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DOI	10.1016/j.epsl.2020.116423
	Reappraisal of the relative importance of dynamic topography and Andean orogeny on Amazon landscape evolution
	Bicudo T.C.; Sacek V.; Paes de Almeida R.
发表日期	2020
ISSN	0012821X
卷号	546
英文摘要	The Cenozoic landscape of northern South America evolved under the influence of different geodynamic processes, culminating in the formation of the largest drainage basin on Earth, the Amazon drainage system. The orogeny of the Andean cordillera and the increase in surface denudation induced an asymmetric influx of sediments in Amazonia, which caused an eastward propagation of the Andean sedimentary wedge, reversing the topographic gradient and driving the drainage flow towards the Atlantic Equatorial margin. The low-relief topography of lowlands in Amazonia is also a factor that propitiates this reversal. Concomitantly, variations in the subduction angle of the Nazca plate under the continental lithosphere during the Miocene also contributed to create dynamic topography that perturbed the surface and modified the drainage pattern through time. In the last decade, both surface processes during Andean orogeny and dynamic topography were invoked independently to explain the formation of the present Amazon drainage system connecting the Andes and the equatorial margin. However, hitherto these mechanisms were not considered in a single model, hampering the evaluation of the contribution of each factor on the evolution of the Amazon River. To quantify the combined effect of the different geodynamic processes, in the present work we used numerical models that integrate orogeny, surface processes, dynamic topography and flexural isostasy of the lithosphere. In our results, we present new numerical scenarios for the Cenozoic landscape evolution of Amazonia, showing that the dynamic topography may have affected the environmental evolution in western Amazonia, favoring the development of a megawetland in this region before the establishment of the Amazon River as a transcontinental river. We conclude that, although the formation of the Amazon drainage system can be explained without the influence of mantle convection, variations in dynamic topography may have anticipated the establishment of the transcontinental drainage system a few million years. Furthermore, the stratigraphic evolution and the total Cenozoic sedimentation preserved in the Solimões Basin is a function of the temporal variations in the amplitude of dynamic topography in northern South America. © 2020 Elsevier B.V.
关键词	Amazon River dynamic topography geodynamic modeling tectono-sedimentary processes
英文关键词	Catchments; Drainage; Geodynamics; Lithology; Rivers; Stratigraphy; Continental lithosphere; Dynamic topography; Eastward propagation; Environmental evolution; Geodynamic process; Landscape evolutions; Temporal variation; Topographic gradients; Topography; Cenozoic; geodynamics; isostasy; landscape evolution; numerical model; orogeny; river evolution; topography; wetland; Amazon River; Amazonia; Andes
语种	英语
来源期刊	Earth and Planetary Science Letters
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/202490
作者单位	Instituto de Astronomina, Geofísica e Ciências Atmosféricas, University of Sao Paulo, Brazil; Instituto de Geociências, University of Sao Paulo, Brazil
推荐引用方式 GB/T 7714	Bicudo T.C.,Sacek V.,Paes de Almeida R.. Reappraisal of the relative importance of dynamic topography and Andean orogeny on Amazon landscape evolution[J],2020,546.
APA	Bicudo T.C.,Sacek V.,&Paes de Almeida R..(2020).Reappraisal of the relative importance of dynamic topography and Andean orogeny on Amazon landscape evolution.Earth and Planetary Science Letters,546.
MLA	Bicudo T.C.,et al."Reappraisal of the relative importance of dynamic topography and Andean orogeny on Amazon landscape evolution".Earth and Planetary Science Letters 546(2020).