New Holocene pollen records from the Brazilian Caatinga

Detalhes bibliográficos
Autor(a) principal: MEDEIROS,VANDA B. DE
Data de Publicação: 2018
Outros Autores: OLIVEIRA,PAULO E. DE, SANTOS,RUDNEY A., BARRETO,ALCINA M.F., OLIVEIRA,MARCELO A.T. DE, PINAYA,JORGE L.D.
Tipo de documento: Artigo
Idioma: eng
Título da fonte: Anais da Academia Brasileira de Ciências (Online)
Texto Completo: http://old.scielo.br/scielo.php?script=sci_arttext&pid=S0001-37652018000502011
Resumo: Abstract We present two pollen diagrams from the semi-arid Caatinga of the Catimbau National Park, in Pernambuco and from a Mauritia palm forest in the Caatinga/Cerrado ecotone of southern Piauí, NE Brazil, spanning the last 10,000 cal. yrs BP and the last 1,750 cal yrs BP, respectively. These two records contain a signature of the local vegetation and permit the correlation of the pollen signal with regional climatic changes. The Catimbau record shows Zizyphus sp., a typical Caatinga taxon, in all three pollen zones indicating regional Caatinga vegetation and the predominance of local arboreal taxa adapted to high humidity from 10,000 to ca. 6,000 cal. yrs BP with a gradual tendency towards drier conditions revealed by a deposition hiatus between 6,000 to ca. 2,000 cal. yrs BP. This abrupt loss of sediments in both localities is interpreted as a consequence of the establishment of modern semi-arid climates. The subsequent return of humidity is signaled by increased sedimentation rates and 14C date inversions in agreement with high precipitation, revealed by σ18O ratios in speleothems from NE Brazil. Modern sediments deposited in the last 500 years reflect local conditions with the maintenance of humidity by geological faulting and surfacing water tables.
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spelling New Holocene pollen records from the Brazilian CaatingapaleoclimatologypalynologyPernambucoPiauícaatinga vegetationAbstract We present two pollen diagrams from the semi-arid Caatinga of the Catimbau National Park, in Pernambuco and from a Mauritia palm forest in the Caatinga/Cerrado ecotone of southern Piauí, NE Brazil, spanning the last 10,000 cal. yrs BP and the last 1,750 cal yrs BP, respectively. These two records contain a signature of the local vegetation and permit the correlation of the pollen signal with regional climatic changes. The Catimbau record shows Zizyphus sp., a typical Caatinga taxon, in all three pollen zones indicating regional Caatinga vegetation and the predominance of local arboreal taxa adapted to high humidity from 10,000 to ca. 6,000 cal. yrs BP with a gradual tendency towards drier conditions revealed by a deposition hiatus between 6,000 to ca. 2,000 cal. yrs BP. This abrupt loss of sediments in both localities is interpreted as a consequence of the establishment of modern semi-arid climates. The subsequent return of humidity is signaled by increased sedimentation rates and 14C date inversions in agreement with high precipitation, revealed by σ18O ratios in speleothems from NE Brazil. Modern sediments deposited in the last 500 years reflect local conditions with the maintenance of humidity by geological faulting and surfacing water tables.Academia Brasileira de Ciências2018-08-01info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersiontext/htmlhttp://old.scielo.br/scielo.php?script=sci_arttext&pid=S0001-37652018000502011Anais da Academia Brasileira de Ciências v.90 n.2 suppl.1 2018reponame:Anais da Academia Brasileira de Ciências (Online)instname:Academia Brasileira de Ciências (ABC)instacron:ABC10.1590/0001-3765201820170161info:eu-repo/semantics/openAccessMEDEIROS,VANDA B. DEOLIVEIRA,PAULO E. DESANTOS,RUDNEY A.BARRETO,ALCINA M.F.OLIVEIRA,MARCELO A.T. DEPINAYA,JORGE L.D.eng2019-11-29T00:00:00Zoai:scielo:S0001-37652018000502011Revistahttp://www.scielo.br/aabchttps://old.scielo.br/oai/scielo-oai.php||aabc@abc.org.br1678-26900001-3765opendoar:2019-11-29T00:00Anais da Academia Brasileira de Ciências (Online) - Academia Brasileira de Ciências (ABC)false
dc.title.none.fl_str_mv New Holocene pollen records from the Brazilian Caatinga
title New Holocene pollen records from the Brazilian Caatinga
spellingShingle New Holocene pollen records from the Brazilian Caatinga
MEDEIROS,VANDA B. DE
paleoclimatology
palynology
Pernambuco
Piauí
caatinga vegetation
title_short New Holocene pollen records from the Brazilian Caatinga
title_full New Holocene pollen records from the Brazilian Caatinga
title_fullStr New Holocene pollen records from the Brazilian Caatinga
title_full_unstemmed New Holocene pollen records from the Brazilian Caatinga
title_sort New Holocene pollen records from the Brazilian Caatinga
author MEDEIROS,VANDA B. DE
author_facet MEDEIROS,VANDA B. DE
OLIVEIRA,PAULO E. DE
SANTOS,RUDNEY A.
BARRETO,ALCINA M.F.
OLIVEIRA,MARCELO A.T. DE
PINAYA,JORGE L.D.
author_role author
author2 OLIVEIRA,PAULO E. DE
SANTOS,RUDNEY A.
BARRETO,ALCINA M.F.
OLIVEIRA,MARCELO A.T. DE
PINAYA,JORGE L.D.
author2_role author
author
author
author
author
dc.contributor.author.fl_str_mv MEDEIROS,VANDA B. DE
OLIVEIRA,PAULO E. DE
SANTOS,RUDNEY A.
BARRETO,ALCINA M.F.
OLIVEIRA,MARCELO A.T. DE
PINAYA,JORGE L.D.
dc.subject.por.fl_str_mv paleoclimatology
palynology
Pernambuco
Piauí
caatinga vegetation
topic paleoclimatology
palynology
Pernambuco
Piauí
caatinga vegetation
description Abstract We present two pollen diagrams from the semi-arid Caatinga of the Catimbau National Park, in Pernambuco and from a Mauritia palm forest in the Caatinga/Cerrado ecotone of southern Piauí, NE Brazil, spanning the last 10,000 cal. yrs BP and the last 1,750 cal yrs BP, respectively. These two records contain a signature of the local vegetation and permit the correlation of the pollen signal with regional climatic changes. The Catimbau record shows Zizyphus sp., a typical Caatinga taxon, in all three pollen zones indicating regional Caatinga vegetation and the predominance of local arboreal taxa adapted to high humidity from 10,000 to ca. 6,000 cal. yrs BP with a gradual tendency towards drier conditions revealed by a deposition hiatus between 6,000 to ca. 2,000 cal. yrs BP. This abrupt loss of sediments in both localities is interpreted as a consequence of the establishment of modern semi-arid climates. The subsequent return of humidity is signaled by increased sedimentation rates and 14C date inversions in agreement with high precipitation, revealed by σ18O ratios in speleothems from NE Brazil. Modern sediments deposited in the last 500 years reflect local conditions with the maintenance of humidity by geological faulting and surfacing water tables.
publishDate 2018
dc.date.none.fl_str_mv 2018-08-01
dc.type.driver.fl_str_mv info:eu-repo/semantics/article
dc.type.status.fl_str_mv info:eu-repo/semantics/publishedVersion
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status_str publishedVersion
dc.identifier.uri.fl_str_mv http://old.scielo.br/scielo.php?script=sci_arttext&pid=S0001-37652018000502011
url http://old.scielo.br/scielo.php?script=sci_arttext&pid=S0001-37652018000502011
dc.language.iso.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv 10.1590/0001-3765201820170161
dc.rights.driver.fl_str_mv info:eu-repo/semantics/openAccess
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dc.publisher.none.fl_str_mv Academia Brasileira de Ciências
publisher.none.fl_str_mv Academia Brasileira de Ciências
dc.source.none.fl_str_mv Anais da Academia Brasileira de Ciências v.90 n.2 suppl.1 2018
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