Amazonia: Landscape and Species Evolution 2009
DOI: 10.1002/9781444306408.ch11
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Long‐Term Landscape Development Processes in Amazonia

Abstract: The Amazon River system developed into its present form in a comparatively short period over approximately the last 10 million years. The western part of the drainage basin was mainly controlled by exhumation of the Andes. The Cenozoic Andean foreland consisted of a series of subsiding aggradational basins, interrupted by segments of basement (arches), which were particularly active during the Neogene. In this geodynamic landscape a system of highly instable rivers developed. During the Quaternary, landscape e… Show more

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Cited by 14 publications
(19 citation statements)
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“…These periods actually correspond to two different developmental phases of the main drainage. In the Plio–Pleistocene, the Amazon river (and its tributaries) would have been more entrenched and likely with vast fluctuations in discharge controlled by Quaternary climate fluctuations (see Irion & Kalliola, ). Such debate poses specific challenges to biological interpretations regarding the RBH based on estimates of divergence times.…”
Section: Introductionmentioning
confidence: 99%
“…These periods actually correspond to two different developmental phases of the main drainage. In the Plio–Pleistocene, the Amazon river (and its tributaries) would have been more entrenched and likely with vast fluctuations in discharge controlled by Quaternary climate fluctuations (see Irion & Kalliola, ). Such debate poses specific challenges to biological interpretations regarding the RBH based on estimates of divergence times.…”
Section: Introductionmentioning
confidence: 99%
“…Based on the evolutionary history of the Madeira River paleolandforms analyzed here, these features did not originate according to the hypothesis of ria formation due to erosion during the Last Glacial Maximum low sea level followed by sediment aggradation during the Holocene transgression (i.e. Irion, ; Irion and Kalliola, ). Due to the sandy nature, the active channel deposits were not used for radiocarbon dating.…”
Section: Discussionmentioning
confidence: 73%
“…Previous publications have related the genesis of Amazonian fluvial rias to sediment aggradation at the mouth of tributary channels (Sioli, ; Tricart, ). This process would have occurred as a result of fluvial erosion in the Last Glaciation Maximum low sea level, followed by sediment aggradation during the Holocene transgression (see a review in Irion and Kalliola, ). On the other hand, a few authors have also suggested a neotectonic origin for the Amazonian fluvial rias (Sternberg, , ; Mauro et al ., ; Dumont, ; Dumont and Fournier, ; Bezerra, ).…”
Section: Introductionmentioning
confidence: 99%
“…Over the last 30 million years (Ma), Amazon biodiversity evolved amidst extraordinary geomorphological dynamics. While the western sedimentary portion suffered several changes (Hoorn, Guerrero, Sarmiento, & Lorente, ;Hoorn et al, ;Rossetti, Toledo, & Góes, ;Vonhof, Wesselingh, & Ganssen, ), the eastern granitic shields experienced relative stability (Aleixo & Rossetti, ;Irion & Kalliola, ). How the evolution of the Amazonian biota reflects these environmental changes is still not fully understood (Leite & Rogers, ;Ribas, Aleixo, Nogueira, Miyaki, & Cracraft, ).…”
Section: Introductionmentioning
confidence: 99%