Soil moisture is the major factor influencing microbial community structure and enzyme activities across seven biogeoclimatic zones in western Canada

被引:870
作者
Brockett, Beth F. T. [1 ]
Prescott, Cindy E. [1 ]
Grayston, Sue J. [1 ]
机构
[1] Univ British Columbia, Dept Forest Sci, Belowground Ecosyst Grp, Vancouver, BC V6T 1Z4, Canada
基金
加拿大自然科学与工程研究理事会;
关键词
Forest; Enzymes; PLFA; Soil moisture; Soil microorganisms; Climate; BOREAL FOREST SOILS; DOUGLAS-FIR FORESTS; ORGANIC-MATTER; NITROGEN AVAILABILITY; BACTERIAL BIOMASS; BRITISH-COLUMBIA; DEPTH PROFILES; ARABLE SOILS; DIVERSITY; LANDSCAPE;
D O I
10.1016/j.soilbio.2011.09.003
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
Although soil microorganisms play a central role in the soil processes that determine nutrient availability and productivity of forest ecosystems, we are only beginning to understand how microbial communities are shaped by environmental factors and how the structure and function of soil microbial communities in turn influence rates of key soil processes. Here we compare the structure and function of soil microbial communities in seven mature, undisturbed forest types across a range of regional climates in British Columbia and Alberta, and examine the variation in community composition within forest types. We collected the forest floor fermentation (F) and humus (H) layers and upper 10 cm of mineral soil at 3 sites in each of seven forest types (corresponding to seven Biogeoclimatic zones) in both spring and summer. Phospholipid fatty acid analysis was used to investigate the structure of soil microbial communities and total soil microbial biomass; potential activities of extra-cellular enzymes indicated the functional potential of the soil microbial community in each layer at each site. Multivariate analysis indicated that both structure and enzyme activities of soil microbial communities differed among the forest types, and significantly separated along the regional climate gradient, despite high local variation. Soil moisture and organic matter contents were most closely related to microbial community characteristics. Forests in the Ponderosa Pine and Mountain Hemlock zones were distinct from other forests and from each other when comparing potential enzyme activities and had the most extreme moisture and temperature values. Forest floors from the hot and dry Ponderosa Pine forests were associated with enzymes characteristic of water-stress and high concentrations of phenols and other recalcitrant compounds. The wet and cold Mountain Hemlock forests were associated with low enzyme activity. An influence of tree species was apparent at the three sites within the Coastal Western Hemlock zone; high bacterial:fungal biomass ratios were found under western redcedar (Thuja plicata) which also had high pH and base-cation levels, and under Douglas-fir (Pseudotsuga menziesii), which had high N availability. Potential activities enzymes differed among soil layers: potential activities of phenol oxidase and peroxidase were highest in mineral soil, whereas phosphatase, betaglucosidase. NAGase, sulfatase, xylosidase and cellobiohydrolase were highest in the forest floors. (C) 2011 Elsevier Ltd. All rights reserved.
引用
收藏
页码:9 / 20
页数:12
相关论文
共 92 条
[1]   Changes in enzyme activities and soil microbial community composition along carbon and nutrient gradients at the Franz Josef chronosequence, New Zealand [J].
Allison, V. J. ;
Condron, L. M. ;
Peltzer, D. A. ;
Richardson, S. J. ;
Turner, B. L. .
SOIL BIOLOGY & BIOCHEMISTRY, 2007, 39 (07) :1770-1781
[2]   Using landscape and depth gradients to decouple the impact of correlated environmental variables on soil microbial community composition [J].
Allison, V. J. ;
Yermakov, Z. ;
Miller, R. M. ;
Jastrow, J. D. ;
Matamala, R. .
SOIL BIOLOGY & BIOCHEMISTRY, 2007, 39 (02) :505-516
[3]   Assessing soil microbial community composition across landscapes: Do surface soils reveal patterns? [J].
Allison, Victoria J. ;
Allison, Victoria J. ;
Yermakov, Zhanna ;
Miller, R. Michael ;
Jastrow, Julie D. ;
Matamala, Roser .
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 2007, 71 (03) :730-734
[4]  
Anderson MJ, 2001, AUSTRAL ECOL, V26, P32, DOI 10.1111/j.1442-9993.2001.01070.pp.x
[5]   PHENOLICS IN ECOLOGICAL INTERACTIONS - THE IMPORTANCE OF OXIDATION [J].
APPEL, HM .
JOURNAL OF CHEMICAL ECOLOGY, 1993, 19 (07) :1521-1552
[6]  
BAATH E, 1992, APPL ENVIRON MICROB, V58, P4026
[7]   Variation in soil microbial communities across a boreal spruce forest landscape [J].
Bach, Lisbet Holm ;
Frostegard, Asa ;
Ohlson, Mikael .
CANADIAN JOURNAL OF FOREST RESEARCH-REVUE CANADIENNE DE RECHERCHE FORESTIERE, 2008, 38 (06) :1504-1516
[8]   The measurement of soil fungal:bacterial biomass ratios as an indicator of ecosystem self-regulation in temperate meadow grasslands [J].
Bardgett, RD ;
McAlister, E .
BIOLOGY AND FERTILITY OF SOILS, 1999, 29 (03) :282-290
[9]   Exploring soil microbial communities and soil organic matter: Variability and interactions in arable soils under minimum tillage practice [J].
Bausenwein, U. ;
Gattinger, A. ;
Langer, U. ;
Embacher, A. ;
Hartmann, H. -P. ;
Sommer, M. ;
Munch, J. C. ;
Schloter, M. .
APPLIED SOIL ECOLOGY, 2008, 40 (01) :67-77
[10]  
BLIGH EG, 1959, CAN J BIOCHEM PHYS, V37, P911