Land-ocean fluxes in the Paranaguá Bay estuarine system, southern Brazil

A worldwide modeling effort has been proposed by the LOICZ (Land-Ocean Interactions in the Coastal Zone) Program to foster the acquisition of intercomparable data on land-ocean fluxes in estuaries and continental shelf ecosystems from all continental margins. As part of the South American component of this initiative, we present flux estimates of water, salt, dissolved inorganic phosphorus (DIP), dissolved inorganic nitrogen (DIN) and plankton for the estuarine system of Paranaguá Bay, southern Brazil, based on the LOICZ modeling approach and local data obtained during the 1990's. This system is strongly influenced by a seasonal meteorological cycle, represented by the rainy/summer and dry/winter periods. Semi-diurnal tides of up to the 2.7-m range are responsible for the short time-scale dynamics. The model indicated a potential water export to the adjacent coast of up to 7 x 10(6) m³ d-1 in the dry season, and 28 x 10(6) m³ d-1 during the rainy season. The system exhibits seasonal and spatial variations in DIP and DIN fluxes. "DIP amounted to +2.3 x 10(6) mol P yr-1 and "DIN to -2.7 x 10(6) mol N yr-1, suggesting that net production of phosphate and consumption of inorganic nitrogen predominate throughout in the system. Fluxes and therefore export of DIN and eespecially of DIP are higher in the rainy season. Stoichiometric estimates based on the C:N:P ratios of the reacting particulate organic matter (mangrove and plankton detritus) suggest that net denitrification predominates all over the bay, with values between -24.3 and -10.6 x 10(6) mol N year-1. Estimated seaward outflows had little effect upon the fate of the phyto- and zooplankton biomass in different sectors of the bay. This is exemplified by the low net export of algal production from the upper to the middle sectors of the estuary.

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Main Authors: Marone,Eduardo, Machado,Eunice C., Lopes,Rubens M., Silva,Eduardo Teixeira da
Format: Digital revista
Language:English
Published: Universidade de São Paulo, Instituto Oceanográfico 2005
Online Access:http://old.scielo.br/scielo.php?script=sci_arttext&pid=S1679-87592005000200007
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spelling oai:scielo:S1679-875920050002000072009-07-08Land-ocean fluxes in the Paranaguá Bay estuarine system, southern BrazilMarone,EduardoMachado,Eunice C.Lopes,Rubens M.Silva,Eduardo Teixeira da Mass balance DIN and DIP budgets Plankton dynamics Paranaguá Bay Brazil A worldwide modeling effort has been proposed by the LOICZ (Land-Ocean Interactions in the Coastal Zone) Program to foster the acquisition of intercomparable data on land-ocean fluxes in estuaries and continental shelf ecosystems from all continental margins. As part of the South American component of this initiative, we present flux estimates of water, salt, dissolved inorganic phosphorus (DIP), dissolved inorganic nitrogen (DIN) and plankton for the estuarine system of Paranaguá Bay, southern Brazil, based on the LOICZ modeling approach and local data obtained during the 1990's. This system is strongly influenced by a seasonal meteorological cycle, represented by the rainy/summer and dry/winter periods. Semi-diurnal tides of up to the 2.7-m range are responsible for the short time-scale dynamics. The model indicated a potential water export to the adjacent coast of up to 7 x 10(6) m³ d-1 in the dry season, and 28 x 10(6) m³ d-1 during the rainy season. The system exhibits seasonal and spatial variations in DIP and DIN fluxes. "DIP amounted to +2.3 x 10(6) mol P yr-1 and "DIN to -2.7 x 10(6) mol N yr-1, suggesting that net production of phosphate and consumption of inorganic nitrogen predominate throughout in the system. Fluxes and therefore export of DIN and eespecially of DIP are higher in the rainy season. Stoichiometric estimates based on the C:N:P ratios of the reacting particulate organic matter (mangrove and plankton detritus) suggest that net denitrification predominates all over the bay, with values between -24.3 and -10.6 x 10(6) mol N year-1. Estimated seaward outflows had little effect upon the fate of the phyto- and zooplankton biomass in different sectors of the bay. This is exemplified by the low net export of algal production from the upper to the middle sectors of the estuary.info:eu-repo/semantics/openAccessUniversidade de São Paulo, Instituto OceanográficoBrazilian Journal of Oceanography v.53 n.3-4 20052005-12-01info:eu-repo/semantics/articletext/htmlhttp://old.scielo.br/scielo.php?script=sci_arttext&pid=S1679-87592005000200007en10.1590/S1679-87592005000200007
institution SCIELO
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country Brasil
countrycode BR
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access En linea
databasecode rev-scielo-br
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region America del Sur
libraryname SciELO
language English
format Digital
author Marone,Eduardo
Machado,Eunice C.
Lopes,Rubens M.
Silva,Eduardo Teixeira da
spellingShingle Marone,Eduardo
Machado,Eunice C.
Lopes,Rubens M.
Silva,Eduardo Teixeira da
Land-ocean fluxes in the Paranaguá Bay estuarine system, southern Brazil
author_facet Marone,Eduardo
Machado,Eunice C.
Lopes,Rubens M.
Silva,Eduardo Teixeira da
author_sort Marone,Eduardo
title Land-ocean fluxes in the Paranaguá Bay estuarine system, southern Brazil
title_short Land-ocean fluxes in the Paranaguá Bay estuarine system, southern Brazil
title_full Land-ocean fluxes in the Paranaguá Bay estuarine system, southern Brazil
title_fullStr Land-ocean fluxes in the Paranaguá Bay estuarine system, southern Brazil
title_full_unstemmed Land-ocean fluxes in the Paranaguá Bay estuarine system, southern Brazil
title_sort land-ocean fluxes in the paranaguá bay estuarine system, southern brazil
description A worldwide modeling effort has been proposed by the LOICZ (Land-Ocean Interactions in the Coastal Zone) Program to foster the acquisition of intercomparable data on land-ocean fluxes in estuaries and continental shelf ecosystems from all continental margins. As part of the South American component of this initiative, we present flux estimates of water, salt, dissolved inorganic phosphorus (DIP), dissolved inorganic nitrogen (DIN) and plankton for the estuarine system of Paranaguá Bay, southern Brazil, based on the LOICZ modeling approach and local data obtained during the 1990's. This system is strongly influenced by a seasonal meteorological cycle, represented by the rainy/summer and dry/winter periods. Semi-diurnal tides of up to the 2.7-m range are responsible for the short time-scale dynamics. The model indicated a potential water export to the adjacent coast of up to 7 x 10(6) m³ d-1 in the dry season, and 28 x 10(6) m³ d-1 during the rainy season. The system exhibits seasonal and spatial variations in DIP and DIN fluxes. "DIP amounted to +2.3 x 10(6) mol P yr-1 and "DIN to -2.7 x 10(6) mol N yr-1, suggesting that net production of phosphate and consumption of inorganic nitrogen predominate throughout in the system. Fluxes and therefore export of DIN and eespecially of DIP are higher in the rainy season. Stoichiometric estimates based on the C:N:P ratios of the reacting particulate organic matter (mangrove and plankton detritus) suggest that net denitrification predominates all over the bay, with values between -24.3 and -10.6 x 10(6) mol N year-1. Estimated seaward outflows had little effect upon the fate of the phyto- and zooplankton biomass in different sectors of the bay. This is exemplified by the low net export of algal production from the upper to the middle sectors of the estuary.
publisher Universidade de São Paulo, Instituto Oceanográfico
publishDate 2005
url http://old.scielo.br/scielo.php?script=sci_arttext&pid=S1679-87592005000200007
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