Laboratório de Paleoecologia Vegetal (LAPAV), Departamento de Geologia
e Paleontologia, Museu Nacional, Universidade Federal do Rio de Janeiro,
20940-040, Rio de Janeiro, Brazil
Marcelo de Araujo Carvalho
Laboratório de Paleoecologia Vegetal (LAPAV), Departamento de Geologia
e Paleontologia, Museu Nacional, Universidade Federal do Rio de Janeiro,
20940-040, Rio de Janeiro, Brazil
Cecília Cunha Lana
Laboratório de Paleoecologia Vegetal (LAPAV), Departamento de Geologia
e Paleontologia, Museu Nacional, Universidade Federal do Rio de Janeiro,
20940-040, Rio de Janeiro, Brazil
Gustavo Santiago
Laboratório de Paleoecologia Vegetal (LAPAV), Departamento de Geologia
e Paleontologia, Museu Nacional, Universidade Federal do Rio de Janeiro,
20940-040, Rio de Janeiro, Brazil
Natália de Paula Sá
Laboratório de Paleoecologia Vegetal (LAPAV), Departamento de Geologia
e Paleontologia, Museu Nacional, Universidade Federal do Rio de Janeiro,
20940-040, Rio de Janeiro, Brazil
Gabriel da Cunha Correia
Laboratório de Paleoecologia Vegetal (LAPAV), Departamento de Geologia
e Paleontologia, Museu Nacional, Universidade Federal do Rio de Janeiro,
20940-040, Rio de Janeiro, Brazil
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Total article views: 3,226 (including HTML, PDF, and XML)
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Total article views: 2,166 (including HTML, PDF, and XML)
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This study analyzed ancient climate patterns using plant fossils called palynomorphs. We identified 69 different palynomorphs from different plant groups (e.g., ferns, gymnosperms, angiosperms) and used statistical methods to support our findings. We found a trend towards increased humidity, likely influenced by a weather phenomenon called the Intertropical Convergence Zone.
This study analyzed ancient climate patterns using plant fossils called palynomorphs. We...
