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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: |
20/10/2016 |
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Tipo da produção científica: |
Artigo em Anais de Congresso |
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Autoria: |
TONIETTO, J.; SOTÉS RUIZ, V.; MONTES, C.; MARTÍN ULIARTE, E.; ANTELO BRUNO, L.; CLÍMACO, P.; PÉREZ ACEVEDO, Y.; VALENZUELA-SOLANO, C.; HATTA SAKODA, B.; CARBONNEAU, A. |
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Afiliação: |
JORGE TONIETTO, CNPUV; Vicente SOTÉS RUIZ, UPM - Universidad Politécnica de Madrid, Spain; Carlo MONTES, CEAZA - Centro de Estudios Avanzados en Zonas Áridas, Chile; Ernesto MARTÍN ULIARTE, INTA - EEA Mendoza, Argentina; Luis ANTELO BRUNO, PFCUVS-FAUTAPO, Desarrollo de Mercados, Bolivia; Pedro CLÍMACO, Instituto Nacional de Recursos Biológicos, I.P., INIA - Dois Portos, Portugal; Yenia PÉREZ ACEVEDO, Instituto de Investigaciones en Fruticultura Tropical, Cuba; César VALENZUELA-SOLANO, Instituto Nacional de Investigaciones Forestales, Agrícolas y Pecuarias – INIFAP, México; Beatriz HATTA SAKODA, Universidad Nacional Agraria La Molina, Peru; Alain CARBONNEAU, AGRO Montpellier, France. |
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Título: |
Climatic groups in Ibero-America viticulture compared to worldwide wine producer regions. |
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Ano de publicação: |
2012 |
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Fonte/Imprenta: |
In: CONGRES DES TERROIRS VITIVINICOLES, 9., 2012, Bourgogne/Champagne. [Annales...] [S.l.: s.n.], 2012. |
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Descrição Física: |
1 pendrive. |
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Idioma: |
Português |
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Conteúdo: |
The wine production is an important activity in many Ibero-American countries. The wine producer regions of these countries configure a large use of different climate types and viticultural climates. In a vitivinicultural zoning project of CYTED (Ibero-American Program for Science, Technology and Development), a viticultural climatic characterization was done in this macro viticultural region. The project have assembled a climatic database that characterizes the viticultural regions, including relevant variables for viticulture: air temperature (mean, maximum, and minimum), precipitation, relative humidity, solar radiation, number of sunshine hours, wind speed, and evapotranspiration. Using indices of the Geoviticulture MCC System (HI, CI and DI), more than 70 viticultural regions in different countries (Argentina, Bolivia, Brazil, Chile, Cuba, Spain, Mexico, Peru, Portugal and Uruguay) were characterized according to its viticultural climatic. The results, which will be integrated to the worldwide database of the MCC System, showed that the Ibero-American viticulture is placed in a wide range of climatic groups of the wine producing regions around the world. This article presents the climatic groups found in Ibero-America, identifying also some new climatic groups not yet found in other regions of the world. This work also identifies some climatic groups not found in Ibero-America viticulture. The research has also highlighted viticultural areas characterized by climates with ?intra-annual climatic variability?, with the potential to produce more than one growing cycle per year. The results allow to conclude that the wide variability and climatic diversity present in Ibero-America may be one of the reasons to explain the diversity in terms of wine types, sensorial characteristics, typicity and uniqueness of wines produced on this macro-region. MenosThe wine production is an important activity in many Ibero-American countries. The wine producer regions of these countries configure a large use of different climate types and viticultural climates. In a vitivinicultural zoning project of CYTED (Ibero-American Program for Science, Technology and Development), a viticultural climatic characterization was done in this macro viticultural region. The project have assembled a climatic database that characterizes the viticultural regions, including relevant variables for viticulture: air temperature (mean, maximum, and minimum), precipitation, relative humidity, solar radiation, number of sunshine hours, wind speed, and evapotranspiration. Using indices of the Geoviticulture MCC System (HI, CI and DI), more than 70 viticultural regions in different countries (Argentina, Bolivia, Brazil, Chile, Cuba, Spain, Mexico, Peru, Portugal and Uruguay) were characterized according to its viticultural climatic. The results, which will be integrated to the worldwide database of the MCC System, showed that the Ibero-American viticulture is placed in a wide range of climatic groups of the wine producing regions around the world. This article presents the climatic groups found in Ibero-America, identifying also some new climatic groups not yet found in other regions of the world. This work also identifies some climatic groups not found in Ibero-America viticulture. The research has also highlighted viticultural areas characterized by climates wi... Mostrar Tudo |
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Palavras-Chave: |
Iberoamérica; Produção mundial. |
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Thesagro: |
Clima; Mercado; Producao; Uva; Vinho; Viticultura. |
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Categoria do assunto: |
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URL: |
https://www.alice.cnptia.embrapa.br/alice/bitstream/doc/927783/1/03TONIETTO.pdf
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Marc: |
LEADER 02827nam a2200325 a 4500
001 1927783
005 2016-10-20
008 2012 bl uuuu u00u1 u #d
100 1 $aTONIETTO, J.
245 $aClimatic groups in Ibero-America viticulture compared to worldwide wine producer regions.$h[electronic resource]
260 $aIn: CONGRES DES TERROIRS VITIVINICOLES, 9., 2012, Bourgogne/Champagne. [Annales...] [S.l.: s.n.], 2012.$c2012
300 $c1 pendrive.
520 $aThe wine production is an important activity in many Ibero-American countries. The wine producer regions of these countries configure a large use of different climate types and viticultural climates. In a vitivinicultural zoning project of CYTED (Ibero-American Program for Science, Technology and Development), a viticultural climatic characterization was done in this macro viticultural region. The project have assembled a climatic database that characterizes the viticultural regions, including relevant variables for viticulture: air temperature (mean, maximum, and minimum), precipitation, relative humidity, solar radiation, number of sunshine hours, wind speed, and evapotranspiration. Using indices of the Geoviticulture MCC System (HI, CI and DI), more than 70 viticultural regions in different countries (Argentina, Bolivia, Brazil, Chile, Cuba, Spain, Mexico, Peru, Portugal and Uruguay) were characterized according to its viticultural climatic. The results, which will be integrated to the worldwide database of the MCC System, showed that the Ibero-American viticulture is placed in a wide range of climatic groups of the wine producing regions around the world. This article presents the climatic groups found in Ibero-America, identifying also some new climatic groups not yet found in other regions of the world. This work also identifies some climatic groups not found in Ibero-America viticulture. The research has also highlighted viticultural areas characterized by climates with ?intra-annual climatic variability?, with the potential to produce more than one growing cycle per year. The results allow to conclude that the wide variability and climatic diversity present in Ibero-America may be one of the reasons to explain the diversity in terms of wine types, sensorial characteristics, typicity and uniqueness of wines produced on this macro-region.
650 $aClima
650 $aMercado
650 $aProducao
650 $aUva
650 $aVinho
650 $aViticultura
653 $aIberoamérica
653 $aProdução mundial
700 1 $aSOTÉS RUIZ, V.
700 1 $aMONTES, C.
700 1 $aMARTÍN ULIARTE, E.
700 1 $aANTELO BRUNO, L.
700 1 $aCLÍMACO, P.
700 1 $aPÉREZ ACEVEDO, Y.
700 1 $aVALENZUELA-SOLANO, C.
700 1 $aHATTA SAKODA, B.
700 1 $aCARBONNEAU, A.
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Registro original: |
Embrapa Uva e Vinho (CNPUV) |
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Registro Completo
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Biblioteca(s): |
Embrapa Florestas. |
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Data corrente: |
19/09/2008 |
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Data da última atualização: |
19/09/2008 |
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Autoria: |
HASSALL, M.; WARD, N. |
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Título: |
Effects of climate change on faunal stimulation of CO2 emissions from soils. |
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Ano de publicação: |
2008 |
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Fonte/Imprenta: |
In: INTERNATIONAL COLLOQUIUM ON SOIL ZOOLOGY, 15; INTERNATIONAL COLLOQUIUM ON APTERYGOTA, 12., 2008, Curitiba. Biodiversity, conservation and sustainabele management of soil animal: abstracts. Colombo: Embrapa Florestas. Editors: George Gardner Brown; Klaus Dieter Sautter; Renato Marques; Amarildo Pasini. 1 CD-ROM. |
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Idioma: |
Inglês |
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Conteúdo: |
Ten times as much CO2 is currently emitted from the world?s soils as from all anthropogenic
sources combined. It follows that a 1% change in CO2 output from soils would have a greater
effect on atmospheric concentrations than the all the changes proposed in the Kyoto protocol
combined together. The potential for positive feedback resulting from increased microbial
metabolism in the soil resulting from climate change is very high but changes in soil metabolism
are also the least well understood part of how the whole global C cycle will respond to the effects
of climate change. What is known, as a result of decades of Soil Zoology, is that microbial
activity is strongly regulated by soil animals (Hassall et al. 2006), partly because of the ?Sleeping
Beauty paradox? (Lavelle et al 1995).
If the faunal regulators are affected differently to the microbes by climate change then predictions
from current models of the global carbon cycle are likely to be erroneous. The life cycles, metabolic
pathways, ecology and physiology of animals are so different to those of microbes they are very
unlikely to respond in the same way, particularly to future changes in precipitation, which in
many regions is predicted to involve both changes in both intensity and periodicity.
Soil animals will respond to these changes by alterations in the trade-off between times spent
feeding and sheltering, the degree to which they aggregate, their life histories and population
processes. Particularly good arthropod macro-decomposers for investigating these responses
are the terrestrial isopods for which all of these attributes have been thoroughly studied under
current climate conditions.
In this paper we report results of testing the hypotheses that a) intensity and b) periodicity of
rainfall and c) differences in relative humidity will affect feeding, sheltering and aggregating
behaviour, life history traits, growth and survivorship rates of terrestrial isopods. We further
hypothesise that different species will respond differently to experimental simulations of climate
change due to macro-evolutionary differences between species, particularly their different
physiological, morphological and behavioural adaptations to desiccation stress.. We go on to
test the hypothesis that different ecotypes of one species, from different parts of its geographical
range with different regional climates, will respond differently to alterations in patterns of
precipitation. Results from this experiment will help to answer the question of whether organisms
are likely to respond differently to climate change in different parts of their range as a result of
micro-evolutionary adaptations to different local climates
Finally we report on how responses of this group of soil animals to experimentally manipulated
micro-climates affect the extent to which they stimulate microbial metabolism, and subsequently
soil CO2 emissions. MenosTen times as much CO2 is currently emitted from the world?s soils as from all anthropogenic
sources combined. It follows that a 1% change in CO2 output from soils would have a greater
effect on atmospheric concentrations than the all the changes proposed in the Kyoto protocol
combined together. The potential for positive feedback resulting from increased microbial
metabolism in the soil resulting from climate change is very high but changes in soil metabolism
are also the least well understood part of how the whole global C cycle will respond to the effects
of climate change. What is known, as a result of decades of Soil Zoology, is that microbial
activity is strongly regulated by soil animals (Hassall et al. 2006), partly because of the ?Sleeping
Beauty paradox? (Lavelle et al 1995).
If the faunal regulators are affected differently to the microbes by climate change then predictions
from current models of the global carbon cycle are likely to be erroneous. The life cycles, metabolic
pathways, ecology and physiology of animals are so different to those of microbes they are very
unlikely to respond in the same way, particularly to future changes in precipitation, which in
many regions is predicted to involve both changes in both intensity and periodicity.
Soil animals will respond to these changes by alterations in the trade-off between times spent
feeding and sheltering, the degree to which they aggregate, their life histories and population
processes. Particularly good arth... Mostrar Tudo |
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Categoria do assunto: |
-- |
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Marc: |
LEADER 03560naa a2200133 a 4500
001 1314881
005 2008-09-19
008 2008 bl uuuu u00u1 u #d
100 1 $aHASSALL, M.
245 $aEffects of climate change on faunal stimulation of CO2 emissions from soils.
260 $c2008
520 $aTen times as much CO2 is currently emitted from the world?s soils as from all anthropogenic sources combined. It follows that a 1% change in CO2 output from soils would have a greater effect on atmospheric concentrations than the all the changes proposed in the Kyoto protocol combined together. The potential for positive feedback resulting from increased microbial metabolism in the soil resulting from climate change is very high but changes in soil metabolism are also the least well understood part of how the whole global C cycle will respond to the effects of climate change. What is known, as a result of decades of Soil Zoology, is that microbial activity is strongly regulated by soil animals (Hassall et al. 2006), partly because of the ?Sleeping Beauty paradox? (Lavelle et al 1995). If the faunal regulators are affected differently to the microbes by climate change then predictions from current models of the global carbon cycle are likely to be erroneous. The life cycles, metabolic pathways, ecology and physiology of animals are so different to those of microbes they are very unlikely to respond in the same way, particularly to future changes in precipitation, which in many regions is predicted to involve both changes in both intensity and periodicity. Soil animals will respond to these changes by alterations in the trade-off between times spent feeding and sheltering, the degree to which they aggregate, their life histories and population processes. Particularly good arthropod macro-decomposers for investigating these responses are the terrestrial isopods for which all of these attributes have been thoroughly studied under current climate conditions. In this paper we report results of testing the hypotheses that a) intensity and b) periodicity of rainfall and c) differences in relative humidity will affect feeding, sheltering and aggregating behaviour, life history traits, growth and survivorship rates of terrestrial isopods. We further hypothesise that different species will respond differently to experimental simulations of climate change due to macro-evolutionary differences between species, particularly their different physiological, morphological and behavioural adaptations to desiccation stress.. We go on to test the hypothesis that different ecotypes of one species, from different parts of its geographical range with different regional climates, will respond differently to alterations in patterns of precipitation. Results from this experiment will help to answer the question of whether organisms are likely to respond differently to climate change in different parts of their range as a result of micro-evolutionary adaptations to different local climates Finally we report on how responses of this group of soil animals to experimentally manipulated micro-climates affect the extent to which they stimulate microbial metabolism, and subsequently soil CO2 emissions.
700 1 $aWARD, N.
773 $tIn: INTERNATIONAL COLLOQUIUM ON SOIL ZOOLOGY, 15; INTERNATIONAL COLLOQUIUM ON APTERYGOTA, 12., 2008, Curitiba. Biodiversity, conservation and sustainabele management of soil animal: abstracts. Colombo: Embrapa Florestas. Editors: George Gardner Brown; Klaus Dieter Sautter; Renato Marques; Amarildo Pasini. 1 CD-ROM.
Download
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