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Registro Completo |
Biblioteca(s): |
Embrapa Meio Ambiente. |
Data corrente: |
09/08/2006 |
Data da última atualização: |
17/02/2009 |
Autoria: |
GUIMARÃES, A. P. |
Título: |
A crise agrária. |
Edição: |
3.ed. |
Ano de publicação: |
1982 |
Fonte/Imprenta: |
Rio de Janeiro: Paz e Terra, 1982. |
Páginas: |
362p. |
Idioma: |
Português |
Conteúdo: |
Da revolução agrícola a revolução industrial. A revolução agrícola no Brasil. O processo de industrialização da agricultura. O complexo agroindustrial. Limitações ao crescimento agrícola. A escassez de alimentos e o agropoder. A força humana na agricultura. Futuro da agricultura brasileira. |
Palavras-Chave: |
Brasil. |
Thesagro: |
Agricultura; Industrialização. |
Thesaurus Nal: |
agribusiness. |
Categoria do assunto: |
-- |
Marc: |
LEADER 00721nam a2200181 a 4500 001 1014911 005 2009-02-17 008 1982 bl uuuu 00u1 u #d 100 1 $aGUIMARÃES, A. P. 245 $aA crise agrária. 250 $a3.ed. 260 $aRio de Janeiro: Paz e Terra$c1982 300 $a362p. 520 $aDa revolução agrícola a revolução industrial. A revolução agrícola no Brasil. O processo de industrialização da agricultura. O complexo agroindustrial. Limitações ao crescimento agrícola. A escassez de alimentos e o agropoder. A força humana na agricultura. Futuro da agricultura brasileira. 650 $aagribusiness 650 $aAgricultura 650 $aIndustrialização 653 $aBrasil
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Registro Completo
Biblioteca(s): |
Embrapa Solos. |
Data corrente: |
14/10/2011 |
Data da última atualização: |
03/11/2021 |
Tipo da produção científica: |
Artigo em Periódico Indexado |
Circulação/Nível: |
A - 1 |
Autoria: |
FRASER, J.; TEIXEIRA, W. G.; FALCÃO, N.; WOODS, W.; LEHMANN, J.; JUNQUEIRA, A. B. |
Afiliação: |
James Fraser, University Sussex; WENCESLAU GERALDES TEIXEIRA, CNPS; Newton Falcão, Instituto Nacional de Pesquisas da Amazônia; William Woods, University of Kansas; Johannes Lehmann, Cornell University; André Braga Junqueira, Instituto Nacional de Pesquisas da Amazônia. |
Título: |
Anthropogenic soils in the Central Amazon: from categories to a continuum. |
Ano de publicação: |
2011 |
Fonte/Imprenta: |
Area, v. 43, n. 3, p. 264-273, May 2011. |
DOI: |
https://doi.org/10.1111/j.1475-4762.2011.00999.x |
Idioma: |
Inglês |
Conteúdo: |
Amazonian Dark Earths (ADE), one of the best-known examples of anthropogenic (man-made) soils, are the result of Amerindian settlements in the pre-Columbian period. ADE are highly variable in terms of their size, shape, depth and physical and chemical make-up. Scholars tend to divide ADE into two categories: terra preta and terra mulata. The former are dark and highly fertile soils replete with ceramic shards, indicating former areas of habitation, while the latter are lighter in colour, less fertile, lacking pottery and thought to be old agricultural fields. While a scientific consensus on the origins of terra preta has existed for several decades, the origins of terra mulata remain enigmatic and contested. We argue that owing to the overlapping and constantly changing boundaries of agricultural and habitational areas, it is unlikely that there exist two clear soil fertility classes. This article examines the hypothesis that rather than two distinct anthrosol categories, ADE sites should exhibit a highly fertile 'core area', which grades into more subtly modified soils, with a continuum of fertility between them. Using principal components analysis (PCA) and interpolations based on the geographic distribution of the soil samples, we show that ADE along the Middle Madeira, Brazilian Amazon are extremely diverse, but data support more of a gradient between areas of greater and lesser fertility rather than two distinct categories. We also assess local people's perceptions and classifications of anthropogenic and surrounding soils using ethnographic data. Rather than discarding the terra preta-terra mulata opposition however, we suggest abandoning only the idea that they are separate categories, and instead emphasise a continuum, the darker, bluff edge 'central' regions with abundant ceramics are consonant with published descriptions of terra preta, which grade into surrounding areas with lighter, less fertile soils that better fit terra mulata descriptions. MenosAmazonian Dark Earths (ADE), one of the best-known examples of anthropogenic (man-made) soils, are the result of Amerindian settlements in the pre-Columbian period. ADE are highly variable in terms of their size, shape, depth and physical and chemical make-up. Scholars tend to divide ADE into two categories: terra preta and terra mulata. The former are dark and highly fertile soils replete with ceramic shards, indicating former areas of habitation, while the latter are lighter in colour, less fertile, lacking pottery and thought to be old agricultural fields. While a scientific consensus on the origins of terra preta has existed for several decades, the origins of terra mulata remain enigmatic and contested. We argue that owing to the overlapping and constantly changing boundaries of agricultural and habitational areas, it is unlikely that there exist two clear soil fertility classes. This article examines the hypothesis that rather than two distinct anthrosol categories, ADE sites should exhibit a highly fertile 'core area', which grades into more subtly modified soils, with a continuum of fertility between them. Using principal components analysis (PCA) and interpolations based on the geographic distribution of the soil samples, we show that ADE along the Middle Madeira, Brazilian Amazon are extremely diverse, but data support more of a gradient between areas of greater and lesser fertility rather than two distinct categories. We also assess local people's perceptions and ... Mostrar Tudo |
Palavras-Chave: |
Amazonian Dark Earths; Interpolação; Terra mulata. |
Thesaurus NAL: |
terra preta. |
Categoria do assunto: |
P Recursos Naturais, Ciências Ambientais e da Terra |
Marc: |
LEADER 02690naa a2200241 a 4500 001 1903130 005 2021-11-03 008 2011 bl uuuu u00u1 u #d 024 7 $ahttps://doi.org/10.1111/j.1475-4762.2011.00999.x$2DOI 100 1 $aFRASER, J. 245 $aAnthropogenic soils in the Central Amazon$bfrom categories to a continuum.$h[electronic resource] 260 $c2011 520 $aAmazonian Dark Earths (ADE), one of the best-known examples of anthropogenic (man-made) soils, are the result of Amerindian settlements in the pre-Columbian period. ADE are highly variable in terms of their size, shape, depth and physical and chemical make-up. Scholars tend to divide ADE into two categories: terra preta and terra mulata. The former are dark and highly fertile soils replete with ceramic shards, indicating former areas of habitation, while the latter are lighter in colour, less fertile, lacking pottery and thought to be old agricultural fields. While a scientific consensus on the origins of terra preta has existed for several decades, the origins of terra mulata remain enigmatic and contested. We argue that owing to the overlapping and constantly changing boundaries of agricultural and habitational areas, it is unlikely that there exist two clear soil fertility classes. This article examines the hypothesis that rather than two distinct anthrosol categories, ADE sites should exhibit a highly fertile 'core area', which grades into more subtly modified soils, with a continuum of fertility between them. Using principal components analysis (PCA) and interpolations based on the geographic distribution of the soil samples, we show that ADE along the Middle Madeira, Brazilian Amazon are extremely diverse, but data support more of a gradient between areas of greater and lesser fertility rather than two distinct categories. We also assess local people's perceptions and classifications of anthropogenic and surrounding soils using ethnographic data. Rather than discarding the terra preta-terra mulata opposition however, we suggest abandoning only the idea that they are separate categories, and instead emphasise a continuum, the darker, bluff edge 'central' regions with abundant ceramics are consonant with published descriptions of terra preta, which grade into surrounding areas with lighter, less fertile soils that better fit terra mulata descriptions. 650 $aterra preta 653 $aAmazonian Dark Earths 653 $aInterpolação 653 $aTerra mulata 700 1 $aTEIXEIRA, W. G. 700 1 $aFALCÃO, N. 700 1 $aWOODS, W. 700 1 $aLEHMANN, J. 700 1 $aJUNQUEIRA, A. B. 773 $tArea$gv. 43, n. 3, p. 264-273, May 2011.
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