Proc 2nd Asia-Pacific conf sustainable

agric, Phitsanulok

Proc 2nd Asia-Pacific conf sustainable

agric, Phitsanulok, Dorsomorphin Thailand, pp 55–62 Woodruff DS (2003a) Neogene marine transgressions, paleogeography and biogeographic transitions on the Thai-Malay Peninsula. J Biogeogr 30:551–567CrossRef Woodruff DS (2003b) The location of the Indochinese-Sundaic biogeographic transition in plants and birds. Nat Hist Bull Siam Soc 51:97–108 Woodruff DS (2003c) Non-invasive genotyping and field studies of free-ranging non-human primates. In: Chapais B, Berman C (eds) Kinship and behavior in primates. Oxford University Press, Oxford, pp 46–68 Woodruff DS (2006) Genetics and the future of biodiversity. Keynote talk: Proc. 9th Annu Thai biodiversity research & training progr, Bangkok, pp 20–29 Woodruff DS (2008) International impacts LXH254 concentration of damming the Mekong River. In: DiFrancesco K, Woodruff K (eds) Global perspectives on large dams. Evaluating the state of large dam construction and decommissioning across the world. Report No 13, Yale School of Forestry & Environmental Studies, New Haven, pp 85–89 Woodruff DS, Turner LM (2009) The Indochinese–Sundaic zoogeographic transition: a description of terrestrial mammal species distributions. J Biogeogr 36:803–821 Woodruff DS, Woodruff KA (2008) Paleogeography, buy G418 global sea level changes, and the future coastline of Thailand. Nat Hist Bull Siam Soc 56:1–24 World Bank (2009)

World development report 2010: development and climate change. The World Bank, Washington DC (www.​worldbank.​org/​wdr2010). See: Focus PDK4 B. Biodiversity and ecosystem

services in a changing climate, pp 124–131 World Wildlife Fund (2009) Heart of Borneo. http://​www.​wwf.​or.​id/​en/​about_​wwf/​whatwedo/​hob/​abouthob/​ Wright SJ, Muller-Landau HC, Schipper J (2009) The future of tropical species on a warmer planet. Conserv Biol 23:1418–1426PubMed Ziegler AD, Bruun TB, Guardiola-Claramonte M, Giambelluca TW, Lawrence D, Lam NT (2009) Environmental consequences of the demise in swidden cultivation in montane mainland Southeast Asia: hydrology and geomorphology. Human Ecol 37:361–373″
“Introduction Tropical rainforests, especially montane forests, are rich in epiphytic bryophytes (Richards 1984; Frahm and Gradstein 1991; Parolly and Kürschner 2004). These plants play an important role in the water balance and nutrient cycling of the forest (Pócs 1980; Nadkarni 1984; Hofstede et al. 1994; but see Hölscher et al. 2004), and function as substrate, food source and nesting material for numerous other rainforest organisms (e.g., Nadkarni and Matelson 1989; Yanoviak et al. 2007). Several recent studies have described the species composition and richness of epiphytic bryophytes at different height levels on rainforest trees, as well as substrate preferences within the host trees (e.g., Cornelissen and Ter Steege 1989; Wolf 1993a, b, 1996; Gradstein et al. 2001b; Holz et al. 2002; Acebey et al. 2003).

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