Paleoclimatic and vegetation reconstruction of the last 22,000 years of western Santa Catarina (Brazil) studied by pollen records
Abstract
This study reconstructs vegetation change in southern Brazil from a pollen record spanning the last 27,000 years. Five palynological phases were identified in a 154-cm core from the Floresta Nacional de Chapecó (Santa Catarina). Phase I (26,855–24,622 cal. BP) reflects colder-than-present conditions, with grasslands dominant and small patches of Araucaria Forest. Phase II (23,922–22,593 cal. BP) shows a further increase in grassland taxa, indicating a still-cold but more humid climate. Phase III (21,894–7,620 cal. BP) begins under cold conditions and then transitions to warmer conditions, particularly after 7,000 cal. BP. During Phase IV (6,595–2,355 cal BP), the Araucaria Forest expanded, followed by the spread of Seasonal Deciduous Forest; this interval corresponds to peak warmth and humidity in the sequence. Phase V (after 1500 BP) records forest retreat, especially toward the top of the core, likely associated with Euro-Brazilian colonization and the advance of the modern agricultural frontier.
Keywords: Palynology, Paleoenvironments, Quaternary, Brazil, South America.
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Copyright (c) 2025 Ivan Luís Kirchner Eidt, Mirian Carbonera, Gisele Leite de Lima Primam, Jefferson Nunes Radaeski, Soraia Girardi Bauermann, Guilherme Luiz Girardi, Cristina Gouvêa Redin, Daniel Loponte

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This is an Open Access article distributed under the terms of the Creative Commons Attribution-NonCommercial-NoDerivatives license (http://creativecommons.org/licenses/by-nc-nd/4.0), which permits non-commercial re-use, distribution, and reproduction in any medium, provided that no alterations are made and the original article is properly cited. The written permission of Revista Brasileira de Paleontologia must be obtained before any commercial use and/or adaptation of the article.
