Zobrazeno 1 - 10
of 212
pro vyhledávání: '"KENITIRO SUGUIO"'
Autor:
Aline Meneguci Cunha, João Wagner Alencar Castro, Felipe Melo Barreto Pereira, Marcelo Araújo Carvalho, Kenitiro Suguio
Publikováno v:
Revista Brasileira de Geomorfologia, Vol 18, Iss 1 (2017)
As Flutuações do nível do mar e mudanças climáticas durante o Holoceno foram importante para construção e evolução das paisagens sedimentares costeiras. As variações do nível relativo do mar são identificadas através de indicadores geol
Externí odkaz:
https://doaj.org/article/0852578861c145bead296a42c2c389d3
Publikováno v:
Anais da Academia Brasileira de Ciências, Vol 86, Iss 2, Pp 671-683 (2014)
The present paper aims to investigate the relative sea-level and the coastal evolution during the Holocene in the Rio de Janeiro coastline, based on geological and biological indicators. Using topographic survey, excavation and coring, and 14C dating
Externí odkaz:
https://doaj.org/article/5a8e7abf72cc433b8b769d6d3ee2d0f5
Autor:
Kenitiro Suguio, Alcina Magnólia Franco Barreto, Paulo Eduardo de Oliveira, Francisco Hilário Rego Bezerra, Maria Cristina Santiago Hussein Vilela
Publikováno v:
Geologia USP. Série Científica, Vol 13, Iss 4, Pp 141-152 (2013)
This study deals with the Holocene relative sea level (RSL) changes along the Brazilian northeastern coast, in particular along the states of Pernambuco and Paraíba. It presents 25 sea level superficial indicators, dominantly of a biological nature
Externí odkaz:
https://doaj.org/article/90b5dc0d76e04334948bc5c9cff00a93
Publikováno v:
Geologia USP. Série Científica, Vol 12, Iss 3, Pp 115-132 (2012)
Serra da Capivara National Park and surrounding areas in Southeastern Piau State (Brazil) were subjected to morphostratigraphical, sedimentological, and geochronological studies about superficial deposits in order to interpret quaternary paleoenviron
Externí odkaz:
https://doaj.org/article/0485f770b8394371a5c038abeb5b74d0
Publikováno v:
Geologia USP. Série Científica, Vol 12, Iss 1, Pp 39-51 (2012)
The study area corresponds to the coastal plain neighboring the Ribeira de Iguape river mouth in the São Paulo State littoral,where the Iguape, Cananeia and Ilha Comprida municipalities are situated. This coastal plain exhibits an area of morethan 1
Externí odkaz:
https://doaj.org/article/2db55c25a40642b8ba88d1b11fe6865f
Autor:
João Wagner Alencar Castro, Kenitiro Suguio, Aline Meneguci da Cunha, Eliane Guedes, Frederico Tapajós de Souza Tâmega, Rafael Riosmena Rodriguez
Publikováno v:
Anuário do Instituto de Geociências, Vol 35, Iss 1, Pp 236-241 (2012)
Rochas de praia (beachrocks) marcam a linha de costa pretérita e a constituição sedimentar de paleopraias. Em ambiente de micro-marés definem com precisão a posição do nível médio do mar na ocasião do processo deposicional. O presente tra
Externí odkaz:
https://doaj.org/article/aca215e854ee424fbb5412a8401201b5
Publikováno v:
Anais da Academia Brasileira de Ciências, Vol 83, Iss 3, Pp 907-920 (2011)
This study presents field and chronological investigations along the coast of northeastern Brazil from ~4°S to 9°S latitude, which corresponds to ~700 km of coastline under a semi-diurnal mesotidal regime. We investigated wave-built terrace deposit
Externí odkaz:
https://doaj.org/article/2a6e361704814d47a7311525965c022b
Autor:
Roberto Barbosa Rodrigues, Kenitiro Suguio, Alethéa Ernandes Martins Sallun, Luiz Ricardo Lopes de Simone
Publikováno v:
Geologia USP. Série Científica, Vol 11, Iss 1, Pp 137-147 (2011)
The shell-middens present in the Iguape (São Paulo State) coastal plain are situated at different distances from thepresent shoreline. In general, the more external shell-middens, which show a dominance of Anomalocardia brasilianashells, give younge
Externí odkaz:
https://doaj.org/article/ecd983c3282c471cade92a4f5d8295ff
Autor:
Jacqueline Albino, Kenitiro Suguio
Publikováno v:
Anais da Academia Brasileira de Ciências, Vol 82, Iss 4, Pp 1031-1044 (2010)
The coastal sedimentation model in the Doce River mouth and surroundings extends beyond the hydraulic jetty effect created by its stream-flow. During flooding, marine sediments transported by longshore currents are retained on the updrift side, causi
Externí odkaz:
https://doaj.org/article/17665d52c5804367a5943906d1eed1ff
Autor:
Kenitiro Suguio, Claudio Riccomini, Alethéa Ernandes Martins Sallun, William Sallun Filho, Pedro Aronchi Neto
Publikováno v:
Geologia USP. Série Científica, Vol 10, Iss 3, Pp 49-56 (2010)
The Itaquaquecetuba Formation can be considered as relatively well-known from a paleontological viewpoint. Itsfossil content, which is very rich and represented by plants (tree trunks, seeds and leaves) and palynomorphs, has beenstudied in detail, al
Externí odkaz:
https://doaj.org/article/77e3a5061ffa4e16a2669662b2510580