Late Holocene in central Brazil: vegetation changes and humidity variability in a tropical wetland

ABSTRACT The Pandeiros wetland is a high biodiversity ecosystem located within a semiarid region of the Cerrado biome, a neotropical savanna. This large wetland is of key importance for ecological and hydrological balance in central Brazil and for the conservation of the Cerrado fauna and flora. In...

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Published inJournal of quaternary science Vol. 36; no. 6; pp. 1028 - 1039
Main Authors SABINO, SHIRLEY MARIA LIMA, CASSINO, RAQUEL FRANCO, GOMES, MAKÊNIA OLIVEIRA SOARES, SANT'ANNA, ENEIDA MARIA ESKINAZI, ROCHA AUGUSTIN, CRISTINA HELENA RIBEIRO, DE OLIVEIRA, DIEGO ALVES
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LanguageEnglish
Published Chichester Wiley Subscription Services, Inc 01.08.2021
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Abstract ABSTRACT The Pandeiros wetland is a high biodiversity ecosystem located within a semiarid region of the Cerrado biome, a neotropical savanna. This large wetland is of key importance for ecological and hydrological balance in central Brazil and for the conservation of the Cerrado fauna and flora. In this study, we present the first palaeoecological investigation of the Pandeiros wetland based on pollen analysis of a palm swamp sediment core encompassing the Late Holocene. Our results show that the wetland was subject to multicentennial‐scale oscillations in water availability during the Late Holocene; in particular, higher local humidity was documented between 4100 and 3100 cal a bp and from 2600 to 1000 cal a bp, and two events of drier local conditions occurred at approximately 2900 and 900 cal a bp. Our results also indicate a general decreasing trend in arboreal density in the Pandeiros River Basin from the beginning of the Late Holocene to the present, with the greatest expansion of dry forest occurring between 3600 and 3100 cal a bp.
AbstractList The Pandeiros wetland is a high biodiversity ecosystem located within a semiarid region of the Cerrado biome, a neotropical savanna. This large wetland is of key importance for ecological and hydrological balance in central Brazil and for the conservation of the Cerrado fauna and flora. In this study, we present the first palaeoecological investigation of the Pandeiros wetland based on pollen analysis of a palm swamp sediment core encompassing the Late Holocene. Our results show that the wetland was subject to multicentennial‐scale oscillations in water availability during the Late Holocene; in particular, higher local humidity was documented between 4100 and 3100 cal a bp and from 2600 to 1000 cal a bp , and two events of drier local conditions occurred at approximately 2900 and 900 cal a bp. Our results also indicate a general decreasing trend in arboreal density in the Pandeiros River Basin from the beginning of the Late Holocene to the present, with the greatest expansion of dry forest occurring between 3600 and 3100 cal a bp.
ABSTRACT The Pandeiros wetland is a high biodiversity ecosystem located within a semiarid region of the Cerrado biome, a neotropical savanna. This large wetland is of key importance for ecological and hydrological balance in central Brazil and for the conservation of the Cerrado fauna and flora. In this study, we present the first palaeoecological investigation of the Pandeiros wetland based on pollen analysis of a palm swamp sediment core encompassing the Late Holocene. Our results show that the wetland was subject to multicentennial‐scale oscillations in water availability during the Late Holocene; in particular, higher local humidity was documented between 4100 and 3100 cal a bp and from 2600 to 1000 cal a bp, and two events of drier local conditions occurred at approximately 2900 and 900 cal a bp. Our results also indicate a general decreasing trend in arboreal density in the Pandeiros River Basin from the beginning of the Late Holocene to the present, with the greatest expansion of dry forest occurring between 3600 and 3100 cal a bp.
The Pandeiros wetland is a high biodiversity ecosystem located within a semiarid region of the Cerrado biome, a neotropical savanna. This large wetland is of key importance for ecological and hydrological balance in central Brazil and for the conservation of the Cerrado fauna and flora. In this study, we present the first palaeoecological investigation of the Pandeiros wetland based on pollen analysis of a palm swamp sediment core encompassing the Late Holocene. Our results show that the wetland was subject to multicentennial‐scale oscillations in water availability during the Late Holocene; in particular, higher local humidity was documented between 4100 and 3100 cal a bp and from 2600 to 1000 cal a bp, and two events of drier local conditions occurred at approximately 2900 and 900 cal a bp. Our results also indicate a general decreasing trend in arboreal density in the Pandeiros River Basin from the beginning of the Late Holocene to the present, with the greatest expansion of dry forest occurring between 3600 and 3100 cal a bp.
Author GOMES, MAKÊNIA OLIVEIRA SOARES
SABINO, SHIRLEY MARIA LIMA
SANT'ANNA, ENEIDA MARIA ESKINAZI
ROCHA AUGUSTIN, CRISTINA HELENA RIBEIRO
DE OLIVEIRA, DIEGO ALVES
CASSINO, RAQUEL FRANCO
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  organization: Coordenação de Geografia, Instituto Federal de Minas Gerais, Ouro Preto
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Snippet ABSTRACT The Pandeiros wetland is a high biodiversity ecosystem located within a semiarid region of the Cerrado biome, a neotropical savanna. This large...
The Pandeiros wetland is a high biodiversity ecosystem located within a semiarid region of the Cerrado biome, a neotropical savanna. This large wetland is of...
The Pandeiros wetland is a high biodiversity ecosystem located within a semiarid region of the Cerrado biome, a neotropical savanna. This large wetland is of...
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SubjectTerms Biodiversity
Cerrado
Conservation
Dry forests
Flora
Holocene
Humidity
Hydrology
Late Holocene
neotropical
Oscillations
Pollen
Pollen analysis
River basins
savanna
Savannahs
Semi arid areas
Semiarid zones
Vegetation changes
Water availability
wetland
Wetlands
Wildlife conservation
Title Late Holocene in central Brazil: vegetation changes and humidity variability in a tropical wetland
URI https://onlinelibrary.wiley.com/doi/abs/10.1002%2Fjqs.3351
https://www.proquest.com/docview/2557152767
Volume 36
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