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Extra resources for The Great Basin: A Natural Prehistory
1978), Tanner (1978), N. E. West et al. (1978), show (1979), and P. V. Wells (1983). N. E. West et al. (1978) extend at the function of thermal inversions within the improvement of pinyon-juniper forest. Tueller et al. (1979) and N. E. West, Tausch, and Tueller (1998) supply vital discussions of serious Basin pinyon-juniper wooded area as a complete; i've got relied seriously on those (see additionally Hidy and Klieforth 1990). an enormous literature offers with the hot growth of pinyon and juniper; right here, i've got emphasised the contributions by way of Tueller et al. (1979); Tausch, West, and Nabi (1981); R. F. Miller and Rose (1995, 1999); West, Tausch, and Tueller (1998); R. F. Miller, Svejcar, and Rose (2000); R. F. Miller and Tausch (2001); R. F. Miller et al. (2005); Bradley and Fleishman (2008); and Charlet (2008). The estimate that pinyon-juniper woodlands now conceal ten instances the territory they coated a few a hundred and fifty years in the past is repeated in lots of locations: see, for example, Suring et al. (2005). Janetski (1999b) presents a good precis of using pinyon-juniper woodlands by way of the local peoples of the nice Basin. Treelines often are mentioned in a great ebook via Arno and Hammersly (1984); see additionally Stevens and Fox (1991). For extra on krummholz, see LaMarche and Mooney (1972), Marr (1977), and W. okay. Smith and Knapp (1990). Caveney et al. (2001) supply a huge research of the chemical contents of Ephedra. info on ephedrine and pseudoephedrine are greatly to be had, yet Salocks and Kaley (2003) offer a handy synthesis. Many ethnographers have mentioned using Ephedra via local americans within the nice Basin; Zigmond (1981), C. S. Fowler (1992), and Rhode (2002) are sturdy locations to begin. My dialogue of organic soil crusts attracts seriously on Belnap (2003, 2006), Belnap and Eldredge (2003), Belnap et al. (2001), and Belnap, Phillips, and Troxler (2006). if you would like a basic advent to those crusts, visit www. soilcrust. org (see “Crust 101”); Rosentreter, Bowker, and Belknap (2007) offer a short advent to the subject, besides a very good box consultant to the organisms of which they're composed. Wohlfahrt, Fenstermaker, and Arnone (2008) argue that soil crusts might act as a carbon dioxide sink, yet this recommendation isn't really permitted by means of all, or even soil crust specialist Belnap questions this probability (Stone 2008). My dialogue of serious Basin montane and subalpine conifers has relied not just at the references supplied above but in addition on David Charlet’s learn, which has dramatically altered our knowing of the distribution of conifers within the nice Basin (Charlet 2007, 2009a). DeLucia and Schlesinger (1990) current an outstanding evaluation of the examine that has been performed at the disjunct distribution of Sierran conifers on altered soils within the western nice Basin. the whole info of that learn are in DeLucia, Schlesinger, and Billings (1988, 1989); Schlesinger, DeLucia, and Billings (1989); and DeLucia and Schlesinger (1991). Billings (1950) was once the 1st to monitor and interpret those Sierra “tree islands.