Microbial diversity and activity along the forefields of two receding glaciers

被引:142
作者
Sigler, WV [1 ]
Zeyer, J [1 ]
机构
[1] Swiss Fed Inst Technol, ETH, Inst Terr Ecol, CH-8952 Schlieren, Switzerland
关键词
D O I
10.1007/s00248-001-0045-5
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
Forefields of two receding glaciers were sampled along either a 150 or 200 m long transect at identical spatial intervals for assessment of soil microbial activity and community diversity trends. The forefields belonged to the Dammaglacier (forefield area is 157 ha, 2000 m above sea level) and Rotfirnglacier (100 ha, 2200 m) and at the time of sampling were receding at an estimated rate of 8 and 10 m yr(-1) over the past 5 years, respectively. Direct counting of bacteria (DAPI staining), assessment of dehydrogenase activity (DH), and fluorescein diacetate hydrolysis activity (FDA) were performed to estimate bacteria number and soil microbial activity. Along the Dammaglacier forefield (from youngest to oldest soil), bacteria number (8.21 x 10(7) to 1.49 x 10(9) cells g(-1) soil), DH activity (0 to 61 mug TTC reduced g(-1) soil h(-1)), and FDA activity (0 to 100 mug fluorescein produced g(-1) soil h(-1)) increased, suggesting the development of microbial populations increasing in number and activity. The Rotfirn forefield exhibited similar trends per gram of soil in bacteria number (1.13 x 10(8) to 5.93 x 10(9) cells), DH activity (0 to 36 mug TTC reduced), and FDA activity (2 to 70 mug fluorescein produced), but with more variability among samples than the Damma forefield samples. Molecular assessment of bacterial diversity included denaturing gradient gel electrophoresis (DGGE) and ribosomal intergenic spacer analysis (RISA) of soil DNA. DGGE and RISA revealed that the composition and succession of bacterial populations were different in both forefields. Comparison of Shannon diversity index values indicated that all populations sampled from the Damma forefield were significantly different (p < 0.05). Conversely, similar populations existed in the Rotfirn forefield succession. Overall, the results indicate that diverse bacterial assemblages increasing in number and activity characterize these glacier forefield soils with both forefield successions exhibiting differing modes of bacterial community establishment.
引用
收藏
页码:397 / 407
页数:11
相关论文
共 50 条
[1]  
ALEF K, 1994, SOIL SCI SOC AM BOOK, V5, P228
[2]   COMPARISON OF PHENOTYPICAL AND MOLECULAR METHODS FOR THE IDENTIFICATION OF BACTERIAL STRAINS ISOLATED FROM A DEEP SUBSURFACE ENVIRONMENT [J].
BOIVINJAHNS, V ;
BIANCHI, A ;
RUIMY, R ;
GARCIN, J ;
DAUMAS, S ;
CHRISTEN, R .
APPLIED AND ENVIRONMENTAL MICROBIOLOGY, 1995, 61 (09) :3400-3406
[3]   Molecular microbial diversity in soils from eastern Amazonia: Evidence for unusual microorganisms and microbial population shifts associated with deforestation [J].
Borneman, J ;
Triplett, EW .
APPLIED AND ENVIRONMENTAL MICROBIOLOGY, 1997, 63 (07) :2647-2653
[4]  
Brooks PD, 1996, BIOGEOCHEMISTRY, V32, P93, DOI 10.1007/BF00000354
[5]   A strategy for optimizing quality and quantity of DNA extracted from soil [J].
Bürgmann, H ;
Pesaro, M ;
Widmer, F ;
Zeyer, J .
JOURNAL OF MICROBIOLOGICAL METHODS, 2001, 45 (01) :7-20
[6]   ANTARCTIC SOIL ALGAL CRUSTS - SCANNING ELECTRON AND OPTICAL MICROSCOPE STUDY [J].
CAMERON, RE ;
DEVANEY, JR .
TRANSACTIONS OF THE AMERICAN MICROSCOPICAL SOCIETY, 1970, 89 (02) :264-&
[7]   Effects of resource-island soils, competition, and inoculation with Azospirillum on survival and growth of Pachycereus pringlei, the giant cactus of the Sonoran Desert [J].
Carrillo-Garcia, A ;
Bashan, Y ;
Rivera, ED ;
Bethlenfalvay, FJ .
RESTORATION ECOLOGY, 2000, 8 (01) :65-73
[8]   Identification of and spatio-temporal differences between microbial assemblages from two neighboring sulfurous lakes:: Comparison by microscopy and denaturing gradient gel electrophoresis [J].
Casamayor, EO ;
Schäfer, H ;
Bañeras, L ;
Pedrós-Alió, C ;
Muyzer, G .
APPLIED AND ENVIRONMENTAL MICROBIOLOGY, 2000, 66 (02) :499-508
[9]   MECHANISMS OF PRIMARY SUCCESSION FOLLOWING DEGLACIATION AT GLACIER BAY, ALASKA [J].
CHAPIN, FS ;
WALKER, LR ;
FASTIE, CL ;
SHARMAN, LC .
ECOLOGICAL MONOGRAPHS, 1994, 64 (02) :149-175
[10]  
Dancer SJ, 1997, J APPL MICROBIOL, V82, P597, DOI 10.1111/j.1365-2672.1997.tb02868.x