Affiliation:
1. University of Maryland Center for Environmental Science, Horn Point Laboratory, Cambridge, Maryland
Abstract
ABSTRACT
Anoxia occurs in bottom waters of stratified estuaries when respiratory consumption of oxygen, primarily by bacteria, outpaces atmospheric and photosynthetic reoxygenation. Once water becomes anoxic, bacterioplankton must change their metabolism to some form of anaerobic respiration. Analysis of redox chemistry in water samples spanning the oxycline of Chesapeake Bay during the summer of 2004 suggested that there was a succession of respiratory metabolism following the loss of oxygen. Bacterial community doubling time, calculated from bacterial abundance (direct counts) and production (anaerobic leucine incorporation), ranged from 0.36 to 0.75 day and was always much shorter than estimates of the time that the bottom water was anoxic (18 to 44 days), indicating that there was adequate time for bacterial community composition to shift in response to changing redox conditions. However, community composition (as determined by PCR-denaturing gradient gel electrophoresis analysis of 16S rRNA genes) in anoxic waters was very similar to that in surface waters in June when nitrate respiration was apparent in the water column and only partially shifted away from the composition of the surface community after nitrate was depleted. Anoxic water communities did not change dramatically until August, when sulfate respiration appeared to dominate. Surface water populations that remained dominant in anoxic waters were
Synechococcus
sp.,
Gammaproteobacteria
in the SAR86 clade, and
Alphaproteobacteria
relatives of
Pelagibacter ubique
, including a putative estuarine-specific
Pelagibacter
cluster. Populations that developed in anoxic water were most similar (<92% similarity) to uncultivated
Firmicutes
, uncultivated
Bacteroidetes, Gammaproteobacteria
in the genus
Thioalcalovibrio
, and the uncultivated SAR406 cluster. These results indicate that typical estuarine bacterioplankton switch to anaerobic metabolism under anoxic conditions but are ultimately replaced by different organisms under sulfidic conditions.
Publisher
American Society for Microbiology
Subject
Ecology,Applied Microbiology and Biotechnology,Food Science,Biotechnology
Reference64 articles.
1. Barbosa, A. B., H. M. Galvao, P. A. Mendes, X. A. Alvarez-Salgado, F. G. Figueiras, and I. Joint. 2001. Short-term variability of heterotrophic bacterioplankton during upwelling off the NW Iberian margin. Prog. Oceanogr.51:339-359.
2. The Leucine Incorporation Method Estimates Bacterial Growth Equally Well in Both Oxic and Anoxic Lake Waters
3. Boicourt, W. C. 1992. Influences of circulation processes on dissolved oxygen in the Chesapeake Bay, p. 7-59. In D. E. Smith, M. Leffler, and G. Mackiernan (ed.), Oxygen dynamics in the Chesapeake Bay. Maryland Sea Grant, College Park.
4. Borsuk, M. E., C. A. Stow, R. A. Luettich, H. W. Paerl, and J. L. Pinckney. 2001. Modelling oxygen dynamics in an intermittently stratified estuary: estimation of process rates using field data. Estuar. Coast. Shelf Sci.52:33-49.
5. Bosshard, P. P., R. Stettler, and R. Bachofen. 2000. Seasonal and spatial community dynamics in the meromictic Lake Cadagno. Arch. Microbiol.174:168-174.
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