Organic and inorganic geochemical data of sediment cores XC-03 and XC-01-2, Xingu River, Amazon Basin

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Autores principales: Bertassoli Junior, Dailson José, Sawakuchi, André Oliveira, Chiessi, Cristiano Mazur, Schefuß, Enno, Hartmann, Gelvam André, Häggi, Christoph, Zabel, Matthias, McGlue, Michael M, Santos, Rudney A, Pupim, Fabiano Nascimento
Formato: Dataset Open Access
Lenguaje:en
Publicado: PANGAEA 2019
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author Bertassoli Junior, Dailson José
Sawakuchi, André Oliveira
Chiessi, Cristiano Mazur
Schefuß, Enno
Hartmann, Gelvam André
Häggi, Christoph
Zabel, Matthias
McGlue, Michael M
Santos, Rudney A
Pupim, Fabiano Nascimento
author_facet Bertassoli Junior, Dailson José
Sawakuchi, André Oliveira
Chiessi, Cristiano Mazur
Schefuß, Enno
Hartmann, Gelvam André
Häggi, Christoph
Zabel, Matthias
McGlue, Michael M
Santos, Rudney A
Pupim, Fabiano Nascimento
collection Datos científicos de ciencias marinas y ambientales
contents Late Holocene hydroclimate variations have been extensively recognized in Amazonia, but the effects of such changes on riverine discharge within the Amazon lowlands are still poorly understood. We investigated a sediment core covering circa 4,000 to 300 cal yr BP collected in the lower valley of the Xingu River (Xingu Ria) in an area under the influence of the Amazon River. Our results indicate a decrease in precipitation in the Amazon lowlands throughout the studied period and reduced input of coarser and potassium‐rich Amazon River sediments to the confluence from about 2,600 to 1,400 cal yr BP. We suggest that lower temperatures in the extratropical Southern Hemisphere weakened the South American Summer Monsoon and led to a decrease in the water discharge of the Amazon River during this period.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_906264
institution PANGAEA
language en
publishDate 2019
publisher PANGAEA
record_format pangaea
spellingShingle Organic and inorganic geochemical data of sediment cores XC-03 and XC-01-2, Xingu River, Amazon Basin
Bertassoli Junior, Dailson José
Sawakuchi, André Oliveira
Chiessi, Cristiano Mazur
Schefuß, Enno
Hartmann, Gelvam André
Häggi, Christoph
Zabel, Matthias
McGlue, Michael M
Santos, Rudney A
Pupim, Fabiano Nascimento
Amazon; Compound-specific Isotopes; Late Holocene; Xingu River
Late Holocene hydroclimate variations have been extensively recognized in Amazonia, but the effects of such changes on riverine discharge within the Amazon lowlands are still poorly understood. We investigated a sediment core covering circa 4,000 to 300 cal yr BP collected in the lower valley of the Xingu River (Xingu Ria) in an area under the influence of the Amazon River. Our results indicate a decrease in precipitation in the Amazon lowlands throughout the studied period and reduced input of coarser and potassium‐rich Amazon River sediments to the confluence from about 2,600 to 1,400 cal yr BP. We suggest that lower temperatures in the extratropical Southern Hemisphere weakened the South American Summer Monsoon and led to a decrease in the water discharge of the Amazon River during this period.
title Organic and inorganic geochemical data of sediment cores XC-03 and XC-01-2, Xingu River, Amazon Basin
topic Amazon; Compound-specific Isotopes; Late Holocene; Xingu River
url https://doi.org/10.1594/PANGAEA.906264