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Titlebook: Salt Lakes; Proceedings of the I W. D. Williams Conference proceedings 1981 Dr W. Junk Publishers The Hague-Boston-London 1981 Fauna.benthi

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On the chemistry of some salt lakes and ponds in Yugoslavia,elp us to understand processes important for all lakes, including those exposed to less extreme physic-chemical regimes (Eugster & Hardie 1978). Unfortunately, with some exceptions, they characterize arid regions and are generally accessible for continuous study only with difficulty (Williams 1978).
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On the chemistry and biota of some saline lakes in Western Australia, occur between lakes in these two regions, the only major differences being the presence of dense angiosperm beds (. and .) and several invertebrates with marine affinities in some of the South Australian lakes.
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The ecology of plankton fauna in saline river pools,e Darling Scarp. Below the scarp, the river, now called the Swan, resumes the meanders of an old river as it travels a further 50 km across the coastal plain to the sea. Along most of this final section, intrusion of sea water creates estuarine conditions.
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Photosynthetic activity of phytoplankton in tropical African soda lakes, 30 g O. m.h., and a rate of 36 g O. m.d. was calculated by Melack & Kilham from diel free water analyses in Lake Nakuru (Kenya). More recently, Melack (1979a) reported similar rates for the phytoplankton of Lake Simbi (Kenya).
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Aquatic plant communities of poikilosaline waters,aline group, consists of a number of aquatic plant species occurring in various fresh waters, mixo- and hyperhaline brackish waters, and in continental waters of very different chemical composition and concentration.
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Primary production in saline lakes,the measurement represents the dynamics of the real system. Considerable controversy has always been associated with the choice of method, the frequency of measurement, the length of production incubations, and the comparison of results employing different methods.
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Ostracods of athalassic saline lakes,t time. Confusion also arose when the authors dealt with forms from the Pontocaspian region, that is the Caspian, Black and Aral Seas; rarely was it clearly stated if the ostracods had actually been collected from these inland seas or from adjacent lagoons (and if these were connected with an inland sea).
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