Origin, concentration, availability and fate of dissolved organic carbon in coastal lagoons of the Rio de Janeiro State

The coastal lagoons in the northern Rio de Janeiro State (Brazil) present a wide gradient of dissolved organic carbon (DOC) and water color, with the highest DOC concentrations reported in the literature for aquatic ecosystems. Thus, they represent a peculiar set of ecosystems for the study of the origin, processing and fate of DOC in inland waters. We reviewed data from 2 decades of studies on the carbon cycle in these coastal lagoons and discussed the fluctuations in the concentration and quality of DOC, factors affecting DOC microbial and photochemical degradation, CO2 emission, as well as the role of humic and non-humic carbon to the energy flow through the trophic chains. We show that DOC quality, not its quantity, determines the rates of photochemical and microbial degradation both seasonally (within system) and spatially (among systems), with the exception of DOC photo-oxidation among lagoons, which is partially explained by DOC concentration at regional scale. In humic lagoons, there is a fairly predictable pattern of seasonal variation in DOC concentration associated to rainfall-induced inputs of allochthonous C. However, little is known about the exact timing of these allochthonous inputs and how they relate to the seasonal variation of DOC chemical properties (i.e. its quality). Depth-integrated photo-oxidation rates were less representative in highly humic lagoons, due to strong light attenuation in the water column. Nevertheless, the potential contribution of photo-oxidation and bacterial respiration to total CO2 efflux (~11%) did not differ significantly when all lagoons were pooled together. Contrary to prevailing paradigms for humic waters, microalgae seem to be the main C source in humic lagoons, sustaining pelagic food webs through zooplankton, in spite of some contribution of allochthonous C. Thus, the predominant role of the microbial loop in the DOC recovery to food webs in such systems is to be questioned.

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Main Authors: Suhett,Albert Luiz, Amado,André Megali, Meirelles-Pereira,Frederico, Scofield,Vinicius, Jacques,Saulo Machado de Souza, Laque,Thaís, Farjalla,Vinicius Fortes
Format: Digital revista
Language:English
Published: Associação Brasileira de Limnologia 2013
Online Access:http://old.scielo.br/scielo.php?script=sci_arttext&pid=S2179-975X2013000300011
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spelling oai:scielo:S2179-975X20130003000112014-02-07Origin, concentration, availability and fate of dissolved organic carbon in coastal lagoons of the Rio de Janeiro StateSuhett,Albert LuizAmado,André MegaliMeirelles-Pereira,FredericoScofield,ViniciusJacques,Saulo Machado de SouzaLaque,ThaísFarjalla,Vinicius Fortes coastal lagoons dissolved organic matter dissolved organic carbon DOC humic substances The coastal lagoons in the northern Rio de Janeiro State (Brazil) present a wide gradient of dissolved organic carbon (DOC) and water color, with the highest DOC concentrations reported in the literature for aquatic ecosystems. Thus, they represent a peculiar set of ecosystems for the study of the origin, processing and fate of DOC in inland waters. We reviewed data from 2 decades of studies on the carbon cycle in these coastal lagoons and discussed the fluctuations in the concentration and quality of DOC, factors affecting DOC microbial and photochemical degradation, CO2 emission, as well as the role of humic and non-humic carbon to the energy flow through the trophic chains. We show that DOC quality, not its quantity, determines the rates of photochemical and microbial degradation both seasonally (within system) and spatially (among systems), with the exception of DOC photo-oxidation among lagoons, which is partially explained by DOC concentration at regional scale. In humic lagoons, there is a fairly predictable pattern of seasonal variation in DOC concentration associated to rainfall-induced inputs of allochthonous C. However, little is known about the exact timing of these allochthonous inputs and how they relate to the seasonal variation of DOC chemical properties (i.e. its quality). Depth-integrated photo-oxidation rates were less representative in highly humic lagoons, due to strong light attenuation in the water column. Nevertheless, the potential contribution of photo-oxidation and bacterial respiration to total CO2 efflux (~11%) did not differ significantly when all lagoons were pooled together. Contrary to prevailing paradigms for humic waters, microalgae seem to be the main C source in humic lagoons, sustaining pelagic food webs through zooplankton, in spite of some contribution of allochthonous C. Thus, the predominant role of the microbial loop in the DOC recovery to food webs in such systems is to be questioned.info:eu-repo/semantics/openAccessAssociação Brasileira de LimnologiaActa Limnologica Brasiliensia v.25 n.3 20132013-09-01info:eu-repo/semantics/articletext/htmlhttp://old.scielo.br/scielo.php?script=sci_arttext&pid=S2179-975X2013000300011en10.1590/S2179-975X2013000300011
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language English
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author Suhett,Albert Luiz
Amado,André Megali
Meirelles-Pereira,Frederico
Scofield,Vinicius
Jacques,Saulo Machado de Souza
Laque,Thaís
Farjalla,Vinicius Fortes
spellingShingle Suhett,Albert Luiz
Amado,André Megali
Meirelles-Pereira,Frederico
Scofield,Vinicius
Jacques,Saulo Machado de Souza
Laque,Thaís
Farjalla,Vinicius Fortes
Origin, concentration, availability and fate of dissolved organic carbon in coastal lagoons of the Rio de Janeiro State
author_facet Suhett,Albert Luiz
Amado,André Megali
Meirelles-Pereira,Frederico
Scofield,Vinicius
Jacques,Saulo Machado de Souza
Laque,Thaís
Farjalla,Vinicius Fortes
author_sort Suhett,Albert Luiz
title Origin, concentration, availability and fate of dissolved organic carbon in coastal lagoons of the Rio de Janeiro State
title_short Origin, concentration, availability and fate of dissolved organic carbon in coastal lagoons of the Rio de Janeiro State
title_full Origin, concentration, availability and fate of dissolved organic carbon in coastal lagoons of the Rio de Janeiro State
title_fullStr Origin, concentration, availability and fate of dissolved organic carbon in coastal lagoons of the Rio de Janeiro State
title_full_unstemmed Origin, concentration, availability and fate of dissolved organic carbon in coastal lagoons of the Rio de Janeiro State
title_sort origin, concentration, availability and fate of dissolved organic carbon in coastal lagoons of the rio de janeiro state
description The coastal lagoons in the northern Rio de Janeiro State (Brazil) present a wide gradient of dissolved organic carbon (DOC) and water color, with the highest DOC concentrations reported in the literature for aquatic ecosystems. Thus, they represent a peculiar set of ecosystems for the study of the origin, processing and fate of DOC in inland waters. We reviewed data from 2 decades of studies on the carbon cycle in these coastal lagoons and discussed the fluctuations in the concentration and quality of DOC, factors affecting DOC microbial and photochemical degradation, CO2 emission, as well as the role of humic and non-humic carbon to the energy flow through the trophic chains. We show that DOC quality, not its quantity, determines the rates of photochemical and microbial degradation both seasonally (within system) and spatially (among systems), with the exception of DOC photo-oxidation among lagoons, which is partially explained by DOC concentration at regional scale. In humic lagoons, there is a fairly predictable pattern of seasonal variation in DOC concentration associated to rainfall-induced inputs of allochthonous C. However, little is known about the exact timing of these allochthonous inputs and how they relate to the seasonal variation of DOC chemical properties (i.e. its quality). Depth-integrated photo-oxidation rates were less representative in highly humic lagoons, due to strong light attenuation in the water column. Nevertheless, the potential contribution of photo-oxidation and bacterial respiration to total CO2 efflux (~11%) did not differ significantly when all lagoons were pooled together. Contrary to prevailing paradigms for humic waters, microalgae seem to be the main C source in humic lagoons, sustaining pelagic food webs through zooplankton, in spite of some contribution of allochthonous C. Thus, the predominant role of the microbial loop in the DOC recovery to food webs in such systems is to be questioned.
publisher Associação Brasileira de Limnologia
publishDate 2013
url http://old.scielo.br/scielo.php?script=sci_arttext&pid=S2179-975X2013000300011
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