Bryophyte and pteridophyte spores and other palynomorphs in quaternary marine sediments from Campos Basin, southeastern Brazil: Core BU-91-GL-05

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...

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Main Authors: Aline Gonçalves de Freitas, Marcelo de Araujo Carvalho, Mauro Bevilacqua de Toledo, Claudia Barbieri Ferreira Mendonça, Vania Gonçalves-Esteves
Format: Article
Language:English
Published: Sociedade Botânica do Brasil 2015-06-01
Series:Acta Botânica Brasílica
Subjects:
Online Access:http://www.scielo.br/scielo.php?script=sci_arttext&pid=S0102-33062015000200161&lng=en&tlng=en
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author Aline Gonçalves de Freitas
Marcelo de Araujo Carvalho
Mauro Bevilacqua de Toledo
Claudia Barbieri Ferreira Mendonça
Vania Gonçalves-Esteves
author_facet Aline Gonçalves de Freitas
Marcelo de Araujo Carvalho
Mauro Bevilacqua de Toledo
Claudia Barbieri Ferreira Mendonça
Vania Gonçalves-Esteves
author_sort Aline Gonçalves de Freitas
collection DOAJ
description 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.
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spelling doaj.art-736069b5a4724ea0a1608ce892fd7dc72022-12-22T02:35:21ZengSociedade Botânica do BrasilActa Botânica Brasílica1677-941X2015-06-0129216117410.1590/0102-33062014abb3734S0102-33062015000200161Bryophyte and pteridophyte spores and other palynomorphs in quaternary marine sediments from Campos Basin, southeastern Brazil: Core BU-91-GL-05Aline Gonçalves de FreitasMarcelo de Araujo CarvalhoMauro Bevilacqua de ToledoClaudia Barbieri Ferreira MendonçaVania Gonçalves-EstevesThis 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.http://www.scielo.br/scielo.php?script=sci_arttext&pid=S0102-33062015000200161&lng=en&tlng=enCampos BasinLate Pleistocenenon-pollen palynomorphspaleoecologyspores
spellingShingle Aline Gonçalves de Freitas
Marcelo de Araujo Carvalho
Mauro Bevilacqua de Toledo
Claudia Barbieri Ferreira Mendonça
Vania Gonçalves-Esteves
Bryophyte and pteridophyte spores and other palynomorphs in quaternary marine sediments from Campos Basin, southeastern Brazil: Core BU-91-GL-05
Acta Botânica Brasílica
Campos Basin
Late Pleistocene
non-pollen palynomorphs
paleoecology
spores
title Bryophyte and pteridophyte spores and other palynomorphs in quaternary marine sediments from Campos Basin, southeastern Brazil: Core BU-91-GL-05
title_full Bryophyte and pteridophyte spores and other palynomorphs in quaternary marine sediments from Campos Basin, southeastern Brazil: Core BU-91-GL-05
title_fullStr Bryophyte and pteridophyte spores and other palynomorphs in quaternary marine sediments from Campos Basin, southeastern Brazil: Core BU-91-GL-05
title_full_unstemmed Bryophyte and pteridophyte spores and other palynomorphs in quaternary marine sediments from Campos Basin, southeastern Brazil: Core BU-91-GL-05
title_short Bryophyte and pteridophyte spores and other palynomorphs in quaternary marine sediments from Campos Basin, southeastern Brazil: Core BU-91-GL-05
title_sort bryophyte and pteridophyte spores and other palynomorphs in quaternary marine sediments from campos basin southeastern brazil core bu 91 gl 05
topic Campos Basin
Late Pleistocene
non-pollen palynomorphs
paleoecology
spores
url http://www.scielo.br/scielo.php?script=sci_arttext&pid=S0102-33062015000200161&lng=en&tlng=en
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