Bryophyte and pteridophyte spores and other palynomorphs in quaternary marine sediments from Campos Basin, southeastern Brazil: Core BU-91-GL-05
| Autor: | Mauro Bevilacqua de Toledo, Aline Gonçalves de Freitas, Marcelo de Araujo Carvalho, Cláudia Barbieri Ferreira Mendonça, Vania Gonçalves-Esteves |
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| Jazyk: | angličtina |
| Rok vydání: | 2015 |
| Předmět: |
Palynology
geography geography.geographical_feature_category Microfungi biology Ecology Terrigenous sediment Coastal plain spores Plant Science Biostratigraphy biology.organism_classification non-pollen palynomorphs Swamp paleoecology Campos Basin lcsh:QK1-989 Late Pleistocene lcsh:Botany Botany Glacial period Acrostichum Geology |
| Zdroj: | Acta Botânica Brasílica, Vol 29, Iss 2, Pp 161-174 (2015) Acta Botanica Brasilica, Volume: 29, Issue: 2, Pages: 161-174, Published: JUN 2015 Acta Botanica Brasilica v.29 n.2 2015 Acta Botanica Brasilica Sociedade Botânica do Brasil (SBB) instacron:SBB |
| Popis: | This paper presents morphological descriptions and ecological data of cryptogam spores and other non-pollen palynomorphs from Quaternary sediments of Campos Basin, Rio de Janeiro, SE Brazil. The ages were derived from biostratigraphy of planktonic foraminifers and two radiocarbon dates, and suggest that sediment deposition started in the last 140,000 years BP. Thirty different types of palynomorphs were identified, described, and photographed: two bryophyte spores (sensu lato); 21 pteridophyte spores; four freshwater microalgae; onePseudoschizaea; and two microfungi. Some of the identified spores (Sphagnum, Blechnum, Cyatheaceae, Dennstaedtiaceae, Lycopodiella, Microgramma, Polypodium, Acrostichum, Pityrogramma, and Lygodium) are related to the modern flora found on the northern coast of Rio de Janeiro State, at the Restinga of Jurubatiba, from vegetation types such as shrub swamp/coastal swamp formation, seasonally flooded forest, Clusia and Ericaceae woods, and disturbed vegetation. The freshwater microalgae and the microfungi are also presently recorded from the coastal lagoons of this region. The high spore concentration in slope sediments reflects the intense terrigenous influx, caused by a relative low sealevel during glacial stages. Palynological analysis suggests the presence of taxa from flooded forests and humid areas in the coastal plain during glacial and interglacial stages of the Late Pleistocene. |
| Databáze: | OpenAIRE |
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