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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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Biblioteca(s): |
Embrapa Solos. |
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Data corrente: |
26/09/2013 |
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Data da última atualização: |
08/11/2021 |
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Tipo da produção científica: |
Resumo em Anais de Congresso |
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Autoria: |
OLIVEIRA, F.; SCHAEFER, C.; ABRAHÃO, W.; ALMEIDA, E. de P. C.; SIMAS, F. |
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Afiliação: |
Fábio OLIVEIRA; Carlos SCHAEFER; Walter ABRAHÃO; ELIANE DE PAULA CLEMENTE ALMEIDA, CNPS; Felipe SIMAS. |
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Título: |
Ornithogenic soil toposequence on Rata island, Fernando de Noronha archipelago, south atlantic and quaternary paleoclimatic implications. |
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Ano de publicação: |
2013 |
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Fonte/Imprenta: |
In: IAG INTERNACIONAL CONFERENCE GEOMORPHOLOGY, 8., 2013, Paris. Resumo... Frankfurt: Association Internacionale des Géomorphologues, 2013. |
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Idioma: |
Inglês |
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Conteúdo: |
The formation of highly phosphatized soils on sites of avian activity is a common feature of oceanic islands. We characterized a toposequence of phosphatic soils on Rata Island, to evaluate the soil genesis based on local topographic variations. For this purpose, four soils ranging from the upper hill down to the lowest landscape position on the island, representing a range of parent materials (basalt and calcareous sands), were analyzed. In the lowest landscape position a shallow Entisol was identified, strongly influenced by birds and marine sprays (Litholic Neosol), developed on " karstified" Pleistocene calcarenites; the three other soils in the upper part of the toposequence are Ornithogenic Inceptsols (Cambisols), ranging from a deep Cambisol profile on Basalt lava to intermediate Cambisols on mixed colluvial sediments of the basalt/calcareous. The lowermost Litholic Neosol is associated with a rugged landscape with strong calcarenite dissolution and karstification, related to a former wetter climate. The soil phosphatization is clearly an inherited process of the Late Quaternary age, when climate conditions were different. Initial weathering took place in the last interglacial period, under wetter conditions during which the Tertiary basalts were strongly weathered, leaving corestones in a saprolitic, oxidized mass. In the late Pleistocene, a gentle surface distributed these weathering products along the pediment slopes as colluvial materials, whereas in the coastal areas aeolian processes formed large sand dunes composed of reworked calcareous sands from marine sources during a time of very low sea level. During this time, widespread bird activity accounted for secondary apatite formation on the surface of calcareous oolites. Finally, the Holocene warming was accompanied by increasing sea level, enhanced tropical weathering, Fe and Al mobility and variscite formation superimposed on degraded Ca-phosphates, forming two phase phosphatic aggregates. MenosThe formation of highly phosphatized soils on sites of avian activity is a common feature of oceanic islands. We characterized a toposequence of phosphatic soils on Rata Island, to evaluate the soil genesis based on local topographic variations. For this purpose, four soils ranging from the upper hill down to the lowest landscape position on the island, representing a range of parent materials (basalt and calcareous sands), were analyzed. In the lowest landscape position a shallow Entisol was identified, strongly influenced by birds and marine sprays (Litholic Neosol), developed on " karstified" Pleistocene calcarenites; the three other soils in the upper part of the toposequence are Ornithogenic Inceptsols (Cambisols), ranging from a deep Cambisol profile on Basalt lava to intermediate Cambisols on mixed colluvial sediments of the basalt/calcareous. The lowermost Litholic Neosol is associated with a rugged landscape with strong calcarenite dissolution and karstification, related to a former wetter climate. The soil phosphatization is clearly an inherited process of the Late Quaternary age, when climate conditions were different. Initial weathering took place in the last interglacial period, under wetter conditions during which the Tertiary basalts were strongly weathered, leaving corestones in a saprolitic, oxidized mass. In the late Pleistocene, a gentle surface distributed these weathering products along the pediment slopes as colluvial materials, whereas in the coastal a... Mostrar Tudo |
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Palavras-Chave: |
Fernando de Noronha Archipelago; Ornithogenic soil. |
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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/90171/1/resumo-IAG-Fabio-2013.pdf
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Marc: |
LEADER 02692nam a2200181 a 4500
001 1967192
005 2021-11-08
008 2013 bl uuuu u00u1 u #d
100 1 $aOLIVEIRA, F.
245 $aOrnithogenic soil toposequence on Rata island, Fernando de Noronha archipelago, south atlantic and quaternary paleoclimatic implications.$h[electronic resource]
260 $aIn: IAG INTERNACIONAL CONFERENCE GEOMORPHOLOGY, 8., 2013, Paris. Resumo... Frankfurt: Association Internacionale des Géomorphologues$c2013
520 $aThe formation of highly phosphatized soils on sites of avian activity is a common feature of oceanic islands. We characterized a toposequence of phosphatic soils on Rata Island, to evaluate the soil genesis based on local topographic variations. For this purpose, four soils ranging from the upper hill down to the lowest landscape position on the island, representing a range of parent materials (basalt and calcareous sands), were analyzed. In the lowest landscape position a shallow Entisol was identified, strongly influenced by birds and marine sprays (Litholic Neosol), developed on " karstified" Pleistocene calcarenites; the three other soils in the upper part of the toposequence are Ornithogenic Inceptsols (Cambisols), ranging from a deep Cambisol profile on Basalt lava to intermediate Cambisols on mixed colluvial sediments of the basalt/calcareous. The lowermost Litholic Neosol is associated with a rugged landscape with strong calcarenite dissolution and karstification, related to a former wetter climate. The soil phosphatization is clearly an inherited process of the Late Quaternary age, when climate conditions were different. Initial weathering took place in the last interglacial period, under wetter conditions during which the Tertiary basalts were strongly weathered, leaving corestones in a saprolitic, oxidized mass. In the late Pleistocene, a gentle surface distributed these weathering products along the pediment slopes as colluvial materials, whereas in the coastal areas aeolian processes formed large sand dunes composed of reworked calcareous sands from marine sources during a time of very low sea level. During this time, widespread bird activity accounted for secondary apatite formation on the surface of calcareous oolites. Finally, the Holocene warming was accompanied by increasing sea level, enhanced tropical weathering, Fe and Al mobility and variscite formation superimposed on degraded Ca-phosphates, forming two phase phosphatic aggregates.
653 $aFernando de Noronha Archipelago
653 $aOrnithogenic soil
700 1 $aSCHAEFER, C.
700 1 $aABRAHÃO, W.
700 1 $aALMEIDA, E. de P. C.
700 1 $aSIMAS, F.
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