Quaternary rainforest refugia in south‐east Asia: using termites (Isoptera) as indicators
By F. Gathorne-Hardy, Syaukani, R. G. Davies, P. Eggleton, David T. Jones. 2002
223 citations recorded by the source corpus.
Subfields: Ecology, Evolution, Behavior and Systematics, Genetics, Nature and Landscape Conservation
View Paper: https://www.semanticscholar.org/paper/20b06c0e5efff3902a1a6a36c7c49063be6b5707
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In Ecology, Evolution, Behavior and Systematics
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Citations in the corpus
- The Indochinese–Sundaic faunal transition at the Isthmus of Kra: an analysis of resident forest bird species distributions (2003, background): “Similarly, there is no clear relationship between the inferred positions of the rain forest refugia in southeast Asia and the position(s) of today’s transitions (Morley, 2000; Kershaw et al., 2001; Gathorne-Hardy et al., 2002).”
- A floristic analysis of the lowland dipterocarp forests of Borneo (2003, background): “…periods south-western Borneo consisted mainly of savanna vegetation with some scattered rain forest fragments along major rivers and on mountain slopes, while northern and eastern Borneo remained covered with rain forest (Heaney, 1991; Verstappen, 1992; Thomas, 2000; Gathorne-Hardy et al., 2002).”
- Termite assemblage collapse along a land-use intensification gradient in lowland central Sumatra, Indonesia (2003, background): “…land-use types in the Sunda region showed that the Jambi primary forest transect was very similar in overall taxonomic and functional composition to the other lowland forest transects run in sites that had remained as rainforest throughout the Quaternary period (Gathorne-Hardy et al. 2002).”
- Vicariance or dispersal? Historical biogeography of three Sunda shelf murine rodents (Maxomys surifer, Leopoldamys sabanus and Maxomys whiteheadi) (2004, background): “Second, a study of termite community composition found evidence of former refuges in northern Sumatra and northern and eastern Borneo based on information about rain-forest- and savannatype termite faunas (Gathorne-Hardy et al., 2002).”
- Evolutionary history of the Paradoxurus palm civets – a new model for Asian biogeography (2010, background): “…were probably shaped by major Plio-Pleistocene events, including eustatic (Haq et al., 1987; Miller et al., 2005), climatic and vegetational (Gathorne-Hardy et al., 2002; Bird et al., 2005) changes that have been documented to have influenced the biogeography of other mammals (e.g. Heaney,…”
- Primate Biogeography and Ecology on the Sunda Shelf Islands: A Paleontological and Zooarchaeological Perspective (2006, background): “During these glacial periods, beginning in the Late Pliocene, a belt of dry woodland and savanna probably extended southwards from the eastern side of the Malay Peninsula, through southern and eastern Borneo, to eastern Java and the Lesser Sunda Islands (Morley and Flenley, 1987; Heaney, 1991; Gatho”
- Characteristics of Pleistocene megafauna extinctions in Southeast Asia (2007, background): “The extent of these zones is controlled by a number of factors: temperature and rainfall, and in particular for Southeast Asia (but unlike Africa or America), sea level changes (Heaney, 1991; Gathorne-Hardy et al., 2002).”
- Neogene marine transgressions, palaeogeography and biogeographic transitions on the Thai–Malay Peninsula (2003, background): “More recently, Gathorne-Hardy et al. (2002) have used current termite community distribution patterns to infer the location of the rain forest refugia and reached similar conclusions.”
- Systematics of a widespread Southeast Asian frog, Rana chalconota (Amphibia: Anura: Ranidae) (2009, background): “Isolated minor refugia in sheltered valleys may have persisted elsewhere (Gathorne-Hardy et al., 2002) on the continental peninsula.”
- A Biogeographic Synthesis of the Amphibians and Reptiles of Indochina (2011, background): “This event, and the possible weakening of the summer monsoons, resulted in a seasonal climate (An et al., 2001; Gupta and Thomas, 2003) that was associated with an overall reduction in the extent of humid forest (Gathorne-Hardy et al., 2002).”
- Mammals of south‐east Asian islands and their Late Pleistocene environments (2003, background): “, 2000), mainly because of its dynamic geological past (Holloway & Hall, 1998), relatively stable climatic conditions (Gathorne-Hardy et al., 2002) and associated rapid speciation processes (e.”