In situ spatial patterns of soil bacterial populations, mapped at multiple scales, in an arable soil

被引:156
作者
Nunan, N [1 ]
Wu, K
Young, IM
Crawford, JW
Ritz, K
机构
[1] Scottish Crop Res Inst, Soil Plant Dynam Unit, Dundee DD2 5DA, Scotland
[2] Univ Abertay Dundee, SIMBIOS Ctr, Dundee DD1 1HG, Scotland
[3] Cranfield Univ, Natl Soil Resources Inst, Silsoe MK45 4DT, Beds, England
关键词
D O I
10.1007/s00248-002-2021-0
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
Very little is known about the spatial organization of soil microbes across scales that are relevant both to microbial function and to field-based processes. The spatial distributions of microbes and microbially mediated activity have a high intrinsic variability. This can present problems when trying to quantify the effects of disturbance, management practices, or climate change on soil microbial systems and attendant function. A spatial sampling regime was implemented in an arable field. Cores of undisturbed soil were sampled from a 3 x 3 x 0.9 m volume of soil (topsoil and subsoil) and a biological thin section, in which the in situ distribution of bacteria could be quantified, prepared from each core. Geostatistical analysis was used to quantify the nature of spatial structure from micrometers to meters and spatial point pattern analysis to test for deviations from complete spatial randomness of mapped bacteria. Spatial structure in the topsoil was only found at the microscale (micrometers), whereas evidence for nested scales of spatial structure was found in the subsoil (at the microscale, and at the centimeter to meter scale). Geostatistical ranges of spatial structure at the micro scale were greater in the topsoil and tended to decrease with depth in the subsoil. Evidence for spatial aggregation in bacteria was stronger in the topsoil and also decreased with depth in the subsoil, though extremely high degrees of aggregation were found at very short distances in the deep subsoil. The data suggest that factors that regulate the distribution of bacteria in the subsoil operate at two scales, in contrast to one scale in the topsoil, and that bacterial patches are larger and more prevalent in the topsoil.
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页码:296 / 305
页数:10
相关论文
共 26 条
[1]  
[Anonymous], 1994, EXPLOITATION ENV HET
[2]   Manuring and soil type influence on spatial variation of soil organic matter properties [J].
Bragato, G ;
Primavera, F .
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 1998, 62 (05) :1313-1319
[3]   Preferential flow paths: biological 'hot spots' in soils [J].
Bundt, M ;
Widmer, F ;
Pesaro, M ;
Zeyer, J ;
Blaser, P .
SOIL BIOLOGY & BIOCHEMISTRY, 2001, 33 (06) :729-738
[4]   Spatial patterns of rhizoplane populations of Pseudomonas fluorescens [J].
Dandurand, LM ;
Schotzko, DJ ;
Knudsen, GR .
APPLIED AND ENVIRONMENTAL MICROBIOLOGY, 1997, 63 (08) :3211-3217
[5]   Microscopic observations of bacterial sorption in soil cores [J].
Fisk A.C. ;
Murphy S.L. ;
Tate III R.L. .
Biology and Fertility of Soils, 1999, 28 (2) :111-116
[6]  
FOSTER RC, 1986, ANNU REV PHYTOPATHOL, V24, P211
[7]   Geostatistical analysis of the distribution of NH4+ and NO2--oxidizing bacteria and serotypes at the millimeter scale along a soil transect [J].
Grundmann, GL ;
Debouzie, D .
FEMS MICROBIOLOGY ECOLOGY, 2000, 34 (01) :57-62
[8]  
HASSE P, 1995, J VEG SCI, V6, P575
[9]  
Ihaka R., 1996, J COMPUTATIONAL GRAP, V5, P299, DOI [DOI 10.1080/10618600.1996.10474713, 10.1080/10618600.1996.10474713, 10.2307/1390807]
[10]  
Isaaks EH., 1989, Applied Geostatistics