Influence of the "Hypsithermal Age" and "Neoglaciation" climatic conditions on the Brazilian coast.

dc.contributorpt-BR
dc.creatorSUGUIO, KENITIRO
dc.date2001-12-31
dc.date.accessioned2018-11-07T22:00:16Z
dc.date.available2018-11-07T22:00:16Z
dc.identifierhttps://seer.ufrgs.br/PesquisasemGeociencias/article/view/20296
dc.identifier10.22456/1807-9806.20296
dc.identifier.urihttp://repositorioslatinoamericanos.uchile.cl/handle/2250/2192407
dc.descriptionMeanwhile the highest relative sea-level is the present one in southeastern United States (Gulf of Mexico) or in Netherlands coast, most of the Brazilian coast exhibited Holocene sea-levels higher than the present in the past. The Brazilian curves, representing the relative sea-level changes during last 7.000 years, are outlined using sedimentological, biological and prehistorical past sea-level records. This paper shows that these relative sea-level records, during the Holocene, can be suitably used to demonstrate the influence of the worldwide known paleoclimatic events, like the “Hypsithermal Age” and “Neoglaciation” on the Brazilian coast.pt-BR
dc.formatapplication/pdf
dc.languagepor
dc.publisherInstituto de Geociências /Universidade Federal do Rio Grande do Sulpt-BR
dc.relationhttps://seer.ufrgs.br/PesquisasemGeociencias/article/view/20296/pdf
dc.sourcePesquisas em Geociências; v. 28, n. 2 (2001): Pesquisas em Geociências; 213-222pt-BR
dc.source1807-9806
dc.source1518-2398
dc.subjectGeociências;Geologia;Geografia;Geodésia;Paleontologia;Engenharia Cartográficapt-BR
dc.subject''Hypsithermal Age"; "Neoglaciation"; Holoce paleoclimate.pt-BR
dc.subjectGeociênciaspt-BR
dc.titleInfluence of the "Hypsithermal Age" and "Neoglaciation" climatic conditions on the Brazilian coast.pt-BR
dc.typeArtículos de revistas
dc.typeArtículos de revistas
dc.coveragept-BR
dc.coveragept-BR
dc.coveragept-BR


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