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Provedor de dados:  Anais da ABC (AABC)
País:  Brazil
Título:  Cordão Formation: loess deposits in the southern coastal plain of the state of Rio Grande do Sul, Brazil
Autores:  LOPES,RENATO P.
DILLENBURG,SERGIO R.
SCHULTZ,CESAR L.
Data:  2016-12-01
Ano:  2016
Palavras-chave:  Chuy Creek
Coastal plain
Last glacial stage
Loess
Pleistocene
Resumo:  ABSTRACT Loess consists of silt-dominated sediments that cover ~10% of the Earth's surface. In southern South America it occurs in Argentina, Bolivia, Paraguay and Uruguay, and its presence in southern Brazil was never studied in detail. Here is proposed a new lithostratigraphic unit, Cordão Formation, consisting of loess deposits in the southern Brazilian coastal plain. It consists of fine-very fine silt with subordinate sand and clay, found mostly in lowland areas between Pleistocene coastal barriers. These sediments are pale-colored (10YR hue) and forms ~1,5-2,0 meter-thick stable vertical walls. The clay minerals include illite, smectite, interstratified illite/smectite and kaolinite, the coarser fraction is mostly quartz and plagioclase. Caliche and iron-manganese nodules are also present. The only fossils found so far are rodent teeth and a tooth of a camelid (Hemiauchenia paradoxa). Luminescence ages indicate that this loess was deposited in the latest Pleistocene, between ~30 and 10 kyrs ago, and its upper portion was modified by erosion and accumulation of clay and organic matter in the Holocene. The estimated accumulation rate was ~630 g/m2/year. The probable source of this loess is the Pampean Aeolian System of Argentina and it would have been deposited by the increased aeolian processes of the last glacial.
Tipo:  Info:eu-repo/semantics/article
Idioma:  Inglês
Identificador:  http://www.scielo.br/scielo.php?script=sci_arttext&pid=S0001-37652016000602143
Editor:  Academia Brasileira de Ciências
Relação:  10.1590/0001-3765201620150738
Formato:  text/html
Fonte:  Anais da Academia Brasileira de Ciências v.88 n.4 2016
Direitos:  info:eu-repo/semantics/openAccess
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