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Registro Completo |
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Biblioteca(s): |
Embrapa Solos. |
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Data corrente: |
05/12/2022 |
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Data da última atualização: |
14/12/2022 |
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Tipo da produção científica: |
Capítulo em Livro Técnico-Científico |
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Autoria: |
ANGELINI, M. E.; FONTANA, A.; LANDI, A.; MERMUT, A. R.; MOREIRA, A. L.; LOPATKA, A.; LABAZ, B.; IRINA, B.; VANDENBYGAART, B.; OLGA, B.; PÁLKA, B.; SMRECZAK, B.; CLERICI, C.; PINHEIRO JÚNIOR, C. R.; FERGUSON, C.; OLGA, C.; VAN HUYSSTEEN, C. W.; MONGER, C.; WEI, D.; RODRÍGUEZ, D. M.; LINDBO, D.; NURSYAMSI, D.; CAHYANA, D.; BEAUDETTE, D.; NUREMBERG, E.; LIU, F.; FONTES, F.; OLIVEIRA, F. P. de; ZHANG, G.; OLEG, G.; PEREIRA, G.; SCHULZ, G.; VASQUES, G. M.; IAAICH, H.; MORRÁS, H. J. M.; HUSEIN, H. H.; GUTIÉRREZ DÍAZ, J. S.; IVELIC-SÁEZ, J.; KOBZA, J.; FUENTE, J. C. de la; HE, J.; NIKOLAI, K.; RODRÍGUEZ JIMÉNEZ, L. M.; WANG, L.; TENTI VUEGEN, L.; JIN, L.; MORETTI, L. M.; ANJOS, L. H. C. dos; SANTOS, L. A. C. dos; PFEIFFER, M.; PEREIRA, M. G.; GUEVARA SANTAMARIA, M.; BOLAÑOS-BENAVIDES, M.; DELL'ACQUA, M.; SAKSA, M.; COELHO, M. R.; CAMPOS, M. C. C.; NEVENA, M.; ORDOÑEZ DELGADO, N.; BATKHISHIG, O.; SERRATO ALCAREZ, P. K.; MOUSSSADEK, R.; DART, R. de O.; DALMOLIN, R. S. D.; OROZAKUNOVA, R.; RADIC, S.; TOMA, S.; WILLS, S. A.; ROECKER, S.; VALLE, S.; KIENAST-BROWN, S.; NAKISKO, S.; KUYPER, T. W.; SOLOVEI, V.; IVAN, V.; CHERLINKA, V.; MORA, V. R. de la; LEBED, V.; CARDONA, W. A.; GENG, X.; LI, Y.; ZHANG, Y.; SULAEMAN, Y.; ZALAVSKYI, Y.; YIGINI, Y.; TAKATA, Y.; SUN, Z. |
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Afiliação: |
MARCOS ESTEBAN ANGELINI, FAO-GLOBAL SOIL PARTNERSHIP; ADEMIR FONTANA, CNPS; AHMAD LANDI; AHMET R. MERMUT; ANA LAURA MOREIRA; ARTUR LOPATKA; BEATA LABAZ; BELOZERTSEVA IRINA; BERT VANDENBYGAART; BEZUGLOVA OLGA; BORIS PÁLKA; BOZENA SMRECZAK; CARLOS CLERICI; CARLOS ROBERTO PINHEIRO JÚNIOR; CHARLES FERGUSON; CHERNOVA OLGA; CORNELIUS WILHELM VAN HUYSSTEEN; CURTIS MONGER; DAN WEI; DARÍO M. RODRÍGUEZ; DAVID LINDBO; DEDI NURSYAMSI; DESTIKA CAHYANA; DYLAN BEAUDETTE; ERLANGEN NUREMBERG; FENG LIU; FERNANDO FONTES; FLÁVIO PEREIRA DE OLIVEIRA; GANLIN ZHANG; GOLOZUBOV OLEG; GONZALO PEREIRA; GUILLERMO SCHULZ; GUSTAVO DE MATTOS VASQUES, CNPS; HAMZA IAAICH; HÉCTOR J. M. MORRÁS; HUSSAM HAG HUSEIN; JOAN SEBASTIAN GUTIÉRREZ DÍAZ; JORGE IVELIC-SÁEZ; JOZEF KOBZA; JUAN CARLOS DE LA FUENTE; JUANXIA HE; KHITROV NIKOLAI; LADY MARCELA RODRÍGUEZ JIMÉNEZ; LEI WANG; LEONARDO TENTI VUEGEN; LIANG JIN; LUCAS M. MORETTI; LÚCIA HELENA CUNHA DOS ANJOS, UNIVERSIDADE FEDERAL RURAL DO RIO DE JANEIRO; LUÍS ANTÔNIO COUTRIM DOS SANTOS; MARCO PFEIFFER; MARCOS GERVASIO PEREIRA, UNIVERSIDADE FEDERAL RURAL DO RIO DE JANEIRO; MARIO GUEVARA SANTAMARIA; MARTHA BOLAÑOS-BENAVIDES; MARTIN DELL'ACQUA; MARTIN SAKSA; MAURICIO RIZZATO COELHO, CNPS; MILTON CÉSAR COSTA CAMPOS; MITEVA NEVENA; NAPOLEÓN ORDOÑEZ DELGADO; OCHIRBAT BATKHISHIG; PEDRO KARIN SERRATO ALCAREZ; RACHID MOUSSSADEK; RICARDO DE OLIVEIRA DART, CNPS; RICARDO SIMÃO DINIZ DALMOLIN; ROZA OROZAKUNOVA; SERGIO RADIC; SHISHKOV TOMA; SKYE ANGELA WILLS; STEPHEN ROECKER; SUSANA VALLE; SUZANN KIENAST-BROWN; SVITLANA NAKISKO; THOMAS W. KUYPER; VADYM SOLOVEI; VASENEV IVAN; VASYL CHERLINKA; VERONICA REYNOSO DE LA MORA; VITALII LEBED; WILLIAM ANDRÉS CARDONA; XIAOYUAN GENG; YAN LI; YING ZHANG; YIYI SULAEMAN; YURII ZALAVSKYI; YUSUF YIGINI; YUSUKE TAKATA; ZHENG SUN. |
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Título: |
Global distribution and characteristics of black soils. |
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Ano de publicação: |
2022 |
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Fonte/Imprenta: |
In: FAO. Global status of black soils. Rome, 2022. cap. 2, p. 14-69. |
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Idioma: |
Inglês |
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Conteúdo: |
Definition of black soils; Creation of a global map of black soils; Global map of black soils; The nature of black soils; Regional characteristics of black soils. |
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Palavras-Chave: |
Black soils. |
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Categoria do assunto: |
P Recursos Naturais, Ciências Ambientais e da Terra |
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URL: |
https://ainfo.cnptia.embrapa.br/digital/bitstream/item/243413/1/Global-distribution-and-characteristics-of-black-soils-2022.pdf
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Marc: |
LEADER 03122naa a2201165 a 4500
001 2149223
005 2022-12-14
008 2022 bl uuuu u00u1 u #d
100 1 $aANGELINI, M. E.
245 $aGlobal distribution and characteristics of black soils.$h[electronic resource]
260 $c2022
520 $aDefinition of black soils; Creation of a global map of black soils; Global map of black soils; The nature of black soils; Regional characteristics of black soils.
653 $aBlack soils
700 1 $aFONTANA, A.
700 1 $aLANDI, A.
700 1 $aMERMUT, A. R.
700 1 $aMOREIRA, A. L.
700 1 $aLOPATKA, A.
700 1 $aLABAZ, B.
700 1 $aIRINA, B.
700 1 $aVANDENBYGAART, B.
700 1 $aOLGA, B.
700 1 $aPÁLKA, B.
700 1 $aSMRECZAK, B.
700 1 $aCLERICI, C.
700 1 $aPINHEIRO JÚNIOR, C. R.
700 1 $aFERGUSON, C.
700 1 $aOLGA, C.
700 1 $aVAN HUYSSTEEN, C. W.
700 1 $aMONGER, C.
700 1 $aWEI, D.
700 1 $aRODRÍGUEZ, D. M.
700 1 $aLINDBO, D.
700 1 $aNURSYAMSI, D.
700 1 $aCAHYANA, D.
700 1 $aBEAUDETTE, D.
700 1 $aNUREMBERG, E.
700 1 $aLIU, F.
700 1 $aFONTES, F.
700 1 $aOLIVEIRA, F. P. de
700 1 $aZHANG, G.
700 1 $aOLEG, G.
700 1 $aPEREIRA, G.
700 1 $aSCHULZ, G.
700 1 $aVASQUES, G. M.
700 1 $aIAAICH, H.
700 1 $aMORRÁS, H. J. M.
700 1 $aHUSEIN, H. H.
700 1 $aGUTIÉRREZ DÍAZ, J. S.
700 1 $aIVELIC-SÁEZ, J.
700 1 $aKOBZA, J.
700 1 $aFUENTE, J. C. de la
700 1 $aHE, J.
700 1 $aNIKOLAI, K.
700 1 $aRODRÍGUEZ JIMÉNEZ, L. M.
700 1 $aWANG, L.
700 1 $aTENTI VUEGEN, L.
700 1 $aJIN, L.
700 1 $aMORETTI, L. M.
700 1 $aANJOS, L. H. C. dos
700 1 $aSANTOS, L. A. C. dos
700 1 $aPFEIFFER, M.
700 1 $aPEREIRA, M. G.
700 1 $aGUEVARA SANTAMARIA, M.
700 1 $aBOLAÑOS-BENAVIDES, M.
700 1 $aDELL'ACQUA, M.
700 1 $aSAKSA, M.
700 1 $aCOELHO, M. R.
700 1 $aCAMPOS, M. C. C.
700 1 $aNEVENA, M.
700 1 $aORDOÑEZ DELGADO, N.
700 1 $aBATKHISHIG, O.
700 1 $aSERRATO ALCAREZ, P. K.
700 1 $aMOUSSSADEK, R.
700 1 $aDART, R. de O.
700 1 $aDALMOLIN, R. S. D.
700 1 $aOROZAKUNOVA, R.
700 1 $aRADIC, S.
700 1 $aTOMA, S.
700 1 $aWILLS, S. A.
700 1 $aROECKER, S.
700 1 $aVALLE, S.
700 1 $aKIENAST-BROWN, S.
700 1 $aNAKISKO, S.
700 1 $aKUYPER, T. W.
700 1 $aSOLOVEI, V.
700 1 $aIVAN, V.
700 1 $aCHERLINKA, V.
700 1 $aMORA, V. R. de la
700 1 $aLEBED, V.
700 1 $aCARDONA, W. A.
700 1 $aGENG, X.
700 1 $aLI, Y.
700 1 $aZHANG, Y.
700 1 $aSULAEMAN, Y.
700 1 $aZALAVSKYI, Y.
700 1 $aYIGINI, Y.
700 1 $aTAKATA, Y.
700 1 $aSUN, Z.
773 $tIn: FAO. Global status of black soils. Rome, 2022. cap. 2, p. 14-69.
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Registro original: |
Embrapa Solos (CNPS) |
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Registro |
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Registro Completo
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Biblioteca(s): |
Embrapa Pantanal. |
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Data corrente: |
05/12/2016 |
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Data da última atualização: |
25/07/2017 |
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Tipo da produção científica: |
Artigo em Periódico Indexado |
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Circulação/Nível: |
C - 0 |
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Autoria: |
BRASIL, M. da S.; SOUZA, M. S. T. de; OLIVEIRA, I. B. de; DANIEL, O.; SANTOS, S. A.; MARQUES, M. R.; SILVA, W. M. da. |
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Afiliação: |
MARIVAINE DA SILVA BRASIL, FEDERAL UNIVERSITY OF MATO GROSSO DO SUL/CPAN; MAYARA SILVA TORRES DE SOUZA, FEDERAL UNIVERSITY OF PARANÁ; IZABELA BRAGA DE OLIVEIRA, FEDERAL UNIVERSITY OF MATO GROSSO DO SUL/CPAN; OMAR DANIEL, FEDERAL UNIVERSITY OF THE GRANDE DOURADOS; SANDRA APARECIDA SANTOS, CPAP; MARIA RITA MARQUES, 5FEDERAL UNIVERSITY OF MATO GROSSO OF SUL/CCBS; WILLIAM MARCOS DA SILVA, FEDERAL UNIVERSITY OF MATO GROSSO DO SUL/CPAN. |
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Título: |
Influence of flood areas on the number of diazotrophic bacteria from pasture grasses. |
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Ano de publicação: |
2016 |
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Fonte/Imprenta: |
Applied Ecology and Environmental Sciences, v. 4, n. 4, p. 84-88, 2016. |
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DOI: |
10.12691 /aees-4-4-1 |
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Idioma: |
Inglês |
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Conteúdo: |
Floodplain areas are driven by flood pulse and with consequence, flood gradient are formed, such as, lakes, wetlands and dry areas. And this gradient is one of the most important forcing functions for animal and plant ecology that areas. The aim of this study is testing the hypothesis of the flood gradient in the bacteria diazotrophic association with grasses in their roots and shoots. The study was realized in the Pantanal of the Mato Grosso do Sul, in two periods, rainy (March, 2009) and dry (August, 2010) and the samples of grasses were made in different flood gradients areas: in dry, in seasonally flood and in permanent flooded. The number of bacteria in the roots and stems were counted using the most probable number method using the semi-solid media or semi-specific JNFb and the morphotypes identified using the type strains of Azospirillum and Herbaspirillum. The results show that the grasses presented no difference in roots and shoots and neither for the periods for bacteria number. The principal difference in number were recorded among genera of grasses, were the in grasses influenced by water of flood, the grasses Hymenachne amplexicaulis, Axonopus purpusii presented higher number of bacteria in its tissues and the grass Mesosetum chaseae found in the dry area presented lowest value. The morphotype found belong to three genera, Azospirillum and Herbaspirillum and non-identified genera. The Azospirillum and Herbaspirillum presented high number in grasses Hymenachne amplexicaulis of permanent flood areas and the non-identified genera presented high number in grasses Axonopus purpusii and Mesosetum chaseae dry and seasonally flood area. We conclude that flood gradient hypothesis is valid for association of diazotrophic bacteria and grasses for Pantanal floodplain in two ways: driven the grasses host species distribution along the gradient and the host driven number and bacteria population composition. MenosFloodplain areas are driven by flood pulse and with consequence, flood gradient are formed, such as, lakes, wetlands and dry areas. And this gradient is one of the most important forcing functions for animal and plant ecology that areas. The aim of this study is testing the hypothesis of the flood gradient in the bacteria diazotrophic association with grasses in their roots and shoots. The study was realized in the Pantanal of the Mato Grosso do Sul, in two periods, rainy (March, 2009) and dry (August, 2010) and the samples of grasses were made in different flood gradients areas: in dry, in seasonally flood and in permanent flooded. The number of bacteria in the roots and stems were counted using the most probable number method using the semi-solid media or semi-specific JNFb and the morphotypes identified using the type strains of Azospirillum and Herbaspirillum. The results show that the grasses presented no difference in roots and shoots and neither for the periods for bacteria number. The principal difference in number were recorded among genera of grasses, were the in grasses influenced by water of flood, the grasses Hymenachne amplexicaulis, Axonopus purpusii presented higher number of bacteria in its tissues and the grass Mesosetum chaseae found in the dry area presented lowest value. The morphotype found belong to three genera, Azospirillum and Herbaspirillum and non-identified genera. The Azospirillum and Herbaspirillum presented high number in grasses Hymenachne am... Mostrar Tudo |
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Palavras-Chave: |
Flood; Floodplain. |
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Thesagro: |
Graminea; Inundacao. |
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Thesaurus NAL: |
Grasses. |
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Categoria do assunto: |
P Recursos Naturais, Ciências Ambientais e da Terra |
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URL: |
https://ainfo.cnptia.embrapa.br/digital/bitstream/item/151253/1/grasses-santos.pdf
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Marc: |
LEADER 02701naa a2200265 a 4500
001 2057971
005 2017-07-25
008 2016 bl uuuu u00u1 u #d
024 7 $a10.12691 /aees-4-4-1$2DOI
100 1 $aBRASIL, M. da S.
245 $aInfluence of flood areas on the number of diazotrophic bacteria from pasture grasses.$h[electronic resource]
260 $c2016
520 $aFloodplain areas are driven by flood pulse and with consequence, flood gradient are formed, such as, lakes, wetlands and dry areas. And this gradient is one of the most important forcing functions for animal and plant ecology that areas. The aim of this study is testing the hypothesis of the flood gradient in the bacteria diazotrophic association with grasses in their roots and shoots. The study was realized in the Pantanal of the Mato Grosso do Sul, in two periods, rainy (March, 2009) and dry (August, 2010) and the samples of grasses were made in different flood gradients areas: in dry, in seasonally flood and in permanent flooded. The number of bacteria in the roots and stems were counted using the most probable number method using the semi-solid media or semi-specific JNFb and the morphotypes identified using the type strains of Azospirillum and Herbaspirillum. The results show that the grasses presented no difference in roots and shoots and neither for the periods for bacteria number. The principal difference in number were recorded among genera of grasses, were the in grasses influenced by water of flood, the grasses Hymenachne amplexicaulis, Axonopus purpusii presented higher number of bacteria in its tissues and the grass Mesosetum chaseae found in the dry area presented lowest value. The morphotype found belong to three genera, Azospirillum and Herbaspirillum and non-identified genera. The Azospirillum and Herbaspirillum presented high number in grasses Hymenachne amplexicaulis of permanent flood areas and the non-identified genera presented high number in grasses Axonopus purpusii and Mesosetum chaseae dry and seasonally flood area. We conclude that flood gradient hypothesis is valid for association of diazotrophic bacteria and grasses for Pantanal floodplain in two ways: driven the grasses host species distribution along the gradient and the host driven number and bacteria population composition.
650 $aGrasses
650 $aGraminea
650 $aInundacao
653 $aFlood
653 $aFloodplain
700 1 $aSOUZA, M. S. T. de
700 1 $aOLIVEIRA, I. B. de
700 1 $aDANIEL, O.
700 1 $aSANTOS, S. A.
700 1 $aMARQUES, M. R.
700 1 $aSILVA, W. M. da
773 $tApplied Ecology and Environmental Sciences$gv. 4, n. 4, p. 84-88, 2016.
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Embrapa Pantanal (CPAP) |
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