2012
DOI: 10.1016/j.sedgeo.2012.09.015
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A Late Pleistocene–Holocene wetland megafan in the Brazilian Amazonia

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Cited by 31 publications
(39 citation statements)
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“…Main sedimentological characteristics of surface deposits at the Viruá megafan, with indication of the corresponding radiocarbon ages (modified fromRossetti et al, 2012b).…”
mentioning
confidence: 99%
“…Main sedimentological characteristics of surface deposits at the Viruá megafan, with indication of the corresponding radiocarbon ages (modified fromRossetti et al, 2012b).…”
mentioning
confidence: 99%
“…The area is characterized by sandy, nutrient poor and poorly-drained soils, that are developed on an extensive sedimentary lowland plain, derived from quartzite sands from the Içá geological formation (Rossetti et al 2012b;ICMBio 2014).…”
Section: Study Sitementioning
confidence: 99%
“…The monthly temperatures ranges from 20º-38ºC, the annual average is 24ºC (Rossetti et al 2012b). The average annual rainfall is about 2000 mm, the same for the state.…”
Section: Study Sitementioning
confidence: 99%
“…This was made possible mainly considering the geometry defined by the distribution of vegetation classes, such as shape, elongation, sinuosity, size, as well as pre-knowledge of the geomorphology from previous works undertaken in this region [19,28,29].…”
Section: Validation Of the Phytophysiognomic Mapmentioning
confidence: 99%
“…Such depositional systems are typical of areas of low topographic gradients having numerous avulsive channels and paleochannels (remnant of an inactive river) arranged into a distributary pattern [25][26][27]. Except for the Viruá megafan (e.g., [28,29]), located at the left margin of the Branco River (see location in Figure 1b), areas of open vegetation related with megafans in northern Amazonia remain to be characterized in more detail. The largest of these occurrences is associated with the Demini River, where two patches of open vegetation total ~4180 km 2 .…”
Section: Introductionmentioning
confidence: 99%