Náttúrufræðingurinn

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Náttúrufræðingurinn - 1998, Side 34

Náttúrufræðingurinn - 1998, Side 34
Kharaka & A.S. Maest). Balkema, Rotterdam. Bls. 477-481. Sigurður R. Gíslason, Stefán Arnórsson & Halldór Armannsson 1996. Chemical weath- ering of basalt in Southwest Iceland: effects of runoff, age of rocks and vegetative/glacial cover. American Journal of Science 296. 837- 907. SigurðurGuðjónsson 1990. Classifícation oflce- landic watersheds and rivers to explain life his- tory strategies of Atlantic salmon. Ph.D,- ritgerð, Oregon State University. 136 bls. Sigurjón Rist 1974. Efnarannsókn vatna. Vatnasvið Hvítár - Ölfusár; einnig Þjórsár við Urriðafoss 1973. Orkustofnun OSV-7405. 29 bls. Sigurjón Rist 1986. Efnarannsókn vatna. Borgar- fjörður; einnig Elliðaár í Reykjavík. Orku- stofnun OS-86070/VOD-03. 67 bls. Svanur Pálsson & Guðmundur Vigfússon 1996. Gagnasafn aurburðarmælinga 1963-1995. Orkustofnun OS-96032/VOD-05 B. 270 bls. Vannote, R.I., G.W. Minshall, K.W. Cummins, J.R. Sedell & C.E. Cushing 1980. The river continuum concept. Can. J. Fish. Aquatic Sci. 37. 130-137. Wuhrmann, K. 1974. Some problems and per- spectives in applied limnology. Mitt. Internat. Verein. Limnol. 20. 324^102. Þorleifur Einarsson 1991. Myndun og mótun lands: jarðfræði. Mál og menning, Reykjavík. 299 bls. ■ SUMMARY Terrestrial influence ön the biota in ICELANDIC RIVERS Chemical composition in rivers is determined by the geology, topography and vegetation cover in the catchment areas (fig. 7, table 1). This seems to determine the productivity of the rivers in the catchment areas as indicated by catch of salmon and density of benthic invertebrates. Catchment areas of Icelandic rivers are described and fluc- tuations of nutrients (figs 8 and 9). Rivers origi- nating in lakes and from areas with extensive cover of vegetation produced much more Atlan- tic salmon (Salmo salar) than rivers originating from barren areas, which only produced few salmon or none (fig 10). Organic matter dril'ting downstream from river headwaters determined species composition of benthic communities. Filter-feeding blackfly larvae (Simulium vittatum) dominated lake outlets (fig. 11), whereas algae-grazing chironomids dominated rivers without lake influence (fíg 12). Glacial riv- ers have the lowest density and diversity of benthic invertebrates of all river groups (fig. 13). The study is supported by the Research Council of Iceland (Science Fund), the Research Fund of the University of Iceland and the Framework of EU (Environment and Climate) to the project AASER (Contract ENV-CT95-0164). PÓSTFANG HÖFUNDa/AuTHORS'ADDRESSES Hákon Aðalsteinsson Orkustofnun / National Energy Authority Grensásvegi 9 IS-108Reykjavík ha@os.is Gísli Már Gíslason Líffræðistofnun Háskólans / Institute of Biology, University of Iceland Grensásvegi 12 IS-108Reykjavík gmg@rhi.hi.is 112

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