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| 7. |  | GUERREIRO, R. L.; MCGLUE, M. M.; STONE, J. R.; BERGIER, I.; PAROLIN, M.; CAMINHA, S. A. F. da S.; WARREN, L. V.; ASSINE, M. L. Paleoecology explains Holocene chemical changes in lakes of the Nhecolândia (Pantanal-Brazil). Hydrobiologia, v. 815, n. 1, p. 1-19, jun. 2018.| Biblioteca(s): Embrapa Pantanal. |
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| 8. | | GUERREIRO, R. L.; BERGIER, I.; McGLUE, M. M.; WARREN, L. V.; ABREU, U. G. P. de; ABRAHÃO, J.; ASSINE, M. L. The soda lakes of Nhecolândia: a conservation opportunity for the Pantanal wetlands. Perspectives in Ecology and Conservation, v. 17, p. 9-18, 2019.| Biblioteca(s): Embrapa Pantanal. |
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| Registros recuperados : 8 | |
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 | Acesso ao texto completo restrito à biblioteca da Embrapa Pantanal. Para informações adicionais entre em contato com cpap.biblioteca@embrapa.br. |
Registro Completo
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Biblioteca(s): |
Embrapa Pantanal. |
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Data corrente: |
02/04/2018 |
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Data da última atualização: |
11/03/2019 |
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Tipo da produção científica: |
Artigo em Periódico Indexado |
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Circulação/Nível: |
A - 1 |
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Autoria: |
GUERREIRO, R. L.; MCGLUE, M. M.; STONE, J. R.; BERGIER, I.; PAROLIN, M.; CAMINHA, S. A. F. da S.; WARREN, L. V.; ASSINE, M. L. |
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Afiliação: |
RENATO LADA GUERREIRO, Instituto Federal do Parana-Campus Assis Chateaubriand; MICHAEL M. MCGLUE, University of Kentucky; JEFFERY R. STONE, Indiana State University; IVAN BERGIER TAVARES DE LIMA, CPAP; MAURO PAROLIN, Faculdade Estadual de Ciencias e Letras de Campo Mourão; SILANE A. F. DA SILVA CAMINHA, Universidade Federal de Mato Grosso; LUCAS V. WARREN, Unesp-Universidade Estadual Paulista; MARIO L. ASSINE, Unesp-Universidade Estadual Paulista. |
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Título: |
Paleoecology explains Holocene chemical changes in lakes of the Nhecolândia (Pantanal-Brazil). |
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Ano de publicação: |
2018 |
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Fonte/Imprenta: |
Hydrobiologia, v. 815, n. 1, p. 1-19, jun. 2018. |
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DOI: |
10.1007/s10750-017-3429-3 |
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Idioma: |
Inglês |
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Conteúdo: |
The objective of this research is to examine the history of lentic ecosystem salinity in the southern Pantanal wetlands (Brazil). The timing and controls on hydrochemical changes were inferred using sponge spicule and diatom paleoecology on a Holocene-aged sediment core from Nhecolândia, a lake district situated on a fossil lobe of the Taquari megafan. The oldest portion of the core contains Heterorotula fistula spicules, indicative of an ephemeral freshwater lake that existed until ~ 4.6 cal ka BP. Benthic diatoms of the genus Gomphonema and Eunotia appeared ~ 3.2 cal ka BP, indicating a shallow and dystrophic environment. A transition to a more permanent lake that hosted freshwater sponges (e.g., Corvoheteromeyenia spp.), and diatom assemblages (e.g., Cyclotella meneghiniana, Aulacoseira pantanalensis) endured until ~ 1.3 cal year BP; after this time, most sponges and planktic diatoms disappear from the sedimentary record. High abundances of Anomoeoneis sphaerophora and Craticula guaykuruorum in the latest Holocene reflect a transition to a hyperalkaline, saline lake environment. The results suggest that Nhecolândia?s saline lakes may evolve from freshwater precursors due to local (biochemical) and regional (geo-climatic) controls on water availability, which has implications for patterns of biodiversity and ecosystems services in Pantanal. |
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Palavras-Chave: |
Saline lakes; Salt lakes. |
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Thesagro: |
Água Salina; Salina; Salinidade. |
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Thesaurus NAL: |
Saline water. |
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Categoria do assunto: |
P Recursos Naturais, Ciências Ambientais e da Terra |
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Marc: |
LEADER 02185naa a2200289 a 4500
001 2090018
005 2019-03-11
008 2018 bl uuuu u00u1 u #d
024 7 $a10.1007/s10750-017-3429-3$2DOI
100 1 $aGUERREIRO, R. L.
245 $aPaleoecology explains Holocene chemical changes in lakes of the Nhecolândia (Pantanal-Brazil).$h[electronic resource]
260 $c2018
520 $aThe objective of this research is to examine the history of lentic ecosystem salinity in the southern Pantanal wetlands (Brazil). The timing and controls on hydrochemical changes were inferred using sponge spicule and diatom paleoecology on a Holocene-aged sediment core from Nhecolândia, a lake district situated on a fossil lobe of the Taquari megafan. The oldest portion of the core contains Heterorotula fistula spicules, indicative of an ephemeral freshwater lake that existed until ~ 4.6 cal ka BP. Benthic diatoms of the genus Gomphonema and Eunotia appeared ~ 3.2 cal ka BP, indicating a shallow and dystrophic environment. A transition to a more permanent lake that hosted freshwater sponges (e.g., Corvoheteromeyenia spp.), and diatom assemblages (e.g., Cyclotella meneghiniana, Aulacoseira pantanalensis) endured until ~ 1.3 cal year BP; after this time, most sponges and planktic diatoms disappear from the sedimentary record. High abundances of Anomoeoneis sphaerophora and Craticula guaykuruorum in the latest Holocene reflect a transition to a hyperalkaline, saline lake environment. The results suggest that Nhecolândia?s saline lakes may evolve from freshwater precursors due to local (biochemical) and regional (geo-climatic) controls on water availability, which has implications for patterns of biodiversity and ecosystems services in Pantanal.
650 $aSaline water
650 $aÁgua Salina
650 $aSalina
650 $aSalinidade
653 $aSaline lakes
653 $aSalt lakes
700 1 $aMCGLUE, M. M.
700 1 $aSTONE, J. R.
700 1 $aBERGIER, I.
700 1 $aPAROLIN, M.
700 1 $aCAMINHA, S. A. F. da S.
700 1 $aWARREN, L. V.
700 1 $aASSINE, M. L.
773 $tHydrobiologia$gv. 815, n. 1, p. 1-19, jun. 2018.
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