Distribution and Composition of Cyanobacteria and Microalgae Associated with Biological Soil Crusts in the Gurbantunggut Desert, China

被引:40
作者
Zhang, Bingchang [1 ]
Zhang, Yuanming [1 ]
Downing, Alison [2 ]
Niu, Yulu [3 ]
机构
[1] Chinese Acad Sci, Xinjiang Inst Ecol & Geog, Key Lab Biogeog & Bioresources Arid Land, Urumqi 830011, Peoples R China
[2] Macquarie Univ, Dept Biol Sci, N Ryde, NSW 2109, Australia
[3] Hengshui Univ, Coll Life Sci, Hengshui, Peoples R China
基金
中国国家自然科学基金; 中国科学院西部之光基金;
关键词
cyanobacteria; microalgae; microbiotic soil crusts; spatial distribution; species composition; MICROBIOTIC CRUSTS; GREEN-ALGAE; COMMUNITIES; DIVERSITY; MICROSTRUCTURE; MICROORGANISMS; PATTERNS; XINJIANG; GROWTH; FOREST;
D O I
10.1080/15324982.2011.565858
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
In Gurbantunggut Desert, cyanobacterial and microalgal components were characterized within 60 soil samples collected from sand dunes. Fifty-one taxa of cyanobacteria and algae were identified. Without exception, the soils were alkaline, poor in nutrients, and showed large variations in other soil properties. Spatial heterogeneity for distribution of cyanobacteria and microalgae (diversity of morphotypes, species composition, and microbiomass) existed. Compared with other deserts in the world, the Gurbantunggut Desert has a greater diversity of cyanobacterial-microalgal morphotypes. Results from step regression showed that the diversity of morphotype was determined by total P, available P, and soil layer. Filamentous cyanobacteria dominated the community. Microcoleus vaginatus (Vauch.) Gom was the dominant species in most positions on sand dune, while the abundance of other dominant species varied depending on the sand dune position and the soil layer in which they occurred. The microalgal biomass was influenced by the content of Mg, crust type, soil moisture, sunlight, and oxygen concentration. A significant positive relation was found between microalgal biomass and diversity of morphotype. Species composition, diversity of morphotype, and microalgal biomass interacted with each other. The contents of P and Mg ion, soil texture, and soil moisture may be the main factors responsible for cyanobacterial-microalgal distribution.
引用
收藏
页码:275 / 293
页数:19
相关论文
共 53 条
[1]   Cyanobacterial inoculation of heated soils:: effect on microorganisms of C and N cycles and on chemical composition in soil surface [J].
Acea, MJ ;
Prieto-Fernández, A ;
Diz-Cid, N .
SOIL BIOLOGY & BIOCHEMISTRY, 2003, 35 (04) :513-524
[2]  
ADRIAAN JG, 2004, J BIOL INORG CHEM, V9, P109
[3]  
ANAGNOSTIDIS K, 1988, Archiv fuer Hydrobiologie Supplement, V80, P327
[4]  
Anagnostidis K., 1990, Algological Studies/Archiv fur Hydrobiologie, Supplement Volumes, V59, P1
[5]  
ASHLEY J, 1984, RECLAM REVEG RES, V3, P49
[6]   Protozoa of biological soil crusts of a cool desert in Utah [J].
Bamforth, S. S. .
JOURNAL OF ARID ENVIRONMENTS, 2008, 72 (05) :722-729
[7]  
BELNAP J, 1993, GREAT BASIN NAT, V53, P40
[8]   Impacts of off road vehicles on nitrogen cycles in biological soil crusts: resistance in different US deserts [J].
Belnap, J .
JOURNAL OF ARID ENVIRONMENTS, 2002, 52 (02) :155-165
[9]  
BELNAP J, 2003, BIOL SOIL CRUSTS STR, V150, P241
[10]   Temporal variation in community composition, pigmentation, and Fv/Fm of desert cyanobacterial soil crusts [J].
Bowker, MA ;
Reed, SC ;
Belnap, J ;
Phillips, SL .
MICROBIAL ECOLOGY, 2002, 43 (01) :13-25