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Evidence of sea oscillations of the Late Quaternary in Rio Grande do Sul, Brazil, provided by palynological studies in Quaternary of South America Antarctic peninsula. Volume 1.
(supprimer)
A palynological analysis of a Quaternary, deep-water marine sedimentary core from Southern Brazil (South Atlantic Ocean: 3333S| 4828W) has been performed. Sea transgressions and regressions have been interpreted analyzing the relation between pollen