1946
DOI: 10.1590/s0074-02761946000400001
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Considerações gerais sôbre a vegetação do Estado de Mato Grosso: I- notas preliminares sôbre o cerrado

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“…Earlier in the Cenozoic, much of the basin was an epeiric sea in which there was a deposition of sediments from the erosion of the Andes (Oliveira, 1956). The savanna and open woodlands that now exits in southcentral Brazil were probably continuous with those in northern South America in the Pliocene and probably into the Pleistocene, as evidenced by isolated patches of this habitat throughout the eastern part of the Amazon Basin ( Ducke andBlack, 1953, andVeloso, 1947). If this was the case, the prototype of Phrynohyas must have adapted to sul^humid conditions.…”
Section: Osteocephalus and Trachycephalusmentioning
confidence: 99%
“…Earlier in the Cenozoic, much of the basin was an epeiric sea in which there was a deposition of sediments from the erosion of the Andes (Oliveira, 1956). The savanna and open woodlands that now exits in southcentral Brazil were probably continuous with those in northern South America in the Pliocene and probably into the Pleistocene, as evidenced by isolated patches of this habitat throughout the eastern part of the Amazon Basin ( Ducke andBlack, 1953, andVeloso, 1947). If this was the case, the prototype of Phrynohyas must have adapted to sul^humid conditions.…”
Section: Osteocephalus and Trachycephalusmentioning
confidence: 99%
“…Exceptional floods are rare, with only three registered in the last century, in 1905, 1988 and 1995. There is no information about patterns of mortality of trees in Pantanal riparian forests at these events. Studies on riparian forests of Rio Paraguai mainly deal with structure (Dubs 1994;Guarin-Neto et al 1996;Veloso 1947) or the effects of inundation on the structure and distribution of species (e.g. Adámoli & Pott 1999;Nunes da Cunha & Junk 1999;Nunes da Cunha & Junk 2001;Prado et al 1994).…”
Section: Introductionmentioning
confidence: 99%