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1

McMinn, Andrew. "Quaternary Coastal Evolution and Vegetation History of Northern New South Wales, Australia, Based on Dinoflagellates and Pollen." Quaternary Research 38, no. 3 (November 1992): 347–58. http://dx.doi.org/10.1016/0033-5894(92)90043-i.

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AbstractThe Richmond River Valley of northern N.S.W. contains a late Pleistocene succession dating back to approximately 250,000 yr B.P. Dinoflagellate and spore-pollen assemblages from the lowest interval, the lower “Dungarubba Clay” of Drury (1982), indicate deposition in a restricted estuarine environment at approximately 250,000 yr. Deposition in the overlying interval, the upper “Dungarubba Clay” and “Gundurimba Clay”, at approximately 120,000 yr B.P., began in a restricted estuary, but rising sea level caused inundation and deposition in a more open, marine-dominated environment. Dinoflagellate cyst assemblages from the last interglaciation (stage 5) are interpreted by analogy with those from the morphologically similar, modern Broken Bay, N.S.W. They are indicative of an open, marine-dominated environment and imply that barrier formation in the Richmond River Valley, and possibly elsewhere in northern N.S.W., did not commence until after the initial postglacial transgression. Synchronous changes in sea level and rainforest development suggest that there was no significant time lag between climate and sea-level change.
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2

Teakle, DS, S. Hicks, M. Karan, JB Hacker, RS Greber, and JF Donaldson. "Host range and geographic distribution of pangola stunt virus and its planthopper vectors in Australia." Australian Journal of Agricultural Research 42, no. 5 (1991): 819. http://dx.doi.org/10.1071/ar9910819.

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Natural hosts of pangola stunt virus (PaSV) in eastern Austalia were found to be Digitaria eriantha ssp. pentzii (pangola grass), D. ciliaris (summer grass) and D. milanjiana. Transmission tests using the planthopper vector, Sogatella kolophon, showed that D. polevansii, D. eriantha ssp. eriantha, D. swazilandensis and the Australian native, D. divaricatissima were also susceptible, whereas D. didactyla was not infected. In tests of 22 species in 15 other genera, only Urochloa panicoides (annual urochloa grass) was infected. In field surveys, PaSV was commonly found in pangola grass in near-coastal districts from Grafton, N.S.W. to Walkamin, N. Qld and was detected up to 100 km inland at Toowoomba. The virus was not detected in either pangola grass or D. eriantha ssp. eriantha in subhumid areas west of Toowoomba or at Gayndah. Sogatella kolophon was collected from Bamaga, N. Qld to Murwillumbah, N.S.W. It was commonly associated with both PaSV-infected and PaSV-free digitgrass pastures. It is concluded that PaSV poses a threat to many digitgrasses in near-coastal districts of Qld and subtropical N.S.W., but so far is unknown in inland Australia.
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3

Lambert, D. "GRAFFITI REMOVAL ON ROCK ART.SITES, N.S.W." AICCM Bulletin 14, no. 1-2 (January 1988): 9–12. http://dx.doi.org/10.1179/bac.1988.14.1-2.003.

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4

Holden, E. A. "Anthropological Society of N.S.W.: Financial Position." Mankind 3, no. 10 (February 10, 2009): 312. http://dx.doi.org/10.1111/j.1835-9310.1947.tb00129.x.

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5

Holden, E. A. "Anthropological Society of N.S.W.: Financial Position." Mankind 4, no. 3 (February 10, 2009): 126. http://dx.doi.org/10.1111/j.1835-9310.1949.tb00223.x.

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6

Brereton, Beatrice Le Gay, and Jennifer Sattler. "A Spastic Centre of N.S.W. Publication." Australian Occupational Therapy Journal 14, no. 3 (August 27, 2010): 41. http://dx.doi.org/10.1111/j.1440-1630.1967.tb00208.x.

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7

Freedman, L. "Human skeletal remains from Mossgiel, N.S.W." Archaeology in Oceania 20, no. 1 (April 1985): 21–31. http://dx.doi.org/10.1002/j.1834-4453.1985.tb00097.x.

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8

McCarthy, F. D. "A Rock Shelter near Emu Plains, N.S.W." Mankind 1, no. 10 (February 10, 2009): 240–41. http://dx.doi.org/10.1111/j.1835-9310.1934.tb00050.x.

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9

McMinn, Andrew. "Palynostratigraphy of the Stroud-Gloucester Trough, N.S.W." Alcheringa: An Australasian Journal of Palaeontology 11, no. 2 (January 1987): 151–64. http://dx.doi.org/10.1080/03115518708618986.

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10

Ryan, Michael. "Drug use in N.S.W. institutions — Innovation for inertia." Australia and New Zealand Journal of Developmental Disabilities 17, no. 2 (January 1991): 177–81. http://dx.doi.org/10.1080/07263869100034391.

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11

Elliott, GL, and GJ Holman. "Sodium accession in rainfall near Scone Mountain, N.S.W." Soil Research 23, no. 2 (1985): 315. http://dx.doi.org/10.1071/sr9850315.

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Contemporary sodium accessions in rainfall occurring near Scone Mountain were estimated to be 6.9 � 1.8 kg ha-1 year-1. The ratios of Ca/Na, Mg/Na and K/Na were consistent with the addition of soluble material to rain by aeolian processes, and the estimation of cyclic salt accessions could not be attempted.
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12

Barraclough, D. A. "FIELD OBSERVATIONS OFSENOSTOMASPP. (DIPTERA: TACHINIDAE) AT KATOOMBA, N.S.W." Australian Journal of Entomology 29, no. 3 (August 1990): 247–52. http://dx.doi.org/10.1111/j.1440-6055.1990.tb00355.x.

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13

Hodgson, AS, JF Holland, and EF Rogers. "Iron deficiency depresses growth of furrow irrigated soybean and pigeon pea on vertisols of northern N.S.W." Australian Journal of Agricultural Research 43, no. 3 (1992): 635. http://dx.doi.org/10.1071/ar9920635.

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Crops under furrow irrigation or after heavy rainfall on the alkaline, calcareous Vertisols of northern N.S.W. frequently exhibit chlorosis of young leaves after the soil is wetted, but the specific cause has not been identified previously. The quantitative effects of the syndrome on growth, physiological activity and yield are also unknown. Experiments on soybean and pigeon pea grown on a Vertisol at Breeza, N.S.W., Australia, examined the influence of applying Fe to the leaves, and Fe, Zn, N+P and lime to the soil before sowing, on leaf colour, leaf photosynthesis, crop dry matter, and yield of grain of soybean and dry matter and yield of pigeon pea. In soybean, chelated Fe applied to the soil before sowing increased the levels of active Fe (Fe2+) in leaves by up to 42% and dry matter of shoots by up to 46% early in the season. Active Fe and dry matter of shoots were linearly correlated (r2 = 0.76). Soil Fe treatments did not affect leaf photosynthesis, although addition of chelated Fe to the soil resulted in greener leaves than in the control. Foliar Fe had no significant effect on active Fe, leaf colour, or leaf photosynthesis. The 9% increase in grain yield in response to application of 20 kg Fe ha-1 to the soil was not significant. In pigeon pea, application of 20 kg Fe ha-1 to the soil increased dry matter by 140% and grain yield by 414%. Effects of lime and zinc were not significant, but N+P increased yield by 112%. The study showed that Fe deficiency is limiting the growth and/or yield of irrigated soybean and pigeon pea on the clay soils of northern N.S.W., and pointed to lime-induced iron chlorosis as a possible mechanism of damage.
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14

Kinnell, PI. "Rainfall energy in eastern Australia - Intensity kinetic energy relationships for Canberra, ACT." Soil Research 25, no. 4 (1987): 547. http://dx.doi.org/10.1071/sr9870547.

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Rainfall kinetic energy values measured with a Joss-Waldvogel rainfall distrometer near Canberra are reported and compared with other data obtained in Australia using the same measurement technique. Intensity-energy relationships for Canberra are similar to those previously obtained at Gunnedah, N.S.W. and should apply over a wide area of south-eastern Australia.
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15

McFarland, DC. "Flowering Biology and Phenology of Banksia integrifolia and B. spinulosa (Proteaceae) in New England National Park, N.S.W." Australian Journal of Botany 33, no. 6 (1985): 705. http://dx.doi.org/10.1071/bt9850705.

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The flowering biology and phenology of two species of Banksia, including anthesis rates, inflorescence survivorship and nectar production, were examined in the Northern Tablelands, N.S.W. Rainfall, temperature and wind are all important factors in determining nectar productivity and availability. The species investigated here are compared with other banksias studied elsewhere in Australia.
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16

Osborne, R. A. L. "A new history of cave development at Bungonia, N.S.W." Australian Geographer 24, no. 1 (May 1993): 62–74. http://dx.doi.org/10.1080/00049189308703078.

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17

Beck, P. H., and I. R. Qureshi. "Gravity Mapping of a Subsurface Cavity at Marulan, N.S.W." Exploration Geophysics 20, no. 4 (September 1989): 481–86. http://dx.doi.org/10.1071/eg989481.

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18

Kennedy, Elizabeth. "EXCAVATING A ROCK-SHELTER AT BROWN'S BAY, PITTWATER, N.S.W." Mankind 1, no. 8 (February 10, 2009): 200–201. http://dx.doi.org/10.1111/j.1835-9310.1934.tb00039.x.

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19

Dow, Edmund B. "Rock Carvings and Ceremonial Mounds, Noonthorungee Ranges, Koonawarra, N.S.W." Mankind 2, no. 7 (February 10, 2009): 210–16. http://dx.doi.org/10.1111/j.1835-9310.1939.tb00965.x.

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20

Austin, E. L. "Annual Report of the Anthropological Society of N.S.W., 1948." Mankind 4, no. 2 (February 10, 2009): 69–74. http://dx.doi.org/10.1111/j.1835-9310.1949.tb00216.x.

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21

McA. Powell, C., and M. J. Rickard. "Significance of the early foliation at Bermagui, N.S.W., Australia." Journal of Structural Geology 7, no. 3-4 (January 1985): 385–400. http://dx.doi.org/10.1016/0191-8141(85)90043-4.

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22

Ryan, P. J. "Soil formation on the Wallagaraugh Adamellite, southeastern N.S.W., Australia." CATENA 20, no. 6 (December 1993): 543–61. http://dx.doi.org/10.1016/0341-8162(93)90016-i.

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23

Wake, B. A., and G. R. Taylor. "Major's Creek, N.S.W., Australia — A Devonian epithermal gold deposit." Mineralium Deposita 23, no. 4 (October 1988): 239–46. http://dx.doi.org/10.1007/bf00206401.

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24

Davies, L. "An economic study of the Western Division of N.S.W." Rangeland Journal 7, no. 1 (1985): 32. http://dx.doi.org/10.1071/rj9850032.

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The Hassall Report was based on an economic survey of 150 landholders throughout the Western Division of New South Wales for the financial years 197711978, 197811979 and 1979/1980. The survey used taxation records, however. some attitudinal informa- tion was collected from face to face interviews with landholders. The survey examined the financial performance in relation to the carrying capacity of the property and in relation to five land- scape categories. The survey found that the financial performance of the landscape categorized as "tall dense woodlands with scrub" was significantly poorer than for other landscape categories. The report has been used as a major reference for the recently completed Joint Parliamentary Committee Enquiry into the Western Division of New South Wales and has influenced a number of the economic recommendations in this report. This paper gives a brief summary of the financial results, a comparison of these results to those of other agricultural areas and the major policy recom- mendations made in the report.
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25

Leven, J. H., P. G. Stuart-Smith, R. J. Musgrave, M. J. Rickard, and K. A. W. Crook. "A geophysical transect across the Tumut Synclinorial Zone, N.S.W." Tectonophysics 214, no. 1-4 (November 1992): 239–48. http://dx.doi.org/10.1016/0040-1951(92)90199-g.

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26

Carthew, SM, DJ Ayre, and RJ Whelan. "High-Levels of Outcrossing in Populations of Banksia spinulosa R.Br. and Banksia paludosa Smith." Australian Journal of Botany 36, no. 2 (1988): 217. http://dx.doi.org/10.1071/bt9880217.

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Rates of outcrossing were measured for two species of Banksia at Barren Grounds Nature Reserve, near Robertson, N.S.W. For B. spinulosa in a woodland area, both single-locus and multi-locus estimates of outcrossing approached the levels predicted for panmixia. A single-locus estimate for B. paludosa cohabiting the same site and a nearby heathland site gave similarly high estimates of outcrossing.
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27

Hochman, Z., DC Edmeades, and E. White. "Changes in effective cation exchange capacity and exchangeable aluminum with soil pH in lime-amended field soils." Soil Research 30, no. 2 (1992): 177. http://dx.doi.org/10.1071/sr9920177.

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Eleven acidic soils from northern N.S.W., having a wide range of values for ECEC, A1 and soil organic carbon (%C), were treated in the field with five rates of lime. The relationships between soil pH and the effective cation exchange capacity (ECEC), and between pH and exchangeable aluminium (Al), were investigated for the top 10 cm of these soils. Increases in the total exchangeable cations (TEC) calculated as ECEC-Al, were shown to be madelup almost entirely by increases in exchangeable calcium. There were no consistent changes in the amount of exchangeable magnesium, potassium or sodium due to liming these acidic soils. Formulae used to predict changes in A1 and ECEC with pH in the 'Lime-it' model were tested and modified on the 11 soils from northern N.S.W. A strong linear relationship was observed in each soil between Al and pH (transformed to hydrogen ion concentration x 103). The slope of this relationship (SALs) can be predicted from the pH and A1 values of unlimed soils. Strong linear relationships were also observed between pH and TEC, for each of the 11 soils. The SL, (the slope of the linear relationship TEC/pH for any soil 's') was shown by multiple regression analysis to be a function of TECi/pHi (where TECi is the sum of exchangeable cations of unlimed soil 's'; and pHi is the pH value of unlimed soil 's'), %C of the unlimed soil, and SALs. By using the measured values of pH, ECEC, Al and %C of unlimed soils, the values of Al, and TEB can be predicted for any pH value that may be measured (or predicted) after liming. The predictive relationships developed on N.S.W. soils were tested against independent data from New Zealand. The results confirmed the Al/pH predictions (R2 = 0.955), while the TEC/pH predictions were less well matched (R2= 0.62) possibly due to unusual clay mineralogy or organic matter fractions of 3 of the 18 soils tested.
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28

Austin, AD, and PC Dangerfield. "Synopsis of Australasian Microgastrinae (Hymenoptera : Braconidae), with a key to genera and description of new taxa." Invertebrate Systematics 6, no. 1 (1992): 1. http://dx.doi.org/10.1071/it9920001.

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The genera of microgastrine braconid wasps present in the Australasian region (defined as Australia, New Zealand, New Caledonia, New Guinea, Solomon Is, Fiji Is, Samoan Is, Cook Is, but not French Polynesia) are reviewed. An illustrated key to genera, comments on their taxonomy, and information on the distribution and host relationships of species are provided. Following examination of holotypes, the generic placement of all species recorded from the region is reassessed since a recent generic reclassification of the subfamily left most of the Australasian species incorrectly placed. Parapanteles Ashmead (N.T.), Fornicia Brullé (Qld) and Deuterixys Mason (Qld) are recorded from Australasia for the first time, while Buluka De Seager, Parenion Nixon, Snellenius Westwood and Wilkinsonellus Mason, previously known from Australasia, are recorded from mainland Australia for the first time. The genus Austrocotesia is described as new [with A. exigua, sp. nov. (Papua New Guinea) as the type species], along with the following 14 species: Austrocotesia delicata, sp. nov. (Papua New Guinea, Qld), A. paradoxa, sp. nov. (Papua New Guinea), Buluka collessi, sp. nov. (Qld), Deuterixys anica, sp. nov. (Vic., N.S. W., Qld), Fornicia commoni, sp. nov. (Qld), Glyptapanteles deliasa, sp. nov. (S.A.), Microgaster nixoni, sp. nov. (Tas., N.S.W.), Parapanteles masoni, sp. nov. (N.T.), Parenion beelaronga, sp. nov. (Qld), P. bootha, sp. nov. (Qld), Sathon albicoxa, sp. nov. (Tas., Vic., N.S.W.), S. naryciae, sp. nov. (Vic.), Wilkinsonellus amplus, sp. nov. (Qld, N.T.) and W. tomi, sp. nov. (Papua New Guinea, New Britain, Qld). Glyptapanteles guyanensis (Cameron), comb. nov. is excluded from the Australasian fauna; the name Glyptapanteles fullawayi, nom. nov. (Samoa) is proposed for Apanteles opercuiinae var. polita Fullaway; lectotypes are designated for Cotesia deliadis (Bingham), comb. nov. (Qld), C. philoeampa (Cameron), comb. nov. (N.S.W) and C. rufiventris (Bingham), comb. nov. (Qld); Glyptapanteles operculinae (Fullaway), comb. nov. (Samoa), Microgaster kuchingensis Wilkinson (Papua New Guinea) and Sathon moratus (Wilkinson), comb. nov. (Vic., S.A., W.A.) are redescribed; and 41 additional new combinations are proposed.
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29

Sharp, I. H., and M. A. Schell. "Study of Recreational Use of Sydney Water Board and Fish River Water Supply Storages (Australia)." Water Science and Technology 21, no. 2 (February 1, 1989): 119–22. http://dx.doi.org/10.2166/wst.1989.0037.

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Existing and potential recreational uses in a number of very different water supply catchments managed by two major N.S.W. authorities were investigated. Community attitudes to recreational use of both land based and water based activities were analysed together with reactions to increased charges to cover costs of ensuring safe water quality. Threats to water quality were studied and additional management and water quality control measures formulated.
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30

Lewis, F., and L. Bishop. "Tylos australis: a new species of Tylidae (Isopoda : Oniscidea) a family previously not recorded in Australia." Invertebrate Systematics 3, no. 6 (1989): 747. http://dx.doi.org/10.1071/it9890747.

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The Tylidae Milne-Edwards, 1840 is the sole family in the infra-order Tylomorpha Vandel, 1943 (Holdich et al. 1983) and is divided into two genera, Tylos Latreille, 1826, and Helleria Ebner, 1868 (Vandel 1960). Specimens collected from Bawley Point, N.S.W. belong to the genus Tylos. They are described as a new species, Tylos australis. The significance of the shapes of frontal processes in Tylos is discussed in terms of zoogeography.
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31

Blumenthal, CS, F. Bekes, IL Batey, CW Wrigley, HJ Moss, DJ Mares, and EWR Barlow. "Interpretation of grain quality results from wheat variety trials with reference to high temperature stress." Australian Journal of Agricultural Research 42, no. 3 (1991): 325. http://dx.doi.org/10.1071/ar9910325.

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Grain quality results for variety trials extending over 27 years (3 sites and 5 varieties) were compared with the temperature profiles during the grain filling period (56 days prior to harvest) to determine the effects on quality of high temperatures (>35�C) during this period of growth. Heat stress episodes have been frequent at two (Narrabri, N.S.W., and Turretfield, S.A.) of the three sites studied; spring temperatures were more moderate at the third site, Wongan Hills, W.A. There were highly significant (P< 0.01) correlations of heat stress (as hours above 35�C, during grain filling) with protein content (positive) and with grain yields (negative) at Narrabri for all varieties. In many combinations of site and variety, heat stress correlated negatively with loaf volume, and with dough strength (as Rmax, resistance to stretching with the Extensograph). Heat stress episodes in the Narrabri (N.S.W.) region in 1981 and 1982 gave further opportunity to examine these relationships. Results showed very clearly that high temperatures late in grain filling were associated with weaker dough properties (lower Rmax) in the resulting grain. These trends may form the basis of a predictive system by which to estimate crop quality and to interpret the results of variety trials.
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32

Uddin, MN, FW Ellison, L. O'Brien, and BDH Latter. "Heterosis in F1 hybrids derived from crosses of adapted Australian wheats." Australian Journal of Agricultural Research 43, no. 5 (1992): 907. http://dx.doi.org/10.1071/ar9920907.

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Data on the level of heterosis for grain yield under Australian dryland wheat growing conditions is essential before any decision can be made to commit resources to hybrid wheat breeding. Experiments were conducted at Narrabri, N.S.W., to determine the level and stability of heterosis for grain yield expressed by F1 hybrids derived from crosses of adapted Australian varieties. The hybrids and their parents were grown in hill plots in replicated experiments at three sowing times for two years (six environments). The hybrids outyielded their parents in each of the six environments with levels of mid- and high-parent heterosis up to 31.5 and 26.8%, respectively. The best hybrid outperformed the best check variety by an average yield margin of 18.2%. The hybrids were marginally but not significantly more stable in their yield performance across environments than their parents. While heterosis for grain protein content was generally negative, some hybrids were superior to the check varieties for both grain yield and protein content. Yield component analysis revealed no consistent pattern by which the best hybrids obtained their yield advantage over their parents. The levels of heterosis and the absolute yield advantage displayed by the hybrids over the best pure line check varieties were sufficient to sustain the commercial production of hybrid wheats in northern N.S.W.
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33

Enright, W. J. "Notes on the Aborigines of the North Coast of N.S.W." Mankind 2, no. 7 (February 10, 2009): 193–95. http://dx.doi.org/10.1111/j.1835-9310.1939.tb00962.x.

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Enright, W. J. "Notes on the Aborigines of the North Coast of N.S.W." Mankind 2, no. 9 (February 10, 2009): 321–24. http://dx.doi.org/10.1111/j.1835-9310.1940.tb00976.x.

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35

Thomas, H. F. "A Possible Aboriginal Ceremonial Ground at Lake Gol Gol, N.S.W." Mankind 6, no. 3 (May 10, 2010): 105–20. http://dx.doi.org/10.1111/j.1835-9310.1964.tb01362.x.

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36

Martin, Eric J., and Howard Tanner. "HISTORIC ARCHITECTURE OF H.M.A. NAVAL DOCKYARD, GARDEN ISLAND N.S.W. AUSTRALIA." Mariner's Mirror 74, no. 4 (January 1988): 363–90. http://dx.doi.org/10.1080/00253359.1988.10656220.

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37

PROSSER, IAN. "Fire, Humans and Denudation at Wangrah Creek, Southern Tablelands, N.S.W." Australian Geographical Studies 28, no. 1 (April 1990): 77–95. http://dx.doi.org/10.1111/j.1467-8470.1990.tb00623.x.

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38

McCaskill, Malcolm R., and Graeme J. Blair. "Medium-term climatic variation of the northern tablelands of N.S.W." Mathematics and Computers in Simulation 30, no. 1-2 (February 1988): 159–64. http://dx.doi.org/10.1016/0378-4754(88)90119-x.

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39

Cahill, Rowan, and John O'Brien. "A Divided Unity! Politics of N.S.W. teacher militancy since 1945." Labour History, no. 56 (1989): 103. http://dx.doi.org/10.2307/27508943.

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40

Rich, I. H. V., T. F. Flannery, and M. Archer. "A second Cretaceous mammalian specimen from Lightning Ridge, N.S.W., Australia." Alcheringa: An Australasian Journal of Palaeontology 13, no. 2 (January 1989): 85–88. http://dx.doi.org/10.1080/03115518908619043.

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41

Crouch, R. J., J. W. McGarity, and R. R. Storrier. "Tunnel formation processes in the Riverina area of N.S.W., Australia." Earth Surface Processes and Landforms 11, no. 2 (March 1986): 157–68. http://dx.doi.org/10.1002/esp.3290110206.

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42

Tindale, MD. "Taxonomic notes on three Australian and Norfolk Island species of Glycine Willd. (Fabaceae: Phaseolae) including the choice of a Neotype for G.clandestina Wendl." Brunonia 9, no. 2 (1986): 179. http://dx.doi.org/10.1071/bru9860179.

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Explanations are made for the choice of a neotype from Kurnell, Botany Bay, N.S.W., Australia. A new combination is made for G. microphylla from Australia (Queensland, New South Wales, Victoria, South Australia and Tasmania) and Norfolk Island. A new species, G. arenaria, is described from the East Kimberley District of Western Australia, and the Northern Territory. The three species are illustrated in detail. Keys are provided to distinguish these taxa from their allies.
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43

Humphreys, GS, PA Hunt, and R. Buchanan. "Wood ash stone near Sydney, NSW - a carbonate pedologial feature in an acidic soil." Soil Research 25, no. 2 (1987): 115. http://dx.doi.org/10.1071/sr9870115.

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Wood-ash stone, composed mainly of calcite (XRD, XRF, EMS and petrological determination), has been found within the remains of a large, standing and mostly burnt tree (Angophora costata) near Sydney, N.S.W. This may be the first recorded occurrence of wood-ash stone in Australia and outside North America. Slow burning of standing trees is proposed as a mechanism for producing carbonate features in nutrient poor and acidic soil parent materials such as the quartzose Hawkesbury Sandstone.
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44

Bernard, A. G. "Factors Influencing the Bacteriological Quality of Spa-Pool Waters in New South Wales (Australia)." Water Science and Technology 21, no. 2 (February 1, 1989): 141–45. http://dx.doi.org/10.2166/wst.1989.0041.

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The increasing popularity in the use of spa pools during the 1970's and 1980's and the accompanying incidents of folliculitis and ear infections caused by Pseudomonas aeruginosa associated with spa-pool use has necessitated the development of bacteriological and chemical guidelines for spa-pool water quality. The New South Wales (N.S.W.) Department of Health introduced a bacteriological standard for swimming pools and spa-pools in 1981 based on the findings of a series of surveys aimed at identifying the principal factors influencing the bacteriological quality of spa waters. Four surveys are summarised in this paper. The major findings described are the tenfold higher recovery of P. aeruginosa from spa-pools than from outdoor pools; the need for at least 2.0 milligrams per litre (mg/L) free chlorine residual in order to achieve reliable satisfactory water quality in spas compared with a requirement of 1.0mg/L to achieve the same quality in outdoor pools; the need to maintain pH below 8.0 in order to ensure efficient chlorine disinfection; the apparent inability of bromochlorodimethylhydantoin to adequately disinfect spas during heavy bather load periods; and the success of the Health Department's spa-pool operator education program which resulted in a 30% reduction in the incidence of bacteriologically unsatisfactory spa-pool waters in N.S.W. between 1980 and 1986.
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45

Eby, P. "Seasonal movements of grey-headed flying-foxes, Pteropus poliocephalus (Chiroptera : Pteropodidae), from two maternity camps in northern New South Wales." Wildlife Research 18, no. 5 (1991): 547. http://dx.doi.org/10.1071/wr9910547.

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Seasonal movements of 22 Pteropus poliocephalus, from two maternity camps in north-eastern New South Wales, were monitored from January to June 1989 using radiotelemetry. The animals moved independently in time and space among various communal roosts located 8-610 km from the maternity camp sites. Generally, P. poliocephalus from a camp near rainforest (Currie Park, Lismore) remained within 50 km of the maternity site. These localised movements were attributed to the continued availability of fruits in the rainforest throughout the study. Animals from a maternity camp surrounded by sclerophyll forest (Susan I., Grafton) undertook long migrations south (median distance 342.5 km, n = 11) to camps containing up to 200 000 P. poliocephalus of both sexes. These large aggregations formed during the mating season and comprised individuals drawn from various previous sites. Thus, P. poliocephalus in northern and central N.S.W. appear to function as a single breeding population and should be managed as such. After mid-May, animals from Susan I. returned to north-eastern N.S.W. There was high correlation between movements of P. poliocephalus from the camp at Susan I. and the flowering patterns of certain species of Myrtaceae and Proteaceae. It is hypothesised that flowering attractive to apiarists is also attractive to P. poliocephalus and that information from apiarists could be used by wildlife managers to predict large aggregations of the animals.
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46

Lackie, M. A. "The magnetic fabric of the Late Permian Dundee Ignimbrite, Dundee, N.S.W." Exploration Geophysics 19, no. 4 (September 1988): 481–88. http://dx.doi.org/10.1071/eg988481.

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47

Johanson, Zerina. "New antiarchs (Placodermi) from the Hunter Siltstone (Famennian) near Grenfell, N.S.W." Alcheringa: An Australasian Journal of Palaeontology 21, no. 3 (January 1997): 191–217. http://dx.doi.org/10.1080/03115519708619173.

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48

Paver, Kenneth. "THE EARLY HISTORY OF THE SKIN & CANCER FOUNDATION OF N.S.W." Australasian Journal of Dermatology 32, no. 3 (December 1991): 121–23. http://dx.doi.org/10.1111/j.1440-0960.1991.tb01772.x.

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49

Jack, R. J. B. "Preliminary Examination, Institute of Optometrists of N.S.W., set 6th September, 1920." Australasian Journal of Optometry 2, no. 12 (March 25, 2010): 3–6. http://dx.doi.org/10.1111/j.1444-0938.1921.tb00200.x.

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50

Crouch, R. J., and T. Novruzi. "Threshold conditions for rill initiation on a vertisol, Gunnedah, N.S.W., Australia." CATENA 16, no. 1 (February 1989): 101–10. http://dx.doi.org/10.1016/0341-8162(89)90007-6.

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