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Artykuły w czasopismach na temat „Limnology Australia”

Autor: Grafiati

Data publikacji: 4 czerwca 2021

Data aktualizacji: 2 lutego 2022

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1

Den Hartog, C. "Limnology in Australia." Aquatic Botany 40, no. 4 (January 1991): 394–96. http://dx.doi.org/10.1016/0304-3770(91)90085-j.

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2

MACINTYRE, S. "Aquatic Studies: Limnology in Australia." Science 236, no. 4808 (June 19, 1987): 1579–81. http://dx.doi.org/10.1126/science.236.4808.1579-a.

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3

Khan, Tariq A. "Limnology of four saline lakes in western Victoria, Australia." Limnologica 33, no. 4 (December 2003): 316–26. http://dx.doi.org/10.1016/s0075-9511(03)80026-9.

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Khan, Tariq A. "Limnology of four saline lakes in western Victoria, Australia." Limnologica 33, no. 4 (December 2003): 327–39. http://dx.doi.org/10.1016/s0075-9511(03)80027-0.

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5

Benke, Arthur C. "Limnology in Australia. P. De Deckker , W. D. Williams." Journal of the North American Benthological Society 6, no. 4 (December 1987): 292–93. http://dx.doi.org/10.2307/1467320.

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6

Boulton, Andrew J. "Limnology and conservation of rivers in arid inland Australia." SIL Proceedings, 1922-2010 27, no. 2 (October 2000): 655–60. http://dx.doi.org/10.1080/03680770.1998.11901316.

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7

Timms, Brian V. "Limnology of the claypans of the Paroo, arid-zone Australia." SIL Proceedings, 1922-2010 28, no. 1 (February 2002): 130–33. http://dx.doi.org/10.1080/03680770.2001.11902560.

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8

Chang, Jie Christine, Craig Woodward, and James Shulmeister. "A snapshot of the limnology of eastern Australian water bodies spanning the tropics to Tasmania: the land-use, climate, limnology nexus." Marine and Freshwater Research 65, no. 10 (2014): 872. http://dx.doi.org/10.1071/mf13265.

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The present study investigates 45 natural and artificial water bodies extending across the whole of eastern Australia from the tropics to Tasmania. A broad variety of physio-chemical, land-use and climatic parameters were measured. Reservoirs and other artificial water bodies responded to stressors in their catchments in a similar fashion to natural lakes, but tended to be less nutrient rich, possibly because of shorter residence times and active management. Salinity and pH were strongly correlated in the dataset. Bedrock had a strong influence on pH in freshwater lakes, whereas all highly sal

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9

Burke, CM, and B. Knott. "Limnology of four groundwater-fed saline lakes in South-sestern Australia." Marine and Freshwater Research 40, no. 1 (1989): 55. http://dx.doi.org/10.1071/mf9890055.

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Salinity, temperature, dissolved oxygen (DO), pH and total alkalinity (TA) were measured in four saline lakes of Yalgorup National Park, Western Australia, primarily over an 18-month period, July 1985 to January 1987, but also during 1987 and in 1988. These lakes are shallow (<3 m) ground-water sinks with no surface drainage. Rainfall and hence ground-water inflow to the lakes was highly seasonal and occurred mainly between May and October. Lakes Hayward, North Newnham and South Newnham were consistently hypersaline (e.g. Hayward 61-214 g L-1) and Hayward and North Newnham were stratified f

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10

Timms, BV. "Reconnaissance limnology of some coastal dune lakes of Cape York Peninsula, Queensland." Marine and Freshwater Research 37, no. 2 (1986): 167. http://dx.doi.org/10.1071/mf9860167.

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All nine lakes studied are small (mean area 32 ha), shallow (< 5 m deep), watertable exposures in thin dunes overlying laterite or sandstone. Their water is fresh (mean salinity 52 mg I-1), acid (mean pH 4.8) and dominated by Na+ and Cl-, but with appreciable amounts of Ca2+, Mg2+ and HCO3-. Almost all macrophytes, littoral invertebrates, fish and limnetic zooplankters are common tropical species. A few species are shared with dune lakes in southern Australia and even fewer are endemic. Hence, these tropical dune lakes are different from those in temperate and subtropical eastern Australia.

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11

Hawkins, PR, LE Taplin, LJ Duivenvoorden, and F. Scott. "Limnology of oligotrophic dune lakes at Cape Flattery, North Queensland." Marine and Freshwater Research 39, no. 4 (1988): 535. http://dx.doi.org/10.1071/mf9880535.

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Physical, chemical and biotic attributes of 16 lakes and ponds in the siliceous dunefields of Cape Flattery, in the humid tropics of Australia, have been investigated. The dune lakes are similar to those of dunefields in south-eastern Queensland, with very low to low conductivity (62-338 �S cm-1), low pH (3.9-6.8), and low to high humic content (gilvin 0.0-31.0 g440 m-1). These lakes are apparently not perched above the local water table. The ionic compositions of all lakes were very similar, with NaCl predominating and with very low concentrations of Mg, Ca, K, and SO4. Bicarbonate was absent

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12

De Deckker, P., and W. D. Williams. "Physico-chemical limnology of eleven, mostly saline permanent lakes in western Victoria, Australia." Hydrobiologia 162, no. 3 (May 1988): 275–86. http://dx.doi.org/10.1007/bf00016673.

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13

Pearson, R. G. "Limnology in the northeastern tropics of Australia, the wettest part of the driest continent." SIL Communications, 1953-1996 24, no. 1 (January 1994): 155–63. http://dx.doi.org/10.1080/05384680.1994.11904033.

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14

Outridge, P. M., A. H. Arthington, and G. J. Miller. "Limnology of naturally acidic, oligotrophic dune lakes in subtropical Australia, including chlorophyll — phosphorus relationships." Hydrobiologia 179, no. 1 (July 1989): 39–51. http://dx.doi.org/10.1007/bf00011928.

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15

Mackey, AP. "Aspects of the limnology of Yeppen Yeppen Lagoon, central Queensland." Marine and Freshwater Research 42, no. 3 (1991): 309. http://dx.doi.org/10.1071/mf9910309.

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Aspects of the morphometry and physical and chemical limnology of Yeppen Yeppen Lagoon, in tropical Australia, have been investigated. The lagoon is a channel billabong lying in the old bed of the Fitzroy River. It has a relatively small, shallow and elongated basin. Seasonal variations in water temperature, light regime, oxygen concentration, pH and conductivity suggest that the lagoon exhibits a warm monomictic pattern of thermal stratification rather than a continuous warm polymictic one. The annual heat budget was 3294 calories cm-2 year-1. Maximum work of the wind was 238.8 g-cm cm-2, and

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16

Brown, T. E., A. W. Morley, and D. V. Koontz. "The limnology of a naturally acidic tropical water system in Australia II. Dry season characteristics." SIL Proceedings, 1922-2010 22, no. 4 (March 1985): 2131–35. http://dx.doi.org/10.1080/03680770.1983.11897636.

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17

Timms, Brian V. "Large freshwater lakes in arid Australia: A review of their limnology and threats to their future." Lakes and Reservoirs: Research and Management 6, no. 2 (June 2001): 183–96. http://dx.doi.org/10.1046/j.1440-1770.2001.00132.x.

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18

Morley, A. W., T. E. Brown, and D. V. Koontz. "The limnology of a naturally acidic tropical water system in Australia I. General description and wet season characteristics." SIL Proceedings, 1922-2010 22, no. 4 (March 1985): 2125–30. http://dx.doi.org/10.1080/03680770.1983.11897635.

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19

Savage, Alan, and Brenton Knott. "Artemia parthenogenetica in Lake Hayward, Western Australia. I. Interrupted recruitment into adult stages in response to seasonal limnology." International Journal of Salt Lake Research 7, no. 1 (March 1998): 1–12. http://dx.doi.org/10.1007/bf02449920.

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20

Geddes, MC. "The role of turbidity in the limnology of Lake Alexandrina, River Murray, South Australia; comparisons between clear and turbid phases." Marine and Freshwater Research 39, no. 2 (1988): 201. http://dx.doi.org/10.1071/mf9880201.

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In the first months of 1981, the characteristically highly turbid Lake Alexandrina cleared somewhat so that turbidity dropped from a previous mean value (1975-1978) of 93 NTU to 9 NTU, the Secchi transparency and euphotic depth increased from previous means of 19 cm and 0.8 m to 72 cm and 3.1 m, and the light extinction coefficient fell from 6.54 to 1.2 In units m-1. Low flows in the River Murray, especially low contributions from the Darling River, and high salinity appeared to be the major factors responsible for the clearing. During the clear phase, nutrient levels fell, the normal summer p

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21

Vanhoutte, Koenraad, Elie Verleyen, Cathy Kilroy, Koen Sabbe, Renaat Dasseville, and Wim Vyverman. "Catchment characteristics and chemical limnology of small lakes, tarns and mire pools in New Zealand (South Island) and Tasmania." Marine and Freshwater Research 57, no. 1 (2006): 83. http://dx.doi.org/10.1071/mf04276.

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Small alpine water bodies can play a large role in defining patterns of biological and landscape diversity, and may be particularly sensitive to climate change. A large limnological dataset, consisting of 65 and 6 water bodies, respectively, on South Island and Stewart Island (New Zealand) and 76 and 12 water bodies, respectively, in the Tasmanian highlands and coastal areas (Australia), was constructed to assess patterns of variation in alpine and subalpine lakes in the Australasian region. With the exception of the coastal systems, most lakes were very dilute. In general, lake water chemistr

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22

Knott, Brenton, Edyta J. Jasinska, and Kimberly D. Smith. "Limnology and aquatic fauna of EPP 173, Melaleuca Park, refuge for an outlier population of the Black-stripe minnow Galaxiella nigrostriata (Galaxiidae), in southwestern Australia." Records of the Western Australian Museum 21, no. 3 (2002): 291. http://dx.doi.org/10.18195/issn.0312-3162.21(3).2002.291-298.

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23

Brennen, C. E., G. Keady, and J. Imberger. "A note on algal population dynamics." IMA Journal of Applied Mathematics 83, no. 4 (July 25, 2018): 783–96. http://dx.doi.org/10.1093/imamat/hxy010.

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Abstract This is a contribution to the special issue honoring the late John R. Blake of the University of Birmingham. All three authors had the pleasure of extensive technical interactions with John Blake during his career in the UK, USA and Australia and benefited both professionally and personally from his friendship. John’s work in developing fundamental mathematical solutions for Stokes’ flows and his application of those mathematical tools to analyses of microorganism locomotion led to special new insights into the world of small-scale swimming. This special issue devoted to John’s memory

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24

Horn, W. "Limnology in Australia. Eds. P. de Dekker and W. D. Williams.-671 pp., figs., tabs. = Monographiae Biologicae Vol. 61. Series ed. H. J. Dumont. Dordrecht/Boston/Lancaster: 1986. ISBN 90-6193-578-4, and Melbourne: CSIRO 1986. ISBN 06-4304-028-5. Dfl. 250,—; $ A 80.00; US $ 115,—; £ 82.25." Internationale Revue der gesamten Hydrobiologie und Hydrographie 73, no. 1 (1988): 124–25. http://dx.doi.org/10.1002/iroh.19880730114.

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25

Timms, BV. "Limnology of Lake Buchanan, a tropical saline lake, and associated pools, of North Queensland." Marine and Freshwater Research 38, no. 6 (1987): 877. http://dx.doi.org/10.1071/mf9870877.

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During 1974-1984, Lake Buchanan and seven peripheral pools usually contained water for only a few months each year, commencing in late summer. They ranged in salinity from 1 to 202 g l-1, their waters were dominated by sodium chloride, but with Ca2+/Mg2+ ratios of c. 1, and were generally alkaline. The fauna of 53 species included three halobionts (e.g. Parartemia minuta, Diacypris compacts), 18 halophilics (e.g. Mytilocypris splendida, Trigonocypris globulosa, Microcyclops dengizicus) and many salt- tolerant freshwater forms, mainly insects. Overall, the fauna was distinctly Australian, but s

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26

Blanchette, Melanie L., and Mark A. Lund. "Aquatic Ecosystems of the Anthropocene: Limnology and Microbial Ecology of Mine Pit Lakes." Microorganisms 9, no. 6 (June 3, 2021): 1207. http://dx.doi.org/10.3390/microorganisms9061207.

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Mine pit lakes (‘pit lakes’) are new aquatic ecosystems of the Anthropocene. Potentially hundreds of meters deep, these lakes are prominent in the landscape and in the public consciousness. However, the ecology of pit lakes is underrepresented in the literature. The broad goal of this research was to determine the environmental drivers of pelagic microbe assemblages in Australian coal pit lakes. The overall experimental design was four lakes sampled three times, top and bottom, in 2019. Instrument chains were installed in lakes and measurements of in situ water quality and water samples for me

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27

Culver, DA, and MC Geddes. "Limnology of rearing ponds for Australian fish larvae: Relationships among water quality, phytoplankton, zooplankton, and the growth of larval fish." Marine and Freshwater Research 44, no. 4 (1993): 537. http://dx.doi.org/10.1071/mf9930537.

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Fertilization of earthen ponds used to rear the larvae of golden perch, Macquaria ambigua, and silver perch, Bidyanus bidyanus, resulted in phytoplankton blooms dominated by the cyanobacterium Anabaena possibly because of a low N:P ratio. There was a zooplankton succession of rotifers (mostly Brachionus), Moina, Boeckella and Mesocyclops, and then Daphnia. An increase in Daphnia correlated with a decline in Anabaena, suggesting grazing on that cyanobacterium. Golden perch larvae included copepods in their diet whereas silver perch did not, and this was reflected in lower Boeckella numbers in t

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28

Walsh, RGJ, RJ Shiel, and PA Tyler. "Reconnaissance limnology of Tasmania VIII. Tasmanian coastal lagoons - epicentres of endemism in the Australian aquatic microbiota." Papers and Proceedings of the Royal Society of Tasmania, 2004, 67–76. http://dx.doi.org/10.26749/rstpp.138.67.

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29

Thai, Tran Thanh, and Ngo Xuan Quang. "The Seasonal Variability in The Genus-Family Structure of Free-Living Nematode Communities in Organic Shrimp Farming Ponds, Ca Mau Province." VNU Journal of Science: Natural Sciences and Technology, March 27, 2019. http://dx.doi.org/10.25073/2588-1140/vnunst.4864.

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This study determined the seasonal variability of free-living nematode communities structure (genus/family level) in organic shrimp farms ponds in Tam Giang commune, Nam Can district, Ca Mau province. Based on the result of SIMPER analysis, the average similarity in nematode communities at genus level was low with 30.75% and 30.81% (in dry and rainy season, respectively). However, the average dissimilarity between seasons was considerably high with 71.75%. Terschellingia, Daptonema, and Parodontophora were main genera contributing to similarity/dissimilarity between seasons. At the family leve

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