Biogeochemical diversity, O2-supersaturation and hot moments of GHG emissions from shallow alkaline lakes in the Pantanal of Nhecolândia, Brazil

dc.contributor.authorBARBIERO, LAURENT
dc.contributor.authorSIQUEIRA NETO, MARCOS
dc.contributor.authorBRAZ, ROSANGELA R.
dc.contributor.authorCARMO, JANAINA B. do
dc.contributor.authorREZENDE FILHO, ARY T.
dc.contributor.authorMAZZI, EDMAR
dc.contributor.authorFERNANDES, FERNANDO A.
dc.contributor.authorDAMATTO, SANDRA R.
dc.contributor.authorCAMARGO, PLINIO B. de
dc.coverageInternacionalpt_BR
dc.date.accessioned2018-04-19T17:41:37Z
dc.date.available2018-04-19T17:41:37Z
dc.date.issued2018pt_BR
dc.description.abstractNhecolândia is a vast sub-region of the Pantanal wetland in Brazil with great diversity in surface water chemistry evolving in a sodic alkaline pathway under the influence of evaporation. In this region, > 15,000 shallow lakes are likely to contribute an enormous quantity of greenhouse gas to the atmosphere, but the diversity of the biogeochemical scenarios and their variability in time and space is a major challenge to estimate the regional contribution. From 4 selected alkaline lakes, we compiled measurements of the physico-chemical characteristics of water and sediments, gas fluxes in floating chambers, and sedimentation rates to illustrate this diversity. Although these lakes have a similar chemical composition, the results confirm a difference between the black-water and green-water alkaline lakes, corresponding to distinct biogeochemical functioning. This difference does not appear to affect lake sedimentation rates, but is reflected in gas emissions. Black-water lakes are CO2 and CH4 sources, with fairly constant emissions throughout the seasons. Annual carbon dioxide and methane emissions approach 0.86 mol m− 2 y− 1 and 0.07 mol m− 2 y− 1, respectively, and no clear trend towards N2O capture or emission was observed. By contrast, green-water lakes are CO2 and N2O sinks but important CH4 sources with fluxes varying significantly throughout the seasons, depending on the magnitude of the phytoplankton bloom. The results highlight important daily and seasonal variations in gas fluxes, and in particular a hot moments for methane emissions, when the O2-supersaturation is reached during the afternoon under extreme bloom and sunny weather conditions, provoking an abrupt O2 purging of the lakes. Taking into account the seasonal variability, annual methane emissions are around 10.2 mol m− 2 y− 1, i.e., much higher than reported in previous studies for alkaline lakes in Nhecolândia. Carbon dioxide and nitrous oxide consumption is estimated about 1.9 mol m− 2 y− 1 and 0.73 mmol m− 2 y− 1, respectively. However, these balances must be better constrained with systematic and targeted measurements throughout the seasons.pt_BR
dc.description.sponsorshipFundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)pt_BR
dc.description.sponsorshipConselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)pt_BR
dc.description.sponsorshipIDFAPESP: 13/09192-0; 16/14227-5pt_BR
dc.description.sponsorshipIDCNPq: 443030/2015-4pt_BR
dc.format.extent1420-1430pt_BR
dc.identifier.citationBARBIERO, LAURENT; SIQUEIRA NETO, MARCOS; BRAZ, ROSANGELA R.; CARMO, JANAINA B. do; REZENDE FILHO, ARY T.; MAZZI, EDMAR; FERNANDES, FERNANDO A.; DAMATTO, SANDRA R.; CAMARGO, PLINIO B. de. Biogeochemical diversity, O2-supersaturation and hot moments of GHG emissions from shallow alkaline lakes in the Pantanal of Nhecolândia, Brazil. <b>Science of the Total Environment</b>, v. 619-620, p. 1420-1430, 2018. DOI: <a href="https://dx.doi.org/10.1016/j.scitotenv.2017.11.197">10.1016/j.scitotenv.2017.11.197</a>. Disponível em: http://repositorio.ipen.br/handle/123456789/28861.
dc.identifier.doi10.1016/j.scitotenv.2017.11.197pt_BR
dc.identifier.issn0048-9697pt_BR
dc.identifier.percentilfi89.44en
dc.identifier.percentilfiCiteScore88.75
dc.identifier.urihttp://repositorio.ipen.br/handle/123456789/28861
dc.identifier.vol619-620pt_BR
dc.relation.ispartofScience of the Total Environmentpt_BR
dc.rightsopenAccesspt_BR
dc.subjectgreenhouse gases
dc.subjectemission
dc.subjectoxygen
dc.subjectsupersaturation
dc.subjectbiogeochemistry
dc.subjectlakes
dc.subjectbrazil
dc.subjectwetlands
dc.subjectmethane
dc.subjectcarbon dioxide
dc.subjectnitrous oxide
dc.titleBiogeochemical diversity, O2-supersaturation and hot moments of GHG emissions from shallow alkaline lakes in the Pantanal of Nhecolândia, Brazilpt_BR
dc.typeArtigo de periódicopt_BR
dspace.entity.typePublication
ipen.autorSANDRA REGINA DAMATTO
ipen.codigoautor537
ipen.contributor.ipenauthorSANDRA REGINA DAMATTO
ipen.date.recebimento18-04pt_BR
ipen.identifier.fi5.589pt_BR
ipen.identifier.fiCiteScore7.4
ipen.identifier.ipendoc24324pt_BR
ipen.identifier.iwosWoSpt_BR
ipen.identifier.ods13
ipen.range.fi4.500 - 5.999
ipen.range.percentilfi75.00 - 100.00
ipen.type.genreArtigo
relation.isAuthorOfPublication400a52c2-e76f-4536-9966-d7fe1476f2b4
relation.isAuthorOfPublication.latestForDiscovery400a52c2-e76f-4536-9966-d7fe1476f2b4
sigepi.autor.atividadeDAMATTO, SANDRA R.:537:340:Npt_BR
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