includes thecodont, coelurosaur, crocodile and lepidosaur material.
Most of the prosauropod skeleton is represented. An almost complete but disarticulated skull is preserved. The skull and whole skeleton of the prosauropod are reconstructed. Evidence from the size and relative proportions of the bones, also the state of ossification, indicates that the prosauropod remains represent juveniles.
The level of the jaw articulation combined with the form of the teeth would suggest that the Pant-y-ffynnon prosauropod was omnivorous.
The Pant-y-ffynnon prosauropod resembles closely the much less complete Durdham Down (Bristol) remains of Thecodonlosaurus antiquus Morris; the Welsh material could well be juveniles of that species. Here the Pant-y-ffynnon material is ascribed to Thecodonlosaurus sp.
The mode of deposition of the fossil material is discussed, to account for the deposit containing only juveniles of the prosauropod.     

The ecology of the Australian gecko, Gehyra variegata, in northern New South Wales

A two year study was carried out on Gehyra variegata (Dumeril & Bibron) in the Pilliga Scrub by means of visits of six days duration in each month of the year. Animals were individually marked by toe-clipping and a mark-recapture programme was carried out throughout the study.
This arboreal gecko lives below the bark of dead trees or stumps most commonly at a height of two to three feet from the ground.
The mark-recapture programme provided extensive data on the population, its movements, growth, tail loss and regeneration. Monthly samples were collected for intestinal analysis and for gonadal studies. These together with behavioural observations provided a well corroborated picture of the biology of this small gekkonid lizard.     

Mineralization of soil nitrogen in three forest communities from the New England region of New South Wales

Nitrogen (N) mineralization rates and the temperature response patterns of mineral N production in surface (0–7.6 cm) soils were compared in laboratory incubation studies based on disturbed, composite samples. Seasonal variation in the field levels of mineral N, and mineralization potential of intact (7.6 × 5.6 cm diameter) soil cores, were also investigated. Ammonification proceeded rapidly in each soil. Nitrification did not occur in grassy forest (GF) soil but was active in both layered forest (LF) and mossy forest (MF) soils, especially the former. Total mineral N production was greatest in MF and least in LF. Ammonification in disturbed samples was maximal at 50°C in all three soils with a secondary peak at 10°C in LF soil. Nitrification in LF and MF soils was most rapid at 25°C. Several species of ammonifying bacteria with different temperature optima were isolated, indicating that the process of ammonification is a composite of the activities of a variety of decomposer microbes. Mean field levels of mineral N and NH₄–N throughout the year were greatest in MF and least in LF. Seasonal fluctuations in NH₄–N were evident, concentrations being universally low in mid-winter (about 1.5 μgg^-1), increasing to a maximum in late summer (about 5 μg g^-1 in LF: 16–18 μg g^-1 in GF and MF). Field levels of NO₃–N were more constant and never more than 5 μg g^-1 in any community. Both total mineralization and ammonification in intact cores were greatest in MF and least in LF while nitrification was greatest in LF and almost negligible in GF, thus confirming the results obtained with disturbed samples. The potential for mineralization was large in mid-winter when the amount of mineral N was very low, and small in late summer when field levels were higher: this is interpreted as indicating that seasonal climatic factors regulate the availability of substrates for decomposers. Spatial variability in field levels of mineral N and mineral N production in the laboratory was evidenced by significant ‘sampling site’ effects in each community: however, at the sampling intensity used, the presence of bark mounds around Eucalyptus saligna trees could not be shown to affect these attributes. The inability of GF soil to nitrify when incubated in the laboratory could not be ascribed to a high C/N ratio, low pH, lack of substrate ammonium, or a low population of autotrophic nitrifying bacteria. No attempt was made to investigate the presence of allelopathic nitrification inhibitors. No evidence was obtained to support the view that nitrification is atypical of climax communities in situ. The most productive forest (LF) had the greatest capacity to nitrify and the least productive community (GF) the smallest capacity to do so.     

Evidence of Cryptosporidium transmission between cattle and humans in northern New South Wales

Cryptosporidium is an enteric parasite of public health significance that causes diarrhoeal illness through faecal oral contamination and via water. Zoonotic transmission is difficult to determine as most species of Cryptosporidium are morphologically identical and can only be differentiated by molecular means. Transmission dynamics of Cryptosporidium in rural populations were investigated through the collection of 196 faecal samples from diarrheic (scouring) calves on 20 farms and 63 faecal samples from humans on 14 of these farms. The overall prevalence of Cryptosporidium in cattle and humans by PCR and sequence analysis of the 18S rRNA was 73.5% (144/196) and 23.8% (15/63), respectively. Three species were identified in cattle; Cryptosporidium parvum, Cryptosporidium bovis and Cryptosporidium ryanae, and from humans, C. parvum and C. bovis. This is only the second report of C. bovis in humans. Subtype analysis at the gp60 locus identified C. parvum subtype IIaA18G3R1 as the most common subtype in calves. Of the seven human C. parvum isolates successfully subtyped, five were IIaA18G3R1, one was IIdA18G2 and one isolate had a mix of IIaA18G3R1 and IIdA19G2. These findings suggest that zoonotic transmission may have occurred but more studies involving extensive sampling of both calves and farm workers are needed for a better understanding of the sources of Cryptosporidium infections in humans from rural areas of Australia.     

Species-richness and soil phosphorus in plant communities in coastal New South Wales

Species-richness (recorded as number of species in 16 m² quadrats), in more than 60 coastal sites developed over various substrata, exhibited a significant non-linear relationship with soil total phosphorus extracted from associated soil samples. Although the general form of this relationship is not incompatible with a resource competition model, the significant proportion of the total variance accounted for by the species-richness/phosphorus relationship suggests that a more detailed examination of phosphorus use at a community level will be profitable.     

Molecular diversity of soil basidiomycete communities in northern-central New South Wales, Australia

Basidiomycete communities were profiled using terminal RFLP (TRFLP) and amplified ribosomal DNA restriction analysis (ARDRA) approaches at seven field sites under differing land use in northern-central New South Wales (NSW), Australia. TRFLP data indicated greater basidiomycete species richness at sites with natural vegetation. Sixty-seven basidiomycete ARDRA-types were detected. Various putatively ectomycorrhizal fungi were detected at all sites with native vegetation. Most ectomycorrhizal taxa had affinities to the genus Tomentella, while two Pisolithus taxa and putatively ectomycorrhizal Cantharellales taxa were also detected. Although soils under woodland or grassland communities supported a range of putatively saprotrophic taxa, only members of the Ceratobasidiales were detected in soils under agricultural land use. This study is the first investigation of fungal communities in soils of northern-central NSW, Australia.     

Inhibition of soil urease activity by aminocresols

Summary The effect on soil urease activity of five aminocresols, at concentrations of 5–100 g/g soil, was examined in the laboratory. Two compounds, 4-amino-o-cresol and 4-amino-m-cresol, significantly inhibited urease activity. The efficacy of 4-amino-o-cresol was compared with that of phenylphosphorodiamidate (PPDA), a known inhibitor, in three U.K. soils. At 50g/g soil 4-amino-o-cresol was as inhibitory as an equivalent concentration of PPDA in a soil with low urease activity, but was less inhibitory in two soils with high urease activity.     

Historical perspectives on some vegetation and soil changes in semi-arid New South Wales

The history of settlement of the semi-arid rangelands of western New South Wales is reviewed with respect to changes in the vegetation and soil which occurred under a regime of european land management. Simple dynamics of the vegetation response to grazing are illustrated and primary archival data is explored to verify the status of traditional wisdom about three examples of perceived change; the extent of the pioneers knowledge of land degradation, the timing and causes of nineteenth century Callitris pine regrowth events, and the importance of soil compaction. In each case it is shown that the traditional wisdom surrounding these issues is partly erroneous and that folklore is in danger of becoming accepted fact. Such errors must be avoided if we are to improve range dynamics models and management.     

A fossil Selaginella from the Permian of New South Wales

Selaginella harrisiana ap. nov. is described from the Permian (Kungurian) Upper Coal Measures at Victoria Pass, N.S.W. It resembles Selaginella selaginoides in its leafy parts but has a long leafless rhizome recalling Asteroxylon. The present evidence suggests that the herbaceous and arborescent ly copsids are taxonomically remote.     

Length-weight relationships for invertebrates from forests in south-eastern New South Wales

The relationship between length and weight was calculated for nine taxa of eucalypt forest and woodland invertebrates from south-eastern New South Wales. Length and weight were highly correlated. For the majority of taxa the relationship was best described by a power model. There were no significant differences between the length-weight regressions of Australian and North American taxa. This strengthens the value of generalized regressions for estimates of biomass from invertebrate length data in ecological studies.     

Stimulation by nickel of soil microbial urease activity and urease and hydrogenase activities in soybeans grown in a low-nickel soil

Summary The concentration of nickel in some soils may be insufficient to meet the requirements of enzymes such as urease in soybeans and hydrogenase in Rhizobium. In an initial evaluation of nickel availability, several soils were examined for nickel content and microbial urease activity. Total and extractable nickel were determined by atomic emission spectrometry. Purified glucose and urea were added to soils to stimulate microbial growth and urease activity, the latter of which was monitored by the rate of decomposition of¹⁴C urea. Nickel also was added to some samples to determine if the indigenous supply was limiting. In one low-nickel soil (total Ni 13 ppm) urease activity increased 150% in response to additional nickel, while other soils (total Ni 22–3491 ppm) failed to respond to nickel. However, additional nickel did stimulate urease activity (up to 109%) in 3 out of 10 soils to which purified CaCO₃ was added. Presumably the rise in pH associated with this treatment decreased nickel availability. Additions of Co, Mn, Fe, or Cu had no consistent effect on urease activity, thus indicating that the response to Ni was specific. Nickel fertilization increased leaf urease and nodule hydrogenase activity of soybeans grown in low-nickel soil, however, yield was not improved. These results may have practical implications in the nutrition of plants and micro-organisms that metabolize H₂ and urea.