Distribution of culturable microorganisms in Fennoscandian Shield groundwater

被引:55
作者
Haveman, SA [1 ]
Pedersen, K [1 ]
机构
[1] Univ Gothenburg, Dept Cell & Mol Biol, SE-40530 Gothenburg, Sweden
关键词
acetogenesis; groundwater; iron reduction; methanogenesis; principal component; subsurface; sulfate reduction;
D O I
10.1111/j.1574-6941.2002.tb00914.x
中图分类号
Q93 [微生物学];
学科分类号
071005 ; 100705 ;
摘要
Microbial populations in 16 groundwater samples from six Fennoscandian Shield sites in Finland and Sweden were investigated. The average total cell number was 3.7 X 10(5) cells ml(-1), and there was no change in the mean of the total cell numbers to a depth of 1390 m. Culture media were designed based on the chemical composition of each groundwater sample and used successfully to culture anaerobic microorganisms from all samples between 65 and 1350 m depth. Between 0.0084 and 14.8% of total cells were cultured from groundwater samples. Sulfate-reducing bacteria, iron-reducing bacteria and heterotrophic acetogenic bacteria were cultured from groundwater sampled at 65-686 m depth in geographically distant sites. Different microbial populations were cultured from deeper, older and more saline groundwater from 863 to 1350 in depth. Principal component analysis of groundwater chemistry data showed that sulfate- and iron-reducing bacteria were not detected in the most saline groundwater. Iron-reducing bacteria and acetogens were cultured from deep groundwater that contained 0.35-3.5 mM sulfate, while methanogens and acetogens were cultured from deep sulfate-depleted groundwater. In one borehole from which autotrophic methanogens were cultured. dissolved inorganic carbon was enriched in C-13 compared to other Fennoscandian Shield groundwater samples, suggesting that autotrophs were active. It can be concluded that a diverse microbial community is present from the surface to over 1300 m depth in the Fennoscandian Shield. (C) 2002 Federation of European Microbiological Societies. Published by Elsevier Science B.V. All rights reserved.
引用
收藏
页码:129 / 137
页数:9
相关论文
共 31 条
[1]  
Bachofen R, 1998, MICROBIOL RES, V153, P1, DOI 10.1016/S0944-5013(98)80016-5
[2]   Desulfovibrio profundus sp nov, a novel barophilic sulfate-reducing bacterium from deep sediment layers in the Japan Sea [J].
Bale, SJ ;
Goodman, K ;
Rochelle, PA ;
Marchesi, JR ;
Fry, JC ;
Weightman, AJ ;
Parkes, RJ .
INTERNATIONAL JOURNAL OF SYSTEMATIC BACTERIOLOGY, 1997, 47 (02) :515-521
[3]   A NEW GEOCHEMICAL CLASSIFICATION OF SEDIMENTARY ENVIRONMENTS [J].
BERNER, RA .
JOURNAL OF SEDIMENTARY PETROLOGY, 1981, 51 (02) :359-365
[4]   Evaluation of the effect of microbial subsurface ecosystems on spent nuclear fuel repositories [J].
Brown, DA ;
Sherriff, BL .
ENVIRONMENTAL TECHNOLOGY, 1999, 20 (05) :469-477
[5]   CHARACTERIZATION OF ATTACHED BACTERIAL-POPULATIONS IN DEEP GRANITIC GROUNDWATER FROM THE STRIPA RESEARCH MINE BY 16S RIBOSOMAL-RNA GENE SEQUENCING AND SCANNING ELECTRON-MICROSCOPY [J].
EKENDAHL, S ;
ARLINGER, J ;
STAHL, F ;
PEDERSEN, K .
MICROBIOLOGY-UK, 1994, 140 :1575-1583
[6]   CARBON TRANSFORMATIONS BY ATTACHED BACTERIAL-POPULATIONS IN GRANITIC GROUNDWATER FROM DEEP CRYSTALLINE BED-ROCK OF THE STRIPA RESEARCH MINE [J].
EKENDAHL, S ;
PEDERSEN, K .
MICROBIOLOGY-UK, 1994, 140 :1565-1573
[7]   Alteration of oceanic volcanic glass: Textural evidence of microbial activity [J].
Fisk, MR ;
Giovannoni, SJ ;
Thorseth, IH .
SCIENCE, 1998, 281 (5379) :978-980
[8]   AN OUTLINE OF THE PRECAMBRIAN EVOLUTION OF THE BALTIC SHIELD [J].
GAAL, G ;
GORBATSCHEV, R .
PRECAMBRIAN RESEARCH, 1987, 35 :15-52
[9]   THE DEEP, HOT BIOSPHERE [J].
GOLD, T .
PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA, 1992, 89 (13) :6045-6049
[10]   REDOX POTENTIALS AND REDOX REACTIONS IN DEEP GROUNDWATER SYSTEMS [J].
GRENTHE, I ;
STUMM, W ;
LAAKSUHARJU, M ;
NILSSON, AC ;
WIKBERG, P .
CHEMICAL GEOLOGY, 1992, 98 (1-2) :131-150