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Registro Completo |
Biblioteca(s): |
Embrapa Agrossilvipastoril. |
Data corrente: |
18/01/2018 |
Data da última atualização: |
23/01/2018 |
Tipo da produção científica: |
Artigo em Periódico Indexado |
Autoria: |
OLIVEIRA JUNIOR, J. C. de; BEIRIGO, R. M.; CHIAPINI, M.; NASCIMENTO, A. F. do; COUTO, E. G.; VIDAL-TORRADO, P. |
Afiliação: |
JAIRO CALDERARI DE OLIVEIRA JUNIOR, UFTPR; RAPHAEL MOREIRA BEIRIGO, UFPB; MARIANE CHIAPINI, USP-ESQLQ; ALEXANDRE FERREIRA DO NASCIMENTO, CPAMT; EDUARDO GUIMARÃES COUTO, UFMT-CUIABA; PABLO VIDAL-TORRADO, USP-ESALQ. |
Título: |
Origin of mounds in the Pantanal wetlands: An integrated approach between geomorphology, pedogenesis, ecology and soil micromorphology. |
Ano de publicação: |
2017 |
Fonte/Imprenta: |
PLoS One, v. 12, n. 7, e0179197, 2017. |
Idioma: |
Inglês |
Conteúdo: |
Vegetated mounds are an important geomorphological feature of the Pantanal, where the influence of floods dictates not only hydropedological processes, but also the distribution and ecology of the flora and fauna. This work aimed to identify factors and processes that influence the formation and spatial distribution of the mounds, which are commonly associated with termite activity. In order to characterize pedological processes, macro and micro morphological descriptions, satellite image interpretation, dating of the sandy sedimentary material using OSL and carbon dating using 14C AMS were carried out. This dating of the materials indicates that the sediments in which the soils were formed were deposited during the Pleistocene, while the carbonates are from the Holocene. The basin-like format of the laminar structures suggests that part of the more clayey material was deposited in lacustrine environments. The more humid climate in the Holocene intensified argilluviation, which at an advanced stage, led to a more pronounced textural gradient, reducing drainage and leading to ferrolysis and thickening of the E horizon. Besides pedogenic processes, more erosive flooding during the Holocene began reducing and rounding the landscape's more elevated structures (paleolevees). In the final stage, these structures were occupied by termites to shelter from flooding. Thereafter, the bio-cementation action of the termite nests has increased the resistance of the vegetated mounds to processes of erosion. MenosVegetated mounds are an important geomorphological feature of the Pantanal, where the influence of floods dictates not only hydropedological processes, but also the distribution and ecology of the flora and fauna. This work aimed to identify factors and processes that influence the formation and spatial distribution of the mounds, which are commonly associated with termite activity. In order to characterize pedological processes, macro and micro morphological descriptions, satellite image interpretation, dating of the sandy sedimentary material using OSL and carbon dating using 14C AMS were carried out. This dating of the materials indicates that the sediments in which the soils were formed were deposited during the Pleistocene, while the carbonates are from the Holocene. The basin-like format of the laminar structures suggests that part of the more clayey material was deposited in lacustrine environments. The more humid climate in the Holocene intensified argilluviation, which at an advanced stage, led to a more pronounced textural gradient, reducing drainage and leading to ferrolysis and thickening of the E horizon. Besides pedogenic processes, more erosive flooding during the Holocene began reducing and rounding the landscape's more elevated structures (paleolevees). In the final stage, these structures were occupied by termites to shelter from flooding. Thereafter, the bio-cementation action of the termite nests has increased the resistance of the vegetated mounds to pro... Mostrar Tudo |
Palavras-Chave: |
Mato Grosso; Plants; Wetland. |
Thesagro: |
Fauna; Flora. |
Thesaurus Nal: |
Biogeography; Botany; Climate change; Ecology; Environmental factors; Floods; Microstructure; Pantanal; Soil formation; Termite mounds. |
Categoria do assunto: |
P Recursos Naturais, Ciências Ambientais e da Terra |
URL: |
https://ainfo.cnptia.embrapa.br/digital/bitstream/item/171316/1/2017-cpamt-alexandre-nascimento-pantanal-wetlands.pdf
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Marc: |
LEADER 02514naa a2200361 a 4500 001 2085773 005 2018-01-23 008 2017 bl uuuu u00u1 u #d 100 1 $aOLIVEIRA JUNIOR, J. C. de 245 $aOrigin of mounds in the Pantanal wetlands$bAn integrated approach between geomorphology, pedogenesis, ecology and soil micromorphology.$h[electronic resource] 260 $c2017 520 $aVegetated mounds are an important geomorphological feature of the Pantanal, where the influence of floods dictates not only hydropedological processes, but also the distribution and ecology of the flora and fauna. This work aimed to identify factors and processes that influence the formation and spatial distribution of the mounds, which are commonly associated with termite activity. In order to characterize pedological processes, macro and micro morphological descriptions, satellite image interpretation, dating of the sandy sedimentary material using OSL and carbon dating using 14C AMS were carried out. This dating of the materials indicates that the sediments in which the soils were formed were deposited during the Pleistocene, while the carbonates are from the Holocene. The basin-like format of the laminar structures suggests that part of the more clayey material was deposited in lacustrine environments. The more humid climate in the Holocene intensified argilluviation, which at an advanced stage, led to a more pronounced textural gradient, reducing drainage and leading to ferrolysis and thickening of the E horizon. Besides pedogenic processes, more erosive flooding during the Holocene began reducing and rounding the landscape's more elevated structures (paleolevees). In the final stage, these structures were occupied by termites to shelter from flooding. Thereafter, the bio-cementation action of the termite nests has increased the resistance of the vegetated mounds to processes of erosion. 650 $aBiogeography 650 $aBotany 650 $aClimate change 650 $aEcology 650 $aEnvironmental factors 650 $aFloods 650 $aMicrostructure 650 $aPantanal 650 $aSoil formation 650 $aTermite mounds 650 $aFauna 650 $aFlora 653 $aMato Grosso 653 $aPlants 653 $aWetland 700 1 $aBEIRIGO, R. M. 700 1 $aCHIAPINI, M. 700 1 $aNASCIMENTO, A. F. do 700 1 $aCOUTO, E. G. 700 1 $aVIDAL-TORRADO, P. 773 $tPLoS One$gv. 12, n. 7, e0179197, 2017.
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Registro original: |
Embrapa Agrossilvipastoril (CPAMT) |
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Registro Completo
Biblioteca(s): |
Embrapa Rondônia. |
Data corrente: |
06/08/2010 |
Data da última atualização: |
07/06/2017 |
Tipo da produção científica: |
Folder/Folheto/Cartilha |
Autoria: |
FERREIRA, M. das G. R. |
Afiliação: |
MARIA DAS GRACAS RODRIGUES FERREIRA, CPAF-RO. |
Título: |
Crajiru (Arrabidaea chica Verlot). |
Ano de publicação: |
2005 |
Fonte/Imprenta: |
Porto Velho: Embrapa Rondônia, 2005. |
Descrição Física: |
Folder. |
Idioma: |
Português |
Conteúdo: |
Este folder reúne informações sobre o crajiru, planta arbustiva trepadeira. Explica simplificadamente os aspectos agronômicos, as propriedades medicinais, o uso não medicinal e o princípio ativo. |
Palavras-Chave: |
Arrabidaea chica Verlot; Crajiru; Planta arbustiva trepadeira. |
Thesagro: |
Planta Medicinal. |
Categoria do assunto: |
K Ciência Florestal e Produtos de Origem Vegetal |
URL: |
https://ainfo.cnptia.embrapa.br/digital/bitstream/item/24786/1/folder-crajiru.pdf
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Marc: |
LEADER 00648nam a2200169 a 4500 001 1859496 005 2017-06-07 008 2005 bl uuuu u0uu1 u #d 100 1 $aFERREIRA, M. das G. R. 245 $aCrajiru (Arrabidaea chica Verlot). 260 $aPorto Velho: Embrapa Rondônia$c2005 300 $cFolder. 520 $aEste folder reúne informações sobre o crajiru, planta arbustiva trepadeira. Explica simplificadamente os aspectos agronômicos, as propriedades medicinais, o uso não medicinal e o princípio ativo. 650 $aPlanta Medicinal 653 $aArrabidaea chica Verlot 653 $aCrajiru 653 $aPlanta arbustiva trepadeira
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