Plankton and hydrochemistry of Lake Futalaufquen (Patagonia, Argentina) during the growing season

Plankton communities and hydrochemistry of an oligotrophic lake occupying a glacial valley in Argentinian Patagonia (42 °49′S; 71 °43′W) were studied. Monthly samples at three stations integrated from 0 to 50 m and stratified samples at the site of maximum depth, were taken during the growing season...

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Autor principal: Pizzolon, Lino Arturo
Otros Autores: Santinelli, N., Marinone, M.C, Menu-Marque, S.A
Formato: Capítulo de libro
Lenguaje:Inglés
Publicado: Kluwer Academic Publishers 1995
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100 1 |a Pizzolon, Lino Arturo 
245 1 0 |a Plankton and hydrochemistry of Lake Futalaufquen (Patagonia, Argentina) during the growing season 
260 |b Kluwer Academic Publishers  |c 1995 
270 1 0 |m Pizzolon, L.; Laboratorio de Ecología Acuática, Universidad Nacional de la Patagonia, Esquel, Chubut, 9200, Argentina 
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504 |a Díaz, M. & F. L. Pedrozo, 1994. Nutrient limitation in Andean-Patagonian lakes at latitude 40–41 °S. Submitted to Arch. Hydrobiol, 35 pp; Dodds, W. K, Johnson, K.R., Priscu, J.C., Simultaneous nitrogen and phosphorus deficiency in natural phytoplankton assemblages: theory, empirical evidence, and implications for lake management (1989) Lake and Reservoir Management, 5, pp. 21-26 
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504 |a Soto, D., Campos, H., Steffen, W., Agüero, G., Parra, O., Zúñiga, L., The Torres del Paine lake district (Chilean Patagonia): A case of potentially N-limited lakes and ponds (1994) Arch. Hydrobiol. (Supp.), 99, pp. 181-197 
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504 |a Zúñiga, L.R., Domínguez, P.T., Entomostracos planctónicos del Lago Riñihue (Valdivia, Chile): distribución temporal de la taxocenosis (1978) Anal. Mus. Hist. Nat. Valparaiso, 11, pp. 89-95 
506 |2 openaire  |e Política editorial 
520 3 |a Plankton communities and hydrochemistry of an oligotrophic lake occupying a glacial valley in Argentinian Patagonia (42 °49′S; 71 °43′W) were studied. Monthly samples at three stations integrated from 0 to 50 m and stratified samples at the site of maximum depth, were taken during the growing season. Transparency was always controlled by glacial silt, and not by phytoplankton. Lake water belongs to the calcium-bicarbonate type, with low conductivity (24 μS cm-1), and poor buffering capacity. Forty-five phytoplankton taxa were found. Mean phytoplankton density was 49 cells ml-1 and mean biomass 69 μg l-1. N:P relationships, inorganic nitrogen exhaustion in the photic layer, and correlations between nutrients and phytoplankton density suggests nitrogen as the main limiting factor. Fifteen zooplankton species were found. Mean zooplankton density was 12.2 ind. l-1 and mean biomass 22.9 μg l-1. Diatoms and Boeckellidae were the dominant planktonic groups. Morphometry and hydrological factors were responsible for horizontal heterogeneity in phytoplankton and chemical variables. © 1995 Kluwer Academic Publishers.  |l eng 
593 |a Laboratorio de Ecología Acuática, Universidad Nacional de la Patagonia, Esquel, Chubut, 9200, Argentina 
593 |a Facultad de Ciencias Naturales, Universidad Nacional de la Patagonia, Trelew, Chubut, 9100, Argentina 
593 |a Departamento de Ciencias Biológicas, Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires, Pabellón II, Ciudad Universitaria, Buenos Aires, 1428, Argentina 
651 4 |a ARGENTINA, PATAGONIA, LAKE FUTALAUFQUEN 
690 1 0 |a NITROGEN LIMITATION 
690 1 0 |a OLIGOTROPHY 
690 1 0 |a PATAGONIA 
690 1 0 |a PHYTOPLANKTON 
690 1 0 |a SPATIAL HETEROGENEITY 
690 1 0 |a ZOOPLANCTON 
690 1 0 |a DIATOM 
690 1 0 |a HYDROCHEMISTRY 
690 1 0 |a NITROGEN 
690 1 0 |a OLIGOTROPHIC LAKE 
690 1 0 |a PHYTOPLANKTON 
690 1 0 |a POPULATION DENSITY 
690 1 0 |a WATER CHEMISTRY 
690 1 0 |a ZOOPLANKTON 
690 1 0 |a BOECKELLIDAE 
700 1 |a Santinelli, N. 
700 1 |a Marinone, M.C. 
700 1 |a Menu-Marque, S.A. 
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