2004
DOI: 10.1016/s0031-0182(04)00401-8
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Amazonian paleoecological histories: one hill, three watersheds

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Cited by 134 publications
(106 citation statements)
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“…On one hand, the mixture of contraction, stability, and expansion signals shown by both methods agrees with the hypothesis of a continuous and permanent forest cover since the last glacial maximum in the north-western Amazon Basin (Colinvaux et al (1996), Bush et al (2002 and Mayle et al (2004)), with different species reacting differently to climatic oscillations. On the other hand, the overall higher confidence in expansion signals, as well as the complete lack of support for contractions shown by the ML approach, agrees with refugial hypotheses (Haffer 1969;Prance 1982) and floristic transition assumptions (Colinvaux et al 2000;Bush et al 2004), possibly with fastgrowing, light-demanding and pioneer species having responded more intensely than shade-tolerant ones to climatic change. Thus, Guiana Shield forests appear to have had a more complicated history than temperate and boreal forests (Taberlet et al 1998;Hewitt 2000Hewitt , 2004Petit et al 2002;Hu et al 2009): a mixture of gradual compositional changes and expansion from refugia.…”
Section: Discussionsupporting
confidence: 60%
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“…On one hand, the mixture of contraction, stability, and expansion signals shown by both methods agrees with the hypothesis of a continuous and permanent forest cover since the last glacial maximum in the north-western Amazon Basin (Colinvaux et al (1996), Bush et al (2002 and Mayle et al (2004)), with different species reacting differently to climatic oscillations. On the other hand, the overall higher confidence in expansion signals, as well as the complete lack of support for contractions shown by the ML approach, agrees with refugial hypotheses (Haffer 1969;Prance 1982) and floristic transition assumptions (Colinvaux et al 2000;Bush et al 2004), possibly with fastgrowing, light-demanding and pioneer species having responded more intensely than shade-tolerant ones to climatic change. Thus, Guiana Shield forests appear to have had a more complicated history than temperate and boreal forests (Taberlet et al 1998;Hewitt 2000Hewitt , 2004Petit et al 2002;Hu et al 2009): a mixture of gradual compositional changes and expansion from refugia.…”
Section: Discussionsupporting
confidence: 60%
“…The dry-climate-with-refugia hypothesis has nevertheless been challenged (Bush & De Oliveira 2006). One alternative hypothesis, suggested by Amazonian pollen records (Colinvaux et al 1996), is that a 6°C cooling during the LGM may have caused a floristic transition, rather than rainforest fragmentation and replacement of rainforest by open, drier tropical forests (Colinvaux et al 2000;Bush et al 2004;Freycon et al 2010).…”
Section: Introductionmentioning
confidence: 99%
“…Adapted from Figure 5 in Jackson and Overpeck (2000 Cannariato et al 1999;Mix et al 1999). No-analog assemblages occur in terrestrial and marine settings and from high latitudes (Edwards et al 2005) to low (Bush et al 2004). The assemblages appear to represent truly anomalous communities and are not due to after-death mixing of fossils from temporally or spatially distinct communities (Jackson and .…”
Section: No-analog Communities Of the Past: A Late-glacial Case Studymentioning
confidence: 99%
“…Equatorial environments of South America maintained a more stable climate throughout the LGM (Brown and Ab' Saber, 1979;Ledru et al, 1996;Bush et al, 2004). Moreover, lakes and wetlands remained available in the Amazon region at the time (Bush et al, 2004). As the great egret requires shallow water for foraging and vegetation for nest-building, favourable climate conditions at lower Brazilian latitudes during the LGM are likely to have allowed the establishment of populations.…”
Section: Genetic Diversity Demographic Expansion and Effective Populmentioning
confidence: 99%