Literature DB >> 11953808

Microbial diversity and activity along the forefields of two receding glaciers.

W V Sigler1, J Zeyer.   

Abstract

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 mg TTC reduced g(-1) soil h(-1)), and FDA activity (0 to 100 mg 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 mg TTC reduced), and FDA activity (2 to 70 mg 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.

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Year:  2002        PMID: 11953808     DOI: 10.1007/s00248-001-0045-5

Source DB:  PubMed          Journal:  Microb Ecol        ISSN: 0095-3628            Impact factor:   4.552


  35 in total

1.  Bacterial, archaeal and fungal succession in the forefield of a receding glacier.

Authors:  Anita Zumsteg; Jörg Luster; Hans Göransson; Rienk H Smittenberg; Ivano Brunner; Stefano M Bernasconi; Josef Zeyer; Beat Frey
Journal:  Microb Ecol       Date:  2011-12-13       Impact factor: 4.552

2.  Pattern of elemental release during the granite dissolution can be changed by aerobic heterotrophic bacterial strains isolated from Damma Glacier (central Alps) deglaciated granite sand.

Authors:  Aleš Lapanje; Celine Wimmersberger; Gerhard Furrer; Ivano Brunner; Beat Frey
Journal:  Microb Ecol       Date:  2011-11-22       Impact factor: 4.552

3.  Weathering-associated bacteria from the Damma glacier forefield: physiological capabilities and impact on granite dissolution.

Authors:  Beat Frey; Stefan R Rieder; Ivano Brunner; Michael Plötze; Stefan Koetzsch; Ales Lapanje; Helmut Brandl; Gerhard Furrer
Journal:  Appl Environ Microbiol       Date:  2010-06-04       Impact factor: 4.792

4.  Abundances and potential activities of nitrogen cycling microbial communities along a chronosequence of a glacier forefield.

Authors:  Robert Brankatschk; Stefanie Töwe; Kristina Kleineidam; Michael Schloter; Josef Zeyer
Journal:  ISME J       Date:  2010-12-02       Impact factor: 10.302

5.  Distribution of high bacterial taxa across the chronosequence of two alpine glacier forelands.

Authors:  Laurent Philippot; Dagmar Tscherko; David Bru; Ellen Kandeler
Journal:  Microb Ecol       Date:  2010-10-09       Impact factor: 4.552

6.  Colony-forming analysis of bacterial community succession in deglaciated soils indicates pioneer stress-tolerant opportunists.

Authors:  W V Sigler; J Zeyer
Journal:  Microb Ecol       Date:  2004-08-24       Impact factor: 4.552

7.  Microbial community succession in an unvegetated, recently deglaciated soil.

Authors:  Diana R Nemergut; Suzanne P Anderson; Cory C Cleveland; Andrew P Martin; Amy E Miller; Anton Seimon; Steven K Schmidt
Journal:  Microb Ecol       Date:  2006-12-22       Impact factor: 4.552

8.  Abundance of narG, nirS, nirK, and nosZ genes of denitrifying bacteria during primary successions of a glacier foreland.

Authors:  Ellen Kandeler; Kathrin Deiglmayr; Dagmar Tscherko; David Bru; Laurent Philippot
Journal:  Appl Environ Microbiol       Date:  2006-09       Impact factor: 4.792

9.  Bacterial diversity associated with Blood Falls, a subglacial outflow from the Taylor Glacier, Antarctica.

Authors:  Jill A Mikucki; John C Priscu
Journal:  Appl Environ Microbiol       Date:  2007-04-27       Impact factor: 4.792

10.  Bacterial succession in a glacier foreland of the High Arctic.

Authors:  Ursel M E Schütte; Zaid Abdo; Stephen J Bent; Christopher J Williams; G Maria Schneider; Bjørn Solheim; Larry J Forney
Journal:  ISME J       Date:  2009-07-09       Impact factor: 10.302

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