Relationship between sediment organic matter, bacteria composition, and the ecosystem metabolism of alpine streams

Détails

ID Serval
serval:BIB_22093D9F64D2
Type
Article: article d'un périodique ou d'un magazine.
Collection
Publications
Titre
Relationship between sediment organic matter, bacteria composition, and the ecosystem metabolism of alpine streams
Périodique
Limnology and Oceanography
Auteur(s)
Brendan Logue J., Robinson C.T., Meier C., Van Der Meer J.R.
ISSN
0024-3590
Statut éditorial
Publié
Date de publication
2004
Peer-reviewed
Oui
Volume
49
Numéro
6
Pages
2001-2010
Langue
anglais
Notes
http://www.jstor.org/stable/3597506
Résumé
We tested whether sediment bacteria abundance (49,6-diamidino-2-phenylindole-stained cell counts) were related to sediment organic content (ash-free dry mass [AFDM]) in 11 nonforested streams of three different Alpine catchments during summer 2003. We used terminal restriction fragment-length polymorphism (T-RLFP, a molecular genetic technique) to test for seasonal and spatial differences in bacterial composition in these same streams. We then related the above parameters, in conjunction with periphyton biomass and hyporheic respiration, to whole stream estimates of gross primary production (GPP) and ecosystem respiration (ER) in a glacial and nonglacial stream, representing environmental extremes, in one of the catchments. The percentage of organic matter of sediments was 4-14% (0.01-0.04 g AFDM ml sediment21), and counts of bacteria cells per millimeter of sediment averaged 2 3 106-4 3 106. Bacteria counts correlated with sediment AFDM only for streams in the catchment with highest sediment AFDM levels. Bacteria composition (based on the presence and absence of terminal restriction fragments from T-RFLP analysis) changed seasonally in the different streams and differed between glacial- and groundwater-fed streams. In the one catchment, hyporheic respiration averaged 0.0004 and 0.0003 g O2 h21 kg sediment21 and was positively correlated with AFDM (r2 5 0.23). Ecosystem metabolism displayed a strong seasonality,with GPP averaging 4.5 and 8.4 and ER averaging 5.4 and 9.9 g O2 m22 d21 for the two sites, respectively, thus indicating a predominance of heterotrophy (P :R , 1) in these high-elevation, open-canopied systems. Bacteria play a strong role in the trophic dynamics of alpine streams.
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Création de la notice
21/01/2008 14:36
Dernière modification de la notice
20/08/2019 13:58
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