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292S. MEDEANIC & I. C. S. CORREAFigure 2. Percentage palynodiagram of algal palynomorphs from the samples of the core T-64 (adapted from Medeanic& Corrêa 2008).Figure 3. Percentage palynodiagram of algal palynomorphs of Chlorophyta from the samples of the core T-14 (adaptedfrom Medeanic 2006).Pan-American Journal of Aquatic Sciences (2010), 5(2): 287-297
Climatic changes in the coastal plain of the Rio Grande do Sul293Figure 4. Generalized percentage palynodiagram from the samples of the core-drilling T-64: I – pollen and spores ofterrestrial vascular plants, II – pollen and spores of aquatic plants, III – pollen of Poaceae, IV – palynomorphs ofChlorophyta, V – marine algal palynomorphs, T – transgressive stage, R – regressive stage.Figure 5. Percentage palynodiagram of palynomorphs counted from the samples of the core T-14: AP – arboreal pollen,NAP – non-arboreal pollen, T – transgressive stage, R – regressive stage, 1 – mud, 2 – sand, 3 – more humid climate, 4– drier climate (adopted from Medeanic et al. 2003).Pan-American Journal of Aquatic Sciences (2010), 5(2): 287-297
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Representations in the Brazilian me
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XIVResearchers from Rede Clima and
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