Luminescence of quartz and feldspar fingerprints provenance and correlates with the source area denudation in the Amazon River basin

Luminescence of quartz and feldspar fingerprints provenance and correlates with the source area denudation in the Amazon River basin

Autor Sawakuchi, A. O. Google Scholar
Jain, M. Google Scholar
Mineli, T. D. Google Scholar
Nogueira, L. Google Scholar
Bertassoli, D. J., Jr. Google Scholar
Haeggi, C. Google Scholar
Sawakuchi, H. O. Google Scholar
Pupim, F. N. Autor UNIFESP Google Scholar
Grohmann, C. H. Google Scholar
Chiessi, C. M. Google Scholar
Zabel, M. Google Scholar
Mulitza, S. Google Scholar
Mazoca, C. E. M. Google Scholar
Cunha, D. F. Google Scholar
Resumo The Amazon region hosts the world's largest watershed spanning from high elevation Andean terrains to lowland cratonic shield areas in tropical South America. This study explores variations in optically stimulated luminescence (OSL) and infrared stimulated luminescence (IRSL) signals in suspended silt and riverbed sands retrieved from major Amazon rivers. These rivers drain Pre-Cambrian to Cenozoic source rocks in areas with contrasting denudation rates. In contrast to the previous studies, we do not observe an increase in the OSL sensitivity of quartz with transport distance

for example, Tapajos and Xingu Rivers show more sensitive quartz than Solimbes and Madeira Rivers, even though the latter have a significantly larger catchment area and longer sediment transport distance. Interestingly, high sensitivity quartz is observed in rivers draining relatively stable Central Brazil and Guiana shield areas (denudation rate xi = 0.04 mm yr(-1)), while low sensitivity quartz occurs in less stable Andean terrains (xi = 0.24 mm yr(-1)). An apparent linear correlation between quartz OSL sensitivity and denudation rate suggests that OSL sensitivity may be used as a proxy for erosion rates in the Amazon basin. Furthermore, luminescence sensitivity measured in sand or silt arises from the same mineral components (quartz and feldspar) and clearly discriminates between Andean and shield sediments, avoiding the grain size bias in provenance analysis. These results have implications for using luminescence sensitivity as a proxy for Andean and shield contributions in the stratigraphic record, providing a new tool to reconstruct past drainage configurations within the Amazon basin. (C) 2018 Elsevier B.V. All rights reserved.
Assunto sediment provenance
luminescence
denudation
tropical rivers
Amazon
Idioma Inglês
Financiador Sao Paulo Research Foundation [FAPESP]
FAPESP
National Science Foundation [NSF DEB]
Brazilian National Council for Scientific and Technological Development (CNPq) [3009223/2014-8, 302607/2016-1, 422255/2016-5, 307647/2015-3]
Número do financiamento FAPESP: 2011/06609-1
FAPESP: 2012/50260-6
FAPESP: 2014/23334-4
FAPESP: 2016/09293-9
NSF DEB: 1241066
CNPq: 3009223/2014-8
CNPq: 302607/2016-1
CNPq: 422255/2016-5
CNPq: 307647/2015-3
Data 2018
Publicado em Earth And Planetary Science Letters. Amsterdam, v. 492, p. 152-162, 2018.
ISSN 0012-821X (Sherpa/Romeo, fator de impacto)
Editor Elsevier Science Bv
Extensão 152-162
Fonte http://dx.doi.org/10.1016/j.epsl.2018.04.006
Direito de acesso Acesso restrito
Tipo Artigo
Web of Science WOS:000432762000015
URI http://repositorio.unifesp.br/handle/11600/45974

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