title: [Comparisons of Microbial Numbers, Biomasses and Soil Enzyme Activities Between Paddy Field and Drvland Origins in Karst Cave Wetland].
abstract: The purpose of this study is to compare microbial number, microbial biomass as well as soil enzyme activity between paddy field and dryland originated karst wetland ecosystems. The soil samples (0-20 cm) of uncultivated wetland, paddy field and dryland were collected in Huixian karst cave wetland, Guilin, China. Microbial numbers and biomass were detected using dilute plate incubation counting and chloroform fumigation-extraction, respectively. Microbial DNA was extracted according to the manufacturer's instructions of the kit. Microbial activity was examined using soil enzyme assays as well. The result showed that the bacteria number in paddy filed was (4.36 +/- 2.25) x 10(7) CFU x g(-1), which was significantly higher than those in wetland and dryland. Fungi numbers were (6.41 +/- 2.16) x 10(4) CFU x g(-1) in rice paddy and (6.52 +/- 1.55) x 10(4) CFU x g(-1) in wetland, which were higher than that in dryland. Actinomycetes number was (2.65 +/- 0.72) x 10(6) CFU x g(-1) in dryland, which was higher than that in wetland. Microbial DNA concentration in rice paddy was (11.92 +/- 3.69) microg x g(-1), which was higher than that in dryland. Invertase activity was (66.87 +/- 18.61) mg x (g x 24 h)(-1) in rice paddy and alkaline phosphatase activity was (2.07 +/- 0.99) mg x (g x 2 h)(-1) in wetland, both of which were higher than those in dryland. Statistical analysis showed there was a significant positive correlation of microbial DNA content, alkaline phosphatase activity and microbial carbon with soil pH, soil organic carbon (SOC), total nitrogen, alkali-hydrolyzable nitrogen, soil moisture, exchangeable Ca2+ and exchangeable Mg2+, as well as a significant positive correlation of intervase activity with the former three microbial factors. The above results indicated that microbial biomass and function responded much more sensitively to land-use change than microbial number in karst cave wetland system. Soil moisture, SOC and some factors induced by land-use change could affect mainly microbiological characteristics. We suggest that rice paddy, a kind of constructed wetland, should be kept and protected in experimental area or buffer area of Huixian karst cave wetland in the light of its similar property with the natural wetland.
authors.forename: Zhen-jiang
authors.initials: ZJ
authors.lastname: Jin
authors.forename: Hong-hu
authors.initials: HH
authors.lastname: Zeng
authors.forename: Qiang
authors.initials: Q
authors.lastname: Li
authors.forename: Ya-ping
authors.initials: YP
authors.lastname: Cheng
authors.forename: Hua-feng
authors.initials: HF
authors.lastname: Tang
authors.forename: Min
authors.initials: M
authors.lastname: Li
authors.forename: Bing-fu
authors.initials: BF
authors.lastname: Huang
mesh_terms: D001419:Bacteria; D018533:Biomass; D002244:Carbon / Q000032:analysis; D059552:Caves / Q000737:chemistry*; D002681:China; D004798:Enzymes / Q000032:analysis; D005658:Fungi; D009584:Nitrogen / Q000032:analysis; D012275:Oryza; D012987:Soil / Q000737:chemistry*; D012988:Soil Microbiology; D053833:Wetlands
chemical_list: D004798:Enzymes; D012987:Soil; D002244:Carbon; D009584:Nitrogen