Phytoplankton and primary production of the Paraná Medio river.

This paper deals with the phytoplankton primary production and some of its limnological parameters of the Middle Paraná River in the stretch Corrientes-Esquina.Primary production estomates were obtained from incubation in situ of light and dark bottle columns, assessing the 14C fixation during March...

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Autor principal: Bonetto, Carlos A.
Formato: Artículo revista
Lenguaje:Español
Publicado: Centro de Ecología Aplicada del Litoral (Consejo Nacional de Investigaciones Científicas y Técnicas - Universidad Nacional de Nordeste) 2024
Acceso en línea:https://revistas.unne.edu.ar/index.php/eco/article/view/8041
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spelling I48-R154-article-80412024-12-20T15:20:37Z Phytoplankton and primary production of the Paraná Medio river. Fitoplancton y producción primaria del Paraná Medio Bonetto, Carlos A. This paper deals with the phytoplankton primary production and some of its limnological parameters of the Middle Paraná River in the stretch Corrientes-Esquina.Primary production estomates were obtained from incubation in situ of light and dark bottle columns, assessing the 14C fixation during March 1961-March 1962.The annual carbon fixation pattern showed changes closely related to the plankton concentration, transparency of the water and hydrometric level of the river. Primary production was low during the flood in conditions of high phytoplankton dilution and water turbity, increasing sharply during the low water favoured by the increment in phytoplankton concentration and transparency.In Corrientes, there are important limnological differences between both two margins. The influence of the Paraguay River increases the suspended and dissolved solids towards the right bank. Phytoplankton production is very low there, because of the high turbidity. In Esquina, about 300 km down stream there are still some differences in the cross section. . Centro de Ecología Aplicada del Litoral (Consejo Nacional de Investigaciones Científicas y Técnicas - Universidad Nacional de Nordeste) 2024-12-20 info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion Artículo revisado por pares application/pdf https://revistas.unne.edu.ar/index.php/eco/article/view/8041 Ecosur; 1983: vol. 10, nos. 19-20; 79-102 0325-108X spa https://revistas.unne.edu.ar/index.php/eco/article/view/8041/7495 https://creativecommons.org/licenses/by-nc/4.0
institution Universidad Nacional del Nordeste
institution_str I-48
repository_str R-154
container_title_str Revistas UNNE - Universidad Nacional del Noroeste (UNNE)
language Español
format Artículo revista
author Bonetto, Carlos A.
spellingShingle Bonetto, Carlos A.
Phytoplankton and primary production of the Paraná Medio river.
author_facet Bonetto, Carlos A.
author_sort Bonetto, Carlos A.
title Phytoplankton and primary production of the Paraná Medio river.
title_short Phytoplankton and primary production of the Paraná Medio river.
title_full Phytoplankton and primary production of the Paraná Medio river.
title_fullStr Phytoplankton and primary production of the Paraná Medio river.
title_full_unstemmed Phytoplankton and primary production of the Paraná Medio river.
title_sort phytoplankton and primary production of the paraná medio river.
description This paper deals with the phytoplankton primary production and some of its limnological parameters of the Middle Paraná River in the stretch Corrientes-Esquina.Primary production estomates were obtained from incubation in situ of light and dark bottle columns, assessing the 14C fixation during March 1961-March 1962.The annual carbon fixation pattern showed changes closely related to the plankton concentration, transparency of the water and hydrometric level of the river. Primary production was low during the flood in conditions of high phytoplankton dilution and water turbity, increasing sharply during the low water favoured by the increment in phytoplankton concentration and transparency.In Corrientes, there are important limnological differences between both two margins. The influence of the Paraguay River increases the suspended and dissolved solids towards the right bank. Phytoplankton production is very low there, because of the high turbidity. In Esquina, about 300 km down stream there are still some differences in the cross section.
publisher Centro de Ecología Aplicada del Litoral (Consejo Nacional de Investigaciones Científicas y Técnicas - Universidad Nacional de Nordeste)
publishDate 2024
url https://revistas.unne.edu.ar/index.php/eco/article/view/8041
work_keys_str_mv AT bonettocarlosa phytoplanktonandprimaryproductionoftheparanamedioriver
AT bonettocarlosa fitoplanctonyproduccionprimariadelparanamedio
first_indexed 2025-05-17T05:12:37Z
last_indexed 2025-05-17T05:12:37Z
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