1. Identificação | |
Tipo de Referência | Artigo em Revista Científica (Journal Article) |
Site | plutao.sid.inpe.br |
Código do Detentor | isadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S |
Identificador | J8LNKAN8RW/3D53LPR |
Repositório | dpi.inpe.br/plutao/2012/11.28.16.49.44 (acesso restrito) |
Última Atualização | 2012:11.29.16.30.48 (UTC) administrator |
Repositório de Metadados | dpi.inpe.br/plutao/2012/11.28.16.49.45 |
Última Atualização dos Metadados | 2018:06.05.00.02.06 (UTC) administrator |
Chave Secundária | INPE--PRE/ |
DOI | 10.1016/j.geomorph.2012.07.015 |
ISSN | 0169-555X |
Rótulo | lattes: 0307721738107549 1 RossettiBerCreHay:2012:ImOrSa |
Chave de Citação | RossettiBerZanCreHay:2012:ImOrSa |
Título | Late Quaternary sedimentary dynamics in Western Amazonia: implications for the origin of savanna/forest contrasts |
Ano | 2012 |
Mês | Dec. |
Data de Acesso | 30 abr. 2024 |
Tipo Secundário | PRE PI |
Número de Arquivos | 1 |
Tamanho | 5356 KiB |
|
2. Contextualização | |
Autor | 1 Rossetti, Dilce de Fátima 2 Bertani, T. C. 3 Zani, Hiran 4 Cremon, Édipo Henrique 5 Hayakawa, E. H. |
Identificador de Curriculo | 1 8JMKD3MGP5W/3C9JGTQ |
Grupo | 1 DSR-OBT-INPE-MCTI-GOV-BR |
Afiliação | 1 Instituto Nacional de Pesquisas Espaciais (INPE) |
Endereço de e-Mail do Autor | 1 rossetti@dsr.inpe.br 2 3 hzani@dsr.inpe.br 4 edipocremon@yahoo.com.br |
Endereço de e-Mail | rossetti@dsr.inpe.br |
Revista | Geomorphology |
Volume | 177-17 |
Páginas | 74-92 |
Nota Secundária | B1_ANTROPOLOGIA_/_ARQUEOLOGIA B1_ASTRONOMIA_/_FÍSICA B1_CIÊNCIAS_BIOLÓGICAS_I A2_ECOLOGIA_E_MEIO_AMBIENTE B1_ENGENHARIAS_I A2_GEOCIÊNCIAS A1_GEOGRAFIA A1_INTERDISCIPLINAR |
Histórico (UTC) | 2012-11-28 23:06:29 :: lattes -> marciana :: 2012 2012-11-29 16:32:44 :: marciana -> administrator :: 2012 2018-06-05 00:02:06 :: administrator -> marciana :: 2012 |
|
3. Conteúdo e estrutura | |
É a matriz ou uma cópia? | é a matriz |
Estágio do Conteúdo | concluido |
Transferível | 1 |
Tipo do Conteúdo | External Contribution |
Tipo de Versão | publisher |
Palavras-Chave | • Amazonia • Open vegetation–forest contrasts •Paleomorphology Depositional system Late Quaternarycontraste vegetacional savana sedimentologia Amazônia sensoriamento remoto Quaternário |
Resumo | This work investigated the evolution of sedimentary environments during the latest Quaternary and their influence on the paradoxical occurrence of open vegetation patches in sharp contact with the Amazonian forest. The approach integrated pre-existing geological and floristic data from lowlands in the Brazilian Amazonia, with remote sensing imagery including multispectral optical images (TM, ETM+, and ASTER), Phased Array L-band Synthetic Aperture Radar (PALSAR), InSAR C-band SRTM-DEMs, and high resolution images obtained from Google Earth. The detection of an abundance of paleomorphologies provided evidence of a scenario in which constant environmental shifts were linked to the evolution of fluvial and megafan depositional systems. In all studied areas, the open vegetation patches are not random, but associated with sedimentary deposits representative of environments either deactivated during the Holocene or presently in the process of deactivation. Sedimentary evolution would have determined the distribution of wetlands and terra firme in many areas of the Amazonian lowlands, and would have a major impact on the development of open vegetated patches within the modern rainforest. Subsiding areas were filled up with megafan deposits, and many fluvial tributaries were rearranged on the landscape. The close relationship between vegetation and the physical environment suggests that sedimentary history related to the evolution of depositional settings during the latest Quaternary played a major role in the distribution of flooded and non-flooded areas of the Amazonian lowlands, with a direct impact on the distribution of modern floristic patterns. As the depositional sites were abandoned and their sedimentary deposits were exposed to the surface, they became sites suitable for vegetation growth, first of herbaceous species and then of forest. Although climate fluctuations might have been involved, fault reactivation appears to have been the main cause of changes in depositional dynamics through time, a process that had an immediate effect on the development of large open vegetation patches intermingled with the Amazonian rainforest. |
Área | SRE |
Arranjo | urlib.net > DIDSR > Late Quaternary sedimentary... |
Conteúdo da Pasta doc | acessar |
Conteúdo da Pasta source | não têm arquivos |
Conteúdo da Pasta agreement | não têm arquivos |
|
4. Condições de acesso e uso | |
Idioma | en |
Arquivo Alvo | 1-s2.0-S0169555X12003479-dilce.pdf |
Grupo de Usuários | administrator lattes marciana |
Visibilidade | shown |
Política de Arquivamento | denypublisher denyfinaldraft24 |
Permissão de Leitura | deny from all and allow from 150.163 |
Permissão de Atualização | não transferida |
|
5. Fontes relacionadas | |
Unidades Imediatamente Superiores | 8JMKD3MGPCW/3ER446E |
Divulgação | WEBSCI; PORTALCAPES. |
Acervo Hospedeiro | dpi.inpe.br/plutao@80/2008/08.19.15.01 |
|
6. Notas | |
Notas | Setores de Atividade: Outras atividades de serviços. |
Campos Vazios | alternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel format isbn lineage mark mirrorrepository nextedition number orcid parameterlist parentrepositories previousedition previouslowerunit progress project readergroup rightsholder schedulinginformation secondarydate session shorttitle sponsor subject tertiarymark tertiarytype typeofwork url |
|
7. Controle da descrição | |
e-Mail (login) | marciana |
atualizar | |
|