@Article{CremonRossSawaCohe:2016:RoTeCl,
author = "Cremon, {\'E}dipo Henrique and Rossetti, Dilce de F{\'a}tima and
Sawakuchi, Andr{\'e} de Oliveira and Cohen, Marcelo Cancela
Lisboa",
affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and {Instituto
Nacional de Pesquisas Espaciais (INPE)} and Instituto Federal de
Educa{\c{c}}{\~a}o, Ci{\^e}ncia e Tecnologia de Goi{\'a}s and
Instituto Federal de Educa{\c{c}}{\~a}o, Ci{\^e}ncia e
Tecnologia de Goi{\'a}s",
title = "The role of tectonics and climate in the late Quaternary evolution
of a northern Amazonian River",
journal = "Geomorphology",
year = "2016",
volume = "271",
pages = "22--39",
month = "Oct.",
keywords = "Branco River, Late Quaternary, Northern Amazonia, Sedimentary
evolution, Tectonic mega-capture.",
abstract = "The Amazon basin has most of the largest rivers of the world.
However, works focusing the geological evolution of the trunk
river or its tributaries have been only partly approached. The
Branco River constitutes one of the main northern Amazonian
tributaries. A previous work proposed that, before flowing
southward into the Negro-Amazon Rivers, the Branco River had a
southwest to northeast course into the Caribbean Sea. The present
work aimed to establish if the proposed change in the course of
this river is supported by morphological and sedimentological
data. Other goals were to discuss the factors influencing river
development and establish its evolution over time within the
chronological framework provided by radiocarbon and optically
stimulated luminescence dating. The work considered the entire
course of the Branco River downstream of the Precambrian Guiana
Shield, where the river presumably did not exist in ancient times.
The river valley is incised into fluvial sedimentary units
displaying ages between 100 and 250 ky old, which record active
and abandoned channels, crevasse splay/levees, and point bars. The
sedimentary deposits in the valley include two alluvial plain
units as old as 18.7 ky and which intersects a Late Pleistocene
residual megafan. These characteristics suggest that a long
segment of the Branco River was established only a few thousand
years ago. Together with several structural anomalies, these data
are consistent with a mega-capture at the middle reach of this
river due to tectonic reactivation in the Late Pleistocene. This
integrated approach can be applied to other Amazonian tributaries
to unravel how and when the Amazonian drainage basin became
established.",
doi = "10.1016/j.geomorph.2016.07.030",
url = "http://dx.doi.org/10.1016/j.geomorph.2016.07.030",
issn = "0169-555X",
language = "en",
targetfile = "cremon_role.pdf",
urlaccessdate = "05 maio 2024"
}