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Registro Completo |
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Biblioteca(s): |
Embrapa Uva e Vinho. |
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Data corrente: |
05/07/2012 |
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Data da última atualização: |
10/10/2023 |
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Tipo da produção científica: |
Artigo em Anais de Congresso |
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Autoria: |
HOFF, R.; FALCADE, I.; TONIETTO, J. |
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Afiliação: |
ROSEMARY HOFF, CNPUV; IVANIRA FALCADE, UNIVERSIDADE DE CAXIAS DO SUL; JORGE TONIETTO, CNPUV. |
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Título: |
The geology in the context of geographical indications of fine wines in Serra Gaúcha region (Brazil). |
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Ano de publicação: |
2012 |
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Fonte/Imprenta: |
CONGRES DES TERROIRS VITIVINICOLES. 9., 2012, Bourgogne, France. Actes... Bourgogne, Dijon; Champgne, Reims, CIVC, 25 a 29 Juin 2012. |
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Páginas: |
8-41 |
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Idioma: |
Inglês |
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Conteúdo: |
In Brazil, studies of zoning in wine have contributed to the development of geographical indications. As for the geographical identity, the geology of the criteria has been a subject of research. The region of the Serra Gaúcha, located in northeastem Rio Grande do Sul, Brazil, has a geodiversity that induce the formation of soils and terrain, comprising natural and cultural factors that imply different responses of agronomic vine. These features value the production of wines with unique qualities, which can define different terroirs. The region is at the limit of the geomorphologic units Serra Geral and Planalto dos Campos Gerais, generated from the rocks of the Serra Geral Formation. ln the Pinto Bandeira geographical indication for fine wines occurs in the most of area, the Caxias Facies of Serra Geral Formation, which is composed of intermediate to acid rocks (rhyodacite), originated 131 million years ago during a vo1canic fissural event of continental extension. The rocks are grayish mesocratic and show fine granular to microphaneritic texture. The area cultivated with vineyards in the Pinto Bandeira geographical indication is located on higher altitudes and lower slopes terrains, on the tops of the plateaus, occupied by rocks of Caxias Facies. Soils formed on parent material of the Caxias Facies are a set of argisoils, cambisoils and nitosoils. To integrate the information was prepared a base map in O1S for zoning studies and also to spatializing different descriptors of natural factors. To construct the geological sketch, photo-interpretation techniques were employed high-resolution aerial photos associated with field work. The digital image processing was used to construct the digital elevation model from high resolution orbital data and its derivatives such as altimetry, slope and exposure, as well as the geological structures and land forms. MenosIn Brazil, studies of zoning in wine have contributed to the development of geographical indications. As for the geographical identity, the geology of the criteria has been a subject of research. The region of the Serra Gaúcha, located in northeastem Rio Grande do Sul, Brazil, has a geodiversity that induce the formation of soils and terrain, comprising natural and cultural factors that imply different responses of agronomic vine. These features value the production of wines with unique qualities, which can define different terroirs. The region is at the limit of the geomorphologic units Serra Geral and Planalto dos Campos Gerais, generated from the rocks of the Serra Geral Formation. ln the Pinto Bandeira geographical indication for fine wines occurs in the most of area, the Caxias Facies of Serra Geral Formation, which is composed of intermediate to acid rocks (rhyodacite), originated 131 million years ago during a vo1canic fissural event of continental extension. The rocks are grayish mesocratic and show fine granular to microphaneritic texture. The area cultivated with vineyards in the Pinto Bandeira geographical indication is located on higher altitudes and lower slopes terrains, on the tops of the plateaus, occupied by rocks of Caxias Facies. Soils formed on parent material of the Caxias Facies are a set of argisoils, cambisoils and nitosoils. To integrate the information was prepared a base map in O1S for zoning studies and also to spatializing different descriptors o... Mostrar Tudo |
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Palavras-Chave: |
Geology and wine; Indicação geográfica; Pinto Bandeira; Rio Grande do Sul; Wine terroir; Zoneamento. |
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Thesagro: |
Enologia; Uva; Viticultura. |
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Categoria do assunto: |
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P Recursos Naturais, Ciências Ambientais e da Terra |
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URL: |
https://ainfo.cnptia.embrapa.br/digital/bitstream/doc/1157182/1/Hoff-8-41.pdf
https://ainfo.cnptia.embrapa.br/digital/bitstream/item/61773/1/41-HOFF.pdf
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Marc: |
LEADER 02690nam a2200253 a 4500
001 2157182
005 2023-10-10
008 2012 bl uuuu u00u1 u #d
100 1 $aHOFF, R.
245 $aThe geology in the context of geographical indications of fine wines in Serra Gaúcha region (Brazil).$h[electronic resource]
260 $aCONGRES DES TERROIRS VITIVINICOLES. 9., 2012, Bourgogne, France. Actes... Bourgogne, Dijon; Champgne, Reims, CIVC, 25 a 29 Juin 2012.$c2012
300 $a8-41
520 $aIn Brazil, studies of zoning in wine have contributed to the development of geographical indications. As for the geographical identity, the geology of the criteria has been a subject of research. The region of the Serra Gaúcha, located in northeastem Rio Grande do Sul, Brazil, has a geodiversity that induce the formation of soils and terrain, comprising natural and cultural factors that imply different responses of agronomic vine. These features value the production of wines with unique qualities, which can define different terroirs. The region is at the limit of the geomorphologic units Serra Geral and Planalto dos Campos Gerais, generated from the rocks of the Serra Geral Formation. ln the Pinto Bandeira geographical indication for fine wines occurs in the most of area, the Caxias Facies of Serra Geral Formation, which is composed of intermediate to acid rocks (rhyodacite), originated 131 million years ago during a vo1canic fissural event of continental extension. The rocks are grayish mesocratic and show fine granular to microphaneritic texture. The area cultivated with vineyards in the Pinto Bandeira geographical indication is located on higher altitudes and lower slopes terrains, on the tops of the plateaus, occupied by rocks of Caxias Facies. Soils formed on parent material of the Caxias Facies are a set of argisoils, cambisoils and nitosoils. To integrate the information was prepared a base map in O1S for zoning studies and also to spatializing different descriptors of natural factors. To construct the geological sketch, photo-interpretation techniques were employed high-resolution aerial photos associated with field work. The digital image processing was used to construct the digital elevation model from high resolution orbital data and its derivatives such as altimetry, slope and exposure, as well as the geological structures and land forms.
650 $aEnologia
650 $aUva
650 $aViticultura
653 $aGeology and wine
653 $aIndicação geográfica
653 $aPinto Bandeira
653 $aRio Grande do Sul
653 $aWine terroir
653 $aZoneamento
700 1 $aFALCADE, I.
700 1 $aTONIETTO, J.
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Registro original: |
Embrapa Uva e Vinho (CNPUV) |
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 | Acesso ao texto completo restrito à biblioteca da Embrapa Amazônia Ocidental. Para informações adicionais entre em contato com cpaa.biblioteca@embrapa.br. |
Registro Completo
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Biblioteca(s): |
Embrapa Amazônia Ocidental; Embrapa Florestas. |
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Data corrente: |
03/01/2017 |
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Data da última atualização: |
11/07/2017 |
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Tipo da produção científica: |
Artigo em Periódico Indexado |
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Circulação/Nível: |
B - 1 |
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Autoria: |
CUNHA, L.; BROWN, G. G.; STANTON, D. W. G.; SILVA, E. da; HANSEL, F. A.; JORGE, G.; MCKEY, D.; VIDAL-TORRADO, P.; MACEDO, R. S.; VELASQUEZ, E.; JAMES, S. W.; LAVELLE, P.; KILLE, P. |
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Afiliação: |
Luis Cunha, Cardiff University / Embrapa Florestas; GEORGE GARDNER BROWN, CNPF; David W. G. Stanton, Cardiff University; Elodie Da Silva, Pós-doutoranda da Embrapa Florestas; FABRICIO AUGUSTO HANSEL, CNPF; Gabriella Jorge, Universidad de la República; Doyle McKey, CEFE - Université de Montpellier; Pablo Vidal-Torrado, ESALQ; Rodrigo S. Macedo, ESALQ; Elena Velasquez, Universidad Nacional de Colombia; Samuel W. James, University of Iowa; Patrick Lavelle, Institut de Recherche pour le Développement; Peter Kille, Cardiff University. |
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Título: |
Soil animals and pedogenesis: the role of earthworms in anthropogenic soils. |
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Ano de publicação: |
2016 |
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Fonte/Imprenta: |
Soil Science, v. 181, n. 3/4, p. 110-125, Mar./Apr. 2016. |
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DOI: |
10.1097/SS.0000000000000144 |
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Idioma: |
Inglês |
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Notas: |
Participação da Terra Preta de Índio Network. |
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Conteúdo: |
The role of earthworms as one of the most important groups of ecosystem engineers in human-modified and natural environments has been increasingly recognized only during the last 30 years, yet earthworms and humans have been acting together in building landscapes for millennia. This relationship is well represented in the pre-Columbian raised fields, in flood-prone savannas around the rim of Amazonia, but also by the potentially significant role of earthworms in the formation and resilience of Amazonian Dark Earths. Through the bioturbating action of earthworms, soil is biologically, chemically, and physically altered; nutrients are translocated; organic matter is decomposed and transformed; and the surrounding biota interacts as a large orchestra where the soil musicians play together on the various instruments but where earthworms take a leading role, enhancing microbial activity and generally stimulating plant growth. In this article, we assess the remarkable role of earthworms at the center of soil pedogenetic processes within anthropogenic landscapes, dissecting their functions with a special focus on Amazonian Dark Earths. |
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Palavras-Chave: |
Amazonian Dark Earths; Ciclagem de nutrientes; Formação do solo; Terra Preta de Índio. |
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Thesagro: |
Minhoca; Solo. |
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Thesaurus NAL: |
Biogeochemical cycles; Bioturbation; Earthworms; Soil formation. |
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Categoria do assunto: |
P Recursos Naturais, Ciências Ambientais e da Terra |
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Marc: |
LEADER 02307naa a2200409 a 4500
001 2059807
005 2017-07-11
008 2016 bl uuuu u00u1 u #d
024 7 $a10.1097/SS.0000000000000144$2DOI
100 1 $aCUNHA, L.
245 $aSoil animals and pedogenesis$bthe role of earthworms in anthropogenic soils.$h[electronic resource]
260 $c2016
500 $aParticipação da Terra Preta de Índio Network.
520 $aThe role of earthworms as one of the most important groups of ecosystem engineers in human-modified and natural environments has been increasingly recognized only during the last 30 years, yet earthworms and humans have been acting together in building landscapes for millennia. This relationship is well represented in the pre-Columbian raised fields, in flood-prone savannas around the rim of Amazonia, but also by the potentially significant role of earthworms in the formation and resilience of Amazonian Dark Earths. Through the bioturbating action of earthworms, soil is biologically, chemically, and physically altered; nutrients are translocated; organic matter is decomposed and transformed; and the surrounding biota interacts as a large orchestra where the soil musicians play together on the various instruments but where earthworms take a leading role, enhancing microbial activity and generally stimulating plant growth. In this article, we assess the remarkable role of earthworms at the center of soil pedogenetic processes within anthropogenic landscapes, dissecting their functions with a special focus on Amazonian Dark Earths.
650 $aBiogeochemical cycles
650 $aBioturbation
650 $aEarthworms
650 $aSoil formation
650 $aMinhoca
650 $aSolo
653 $aAmazonian Dark Earths
653 $aCiclagem de nutrientes
653 $aFormação do solo
653 $aTerra Preta de Índio
700 1 $aBROWN, G. G.
700 1 $aSTANTON, D. W. G.
700 1 $aSILVA, E. da
700 1 $aHANSEL, F. A.
700 1 $aJORGE, G.
700 1 $aMCKEY, D.
700 1 $aVIDAL-TORRADO, P.
700 1 $aMACEDO, R. S.
700 1 $aVELASQUEZ, E.
700 1 $aJAMES, S. W.
700 1 $aLAVELLE, P.
700 1 $aKILLE, P.
773 $tSoil Science$gv. 181, n. 3/4, p. 110-125, Mar./Apr. 2016.
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Embrapa Florestas (CNPF) |
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