Mammals of south‐east Asian islands and their Late Pleistocene environments

By Erik Meijaard. 2003

193 citations recorded by the source corpus.

Subfields: Geography, Planning and Development, Paleontology, Social Psychology

View Paper: https://www.semanticscholar.org/paper/0aa9cb3dfbaba5599da280c0a04cade889e2460e

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Citations in the corpus

Biogeography of the Indo-Australian Archipelago (2011, background): “…inferred by combining global predictions based on these data with regional data on pollen, diatom and sedimentary studies of lake and bog cores (Dam et al. 2001a), faunal distributions (Meijaard 2003), magnetic susceptibility of sediments (Tamuntuan et al. 2010), and landscape features (Hope 2007).”
Assembly and division of the South and South-East Asian flora in relation to tectonics and climate change (2018, background): “…whether or not there was a ‘savanna corridor’ across the submerged shelf for the dispersal of elements of the Siwalik savanna fauna to Java (Bird et al. 2005, Cannon et al. 2009, Heaney 1991, Kershaw et al. 2002, Medway 1972, Meijaard 2003, Morley & Flenley 1987, Voris 2000, Wurster et al. 2010).”
ASSESSING THE TAXONOMIC STATUS OF THE PALAWAN PANGOLIN MANIS CULIONENSIS (PHOLIDOTA) USING DISCRETE MORPHOLOGICAL CHARACTERS (2005, background): “…from Borneo to Greater Palawan through Early Pleistocene land bridges (in accordance with other terrestrial vertebrate–based scenarios—Heaney 1986; Meijaard 2003; Tougard 2001) and subsequent isolation after rise of sea level about 800,000–500,000 years ago (EPICA 2004; Rohling et al. 1998).”
The Indochinese–Sundaic zoogeographic transition: a description and analysis of terrestrial mammal species distributions (2009, methodology): “The areal extent and distribution of savanna and rain forest (and rain forest refugia) are still controversial (Sun et al., 2000, 2003; Taylor et al., 2001; Meijaard, 2003; Bird et al., 2005; Tougard & Montuire, 2006; Kershaw et al., 2007; Morley, 2007), but the implications of these palaeoenvironme”
Biogeography and conservation in Southeast Asia: how 2.7 million years of repeated environmental fluctuations affect today’s patterns and the future of the remaining refugial-phase biodiversity (2010, background): “The extent to which a continuous or broken savanna corridor covered parts of the Sunda Shelf from Indochina to Borneo is controversial as the evidence is mixed and often sitespecific (Kershaw et al. 2001, 2007; Meijaard 2003; Bird et al. 2005; Meijaard and Groves 2006; Wang et al. 2009).”
Palaeoecology of Southeast Asian megafauna‐bearing sites from the Pleistocene and a review of environmental changes in the region (2010, background): “In particular, the presence of a central savanna corridor running through the middle of Sundaland, as proposed by a number or researchers (e.g. Heaney, 1991; Meijaard, 2003; Bird et al., 2005), should be traceable through an ecological analysis of fossil faunas.”
The state and conservation of Southeast Asian biodiversity (2010, background): “Shifting paleoclimates caused periodic fluctuations in sea level, in turn enabling migrations from the mainland to the Indo-malayan archipelago and isolating islands (Meijaard 2003).”