Biogeography and migration routes of large mammal faunas in South-East Asia during the Late Middle Pleistocene: focus on the fossil and extant faunas from Thailand

By C. Tougard. 2001

177 citations recorded by the source corpus.

Subfields: Atmospheric Science, Geology, Paleontology

View Paper: https://www.semanticscholar.org/paper/b7ec02b5532cdb4e62e00a6a778a9ef138a11218

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Atmospheric Science

In Geology

In Paleontology

Citations in the corpus

Large mammal fossil occurrences and associated archaeological evidence in Pleistocene contexts of peninsular India and Sri Lanka (2008, unknown): “This is unfortunate because although not a part of peninsular India, the northeast region may represent a critical biogeographic corridor between the Pleistocene fauna, including Homo populations, of South Asia (Nanda, this volume) and Southeast Asia (e.g., Hooijer, 1949; Tougard, 2001).”
Evolutionary history of the Paradoxurus palm civets – a new model for Asian biogeography (2010, background): “Fossil records of Paradoxurus exist from the Late Pleistocene to the Holocene transition (Borneo, Medway, 1966; Piper et al., 2008; Java, van den Bergh et al., 2001; South China, Wang et al., 2007; Thailand, Tougard, 2001; Vietnam, Schwartz et al., 1994).”
Characteristics of Pleistocene megafauna extinctions in Southeast Asia (2007, methodology): “Phnom Loang is described as Middle Pleistocene by Tougard (2001), while Carbonnel and Guth (1968) attribute a lower to middle Pleistocene age on the basis of the presence ofDicerorhinus mercki and Crocuta crocuta.”
The Late Pleistocene Duoi U’Oi cave in northern Vietnam: palaeontology, sedimentology, taphonomy and palaeoenvironments (2008, background): “unicornis had been reported so far in the late Middle Pleistocene in North Vietnam and Thailand (Tougard, 2001; Bacon et al., 2004).”
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, background): “According to tradition, the mammalian transition also occurs near the Isthmus of Kra (Chasen, 1940; Musser & Newcomb, 1983; Cranbrook, 1988; Lekagul & McNeely, 1988; Corbet & Hill, 1992; Chaimanee, 1998; Francis, 2001; Tougard, 2001; Luo et al., 2004; Sodhi & Brook, 2006), but this has never been fo”
Palaeoecology of Southeast Asian megafauna‐bearing sites from the Pleistocene and a review of environmental changes in the region (2010, background): “In our analysis, this latter site (Thum Wimam Nakin) is classified as representing a mixed habitat, which agrees with previous palaeoenvironmental reconstructions suggesting that it represents ‘a slightly open forested environment’ (Tougard & Montuire, 2006).”
Neogene marine transgressions, palaeogeography and biogeographic transitions on the Thai–Malay Peninsula (2003, background): “Tougard (2001) reviews records of large mammal species (primates, carnivores, proboscidians, perissodactyls and artiodactyls) from thirteen Middle Pleistocene sites and five Late Pleistocene sites in Southeast Asia.”