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Changes in soil bacterial community profiles associated with ...

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40Ryoichi DOI, Pongsak SAHUNALU, Chongrak WACHRINRAT, Sakhan TEEJUNTUK and Katsutoshi SAKURAI<strong>community</strong> <strong>profiles</strong>. Thus, the primary objective of this research was the determ<strong>in</strong>ation of a degradation gradient as a resultof the elim<strong>in</strong>ation of the tropical forest by multivariate profil<strong>in</strong>g of <strong>soil</strong> <strong>bacterial</strong> communities us<strong>in</strong>g antibiotics and carbonsources.The orig<strong>in</strong>al vegetative type of the Sakaerat Environmental Research Station (SERS), Thailand is dry evergreen forest(DEF), but there are other vegetative types reflect<strong>in</strong>g anthropologic degradation (Kaeoniam et al., 1976). Bare ground (BG)is the most degraded status <strong>in</strong> the SERS (Doi & Sakurai, 2003). Compositional data sets on <strong>soil</strong> <strong>bacterial</strong> communities wereobta<strong>in</strong>ed for DEF and BG <strong>soil</strong>s. The multivariate profil<strong>in</strong>g methods, the antibiotic resistance MPN method (method 1), theantibiotic disk diffusion method (method 2) and the Biolog method (Garland & Mills, 1991) were applied. To <strong>in</strong>vestigate thepossible utilization of the <strong>in</strong>formation given by the above profil<strong>in</strong>g methods, the compositional data sets were analyzed bypr<strong>in</strong>cipal component analysis, Wilk’s lambda determ<strong>in</strong>ation and redundancy analysis.MATERIALS AND METHODSSite descriptionThe Sakaerat Environmental Research Station (SERS), Wang Nam Kiao district, Nakhon Ratchasima (14°30’N, 101°55E)was established <strong>in</strong> 1967. At the time of establishment, some parts of the area had already been disturbed and deforested byhuman activities (Kaeoniam et al., 1976).The area is 7,808 hectares, and the altitude ranges from 250 to 762 m above sea level. The <strong>soil</strong> is classified as an Ultisolaccord<strong>in</strong>g to the USDA scheme (USDA Soil Conservation Service, 1975). The major vegetative types <strong>in</strong>clude dry evergreenforest (DEF), dry deciduous forest (DDF) and plantation plots, and others, such as bare ground (BG) and grassland. Thesevegetative types form a mosaic as shown <strong>in</strong> Fig. 1 (Kaeoniam et al., 1976). The climate is classified as Aw accord<strong>in</strong>g to theKöppen classification (Köppen, 1931). The annual precipitation is 1,260 mm and the average temperature is 26°C(Bunyavejchew<strong>in</strong>, 1986). Approximately, the dry season starts <strong>in</strong> November and ends <strong>in</strong> late April. The site receives most ofthe annual precipitation dur<strong>in</strong>g the ra<strong>in</strong>y season, approximately May to October.Soil sampl<strong>in</strong>g was done at the DEF and the BG. The DEF is primarily dom<strong>in</strong>ated by Hopea ferrea and Shorea spp. thatform the upper story, 20 to 40 m above ground. A typical DEF fosters more than 1,000 trees (trunk diameter at breastheight, DBH>5 cm) ha -1 , and the total basal area at 1.3 m height exceeds 30 m 2 ha -1 and the above ground biomass is over 200tons ha -1 (Kanzaki et al., 1995). The BG, hav<strong>in</strong>g no vegetation as a result of the past deforestation and subsequent humanactivities, is also scattered <strong>in</strong> the plot <strong>in</strong> a mosaic configuration.Fig1Vegetative typeDDF105ºE 110ºEDEFDDF and DEF20ºNPlantationThailandBangkok15ºNN11SERS22OthersSampl<strong>in</strong>g po<strong>in</strong>tsBGDEF5 kmFig. 1. Map of the Sakaerat Environmental Research Station and the sampl<strong>in</strong>g po<strong>in</strong>ts. DEF, DDF and BG<strong>in</strong>dicate dry evergreen forest, dry deciduous forest and bare ground, respectively. The triangle anddiamond <strong>in</strong>dicate sampl<strong>in</strong>g po<strong>in</strong>ts at the DEF and the BG, respectively. The figures <strong>in</strong> the symbolsare replication numbers.

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