FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2088690617> ?p ?o ?g. }

• W2088690617 endingPage "136" @default.
• W2088690617 startingPage "127" @default.
• W2088690617 abstract "RESUMO - Este trabalho visa analisar os processos temporais que influenciaram a sedimentacao de palinomorfos em depositos da lagoa do Campelo (municipio de Campos dos Goitacazes, Estado do Rio de Janeiro). Formada no Holoceno, durante a colmatacao de uma vasta paleolaguna, a lagoa conectava-se ao rio Paraiba do Sul pelo canal da Cataia, que a alimentava de agua durante as cheias. Obras de drenagem realizadas em 1950 mudaram a configuracao geomorfologica original e geraram dois novos canais, um ligando a lagoa ao rio, outro ao mar, que, por varios motivos, acabaram transformando em negativo o balanco hidrico da lagoa. As analises das amostras refletiram uma vegetacao hidrofita bem representada em cerca de 2.790 anos A.P.( 14 ABSTRACT - TEMPORAL DYNAMICS IN LAGOA DO CAMPELO, NORTHERN REGION OF THE STATE OF RIO DE JANEIRO, BASED ON PALYNOLOGYCAL STUDIES. This study aims to analyze the temporal processes that influenced the palynomorph sedimentation in the Campelo Lake (Campos dos Goitacazes municipality, Rio de Janeiro State, Brazil). Formed during the Holocene by the isolation of a large paleolagoon, this lake was connected in the past to the Paraiba do Sul River by Cataia's channel which fed it with waters during the inundations. Drainage modifications in the Campos municipality realized in 1950 changed the geomorphological configuration of the Campelo Lake and two new channels were constructed, connecting the lake to the river and to the sea, respectively, which transformed in negative the hydrological balancing of the lake by several reasons. The palynological analysis reflected around 2,790 years B.P. ( 14 C conventional age) hydrophytic vegetation well represented, with low number of pollen types and a high Pseudoschizaea deposition characterizing the development of a wet environment with lower water level. That period corresponded to the descent of the sea level initiated in 2,800 years B.P. which carried the progradation of the outlet of the Paraiba do Sul River. With the elevation of sea level starting from 2,700 years B.P., that causes the erosion in the outlet of the river Paraiba, occurred a progressive damming of waters in the low plain. Near the period of a maximum sea level around 2.500 years B.P. (interpolated age) pollen deposition in the local was facilitated by the rise of water level in the lake. About 2,320 years B.P. ( 14 C conventional age) the Rate of Total Accumulation of palinomorphs was very high, mostly by increase of the herbaceous types and of the hydrophytes. In the location of the core the sedimentation behind 2,320 years B.P. was practically null." @default.
• W2088690617 created "2016-06-24" @default.
• W2088690617 creator A5004323501 @default.
• W2088690617 creator A5037597773 @default.
• W2088690617 creator A5055630685 @default.
• W2088690617 date "2006-04-30" @default.
• W2088690617 modified "2023-09-25" @default.
• W2088690617 title "Dinâmica temporal na lagoa do Campelo, região norte do Estado do Rio de Janeiro, baseada em estudos palinológicos" @default.
• W2088690617 cites W1967564730 @default.
• W2088690617 cites W1968650615 @default.
• W2088690617 cites W1971516910 @default.
• W2088690617 cites W2002974370 @default.
• W2088690617 cites W2009231912 @default.
• W2088690617 cites W2034289198 @default.
• W2088690617 cites W2034460928 @default.
• W2088690617 cites W2036801951 @default.
• W2088690617 cites W2128694541 @default.
• W2088690617 cites W2141459972 @default.
• W2088690617 cites W2143972625 @default.
• W2088690617 cites W2507981548 @default.
• W2088690617 cites W2944451707 @default.
• W2088690617 cites W2952844206 @default.
• W2088690617 cites W3173951286 @default.
• W2088690617 cites W634543797 @default.
• W2088690617 cites W643192806 @default.
• W2088690617 doi "https://doi.org/10.4072/rbp.2006.1.13" @default.
• W2088690617 hasPublicationYear "2006" @default.
• W2088690617 type Work @default.
• W2088690617 sameAs 2088690617 @default.
• W2088690617 citedByCount "8" @default.
• W2088690617 countsByYear W20886906172013 @default.
• W2088690617 countsByYear W20886906172015 @default.
• W2088690617 countsByYear W20886906172017 @default.
• W2088690617 countsByYear W20886906172022 @default.
• W2088690617 crossrefType "journal-article" @default.
• W2088690617 hasAuthorship W2088690617A5004323501 @default.
• W2088690617 hasAuthorship W2088690617A5037597773 @default.
• W2088690617 hasAuthorship W2088690617A5055630685 @default.
• W2088690617 hasBestOaLocation W20886906171 @default.
• W2088690617 hasConcept C127313418 @default.
• W2088690617 hasConcept C205649164 @default.
• W2088690617 hasConceptScore W2088690617C127313418 @default.
• W2088690617 hasConceptScore W2088690617C205649164 @default.
• W2088690617 hasIssue "1" @default.
• W2088690617 hasLocation W20886906171 @default.
• W2088690617 hasOpenAccess W2088690617 @default.
• W2088690617 hasPrimaryLocation W20886906171 @default.
• W2088690617 hasRelatedWork W1999913942 @default.
• W2088690617 hasRelatedWork W2086120259 @default.
• W2088690617 hasRelatedWork W2137941439 @default.
• W2088690617 hasRelatedWork W2141795027 @default.
• W2088690617 hasRelatedWork W2151614148 @default.
• W2088690617 hasRelatedWork W2245170124 @default.
• W2088690617 hasRelatedWork W2324615561 @default.
• W2088690617 hasRelatedWork W2748952813 @default.
• W2088690617 hasRelatedWork W2899084033 @default.
• W2088690617 hasRelatedWork W3186982001 @default.
• W2088690617 hasVolume "9" @default.
• W2088690617 isParatext "false" @default.
• W2088690617 isRetracted "false" @default.
• W2088690617 magId "2088690617" @default.
• W2088690617 workType "article" @default.