1981
DOI: 10.1007/978-94-009-8629-9_22
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Australian rainforests: patterns and change

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Cited by 186 publications
(181 citation statements)
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“…For instance, the proportion of species with wind-dispersed propagules in our sample was 21%, with representatives from 12 families. By contrast, the available data shows that wind dispersal is rare in lowland rain-forest trees of North Queensland (Irvine & Armstrong 1990, Webb & Tracey 1981 and Costa Rica (Levey et al 1994), although it does reach 16% for the large trees of Barro Colorado Island moist forest (Gentry 1982). The relatively high proportion of wind dispersal in New Caledonia may be related to nutrient-deficient soils and the low diversity of vertebrates.…”
Section: Discussionmentioning
confidence: 99%
“…For instance, the proportion of species with wind-dispersed propagules in our sample was 21%, with representatives from 12 families. By contrast, the available data shows that wind dispersal is rare in lowland rain-forest trees of North Queensland (Irvine & Armstrong 1990, Webb & Tracey 1981 and Costa Rica (Levey et al 1994), although it does reach 16% for the large trees of Barro Colorado Island moist forest (Gentry 1982). The relatively high proportion of wind dispersal in New Caledonia may be related to nutrient-deficient soils and the low diversity of vertebrates.…”
Section: Discussionmentioning
confidence: 99%
“…The climatic oscillations of the Late Quaternary, with greatly reduced temperature and rainfall at the Last Glacial Maximum ( LGM, 18 thousand years before present, 18 Kya), followed by a permissive cool-wet phase in the Early Holocene (8-7.5 Kya) and then a warm-wet phase (5-3.5 Kya) prior to the establishment of current conditions ( Kershaw & Nix 1988), had profound effects on the distribution of rainforests and of rainforest-dependent fauna in the Wet Tropics ( Williams & Pearson 1997;Graham et al 2006). Retraction of Wet Tropics rainforest to refugia during restrictive climates, the LGM in particular, is supported by evidence from palynology ( Kershaw 1994;Kershaw et al 2005), phytogeography ( Webb & Tracey 1981) and also by spatial modelling of rainforests under varying climates ( Nix 1991;Graham et al 2006;Hilbert et al 2007;VanDerWal et al 2008). Predicted Late Quaternary refugia (figure 1b) vary in spatial scale and connectivity, with a major disjunction centred on the Black Mountain Corridor ( BMC) that separates multiple small refugia in the north from a major refugial area along and adjacent to the escarpment of the Moussalli et al (in press) central Wet Tropics.…”
Section: Introductionmentioning
confidence: 94%
“…In general, attempts to locate and circumscribe historical refugia in tropical rainforest systems have proved contentious (41,42), and the same is true for the Australian wet tropics where there is some discrepancy between inferences from paleoclimatic models (12), current phytogeography (17), and evidence for drier sclerophyll vegetation and burning within putative refugia (20). Although consistent phylogeographic divisions across the BMC in vertebrates support the division between the major northern and southern refugia predicted by modeling (22), further details are obscured for vertebrates by varying histories of local extinction and expansion, stochastic variance of gene trees, or both (43).…”
Section: Implications For Biogeography and Evolution In The Wet Tropicsmentioning
confidence: 99%
“…This long-term decline, and particularly the Pleistocene climate oscillations, appears to have driven cycles of contraction and expansion of rainforest, probably structured around montane remnants surrounded by dry sclerophyll woodlands (16). These montane blocks are centers of endemism and have been proposed as Pleistocene refugia (17)(18)(19), and form the basis of the recognized subregions within the Wet Tropics (see Table 1 and Fig. 1).…”
mentioning
confidence: 99%