Community Structure of Denitrifiers, Bacteria , and Archaea along Redox Gradients in Pacific Northwest Marine Sediments by Terminal Restriction Fragment Length Polymorphism Analysis of Amplified Nitrite Reductase ( nirS ) and 16S rRNA Genes
Open Access
- 1 April 2001
- journal article
- research article
- Published by American Society for Microbiology in Applied and Environmental Microbiology
- Vol. 67 (4) , 1893-1901
- https://doi.org/10.1128/aem.67.4.1893-1901.2001
Abstract
Steep vertical gradients of oxidants (O2 and NO3−) in Puget Sound and Washington continental margin sediments indicate that aerobic respiration and denitrification occur within the top few millimeters to centimeters. To systematically explore the underlying communities of denitrifiers,Bacteria, and Archaea along redox gradients at distant geographic locations, nitrite reductase (nirS) genes and bacterial and archaeal 16S rRNA genes (rDNAs) were PCR amplified and analyzed by terminal restriction fragment length polymorphism (T-RFLP) analysis. The suitablility of T-RFLP analysis for investigating communities of nirS-containing denitrifiers was established by the correspondence of dominant terminal restriction fragments (T-RFs) of nirS to computer-simulated T-RFs ofnirS clones. These clones belonged to clusters II, III, and IV from the same cores and were analyzed in a previous study (G. Braker, J. Zhou, L. Wu, A. H. Devol, and J. M. Tiedje, Appl. Environ. Microbiol. 66:2096–2104, 2000). T-RFLP analysis ofnirS and bacterial rDNA revealed a high level of functional and phylogenetic diversity, whereas the level of diversity ofArchaea was lower. A comparison of T-RFLPs based on the presence or absence of T-RFs and correspondence analysis based on the frequencies and heights of T-RFs allowed us to group sediment samples according to the sampling location and thus clearly distinguish Puget Sound and the Washington margin populations. However, changes in community structure within sediment core sections during the transition from aerobic to anaerobic conditions were minor. Thus, within the top layers of marine sediments, redox gradients seem to result from the differential metabolic activities of populations of similar communities, probably through mixing by marine invertebrates rather than from the development of distinct communities.Keywords
This publication has 46 references indexed in Scilit:
- Effect of soil aggregate size on methanogenesis and archaeal community structure in anoxic rice field soilFEMS Microbiology Ecology, 2000
- Sedimentary organic matter preservation; a test for selective degradation under oxic conditionsAmerican Journal of Science, 1999
- Diversity of deep-sea hydrothermal vent Archaea from Loihi Seamount, HawaiiDeep Sea Research Part II: Topical Studies in Oceanography, 1998
- Denitrification in marine sediments: A model studyGlobal Biogeochemical Cycles, 1996
- Is the ocean losing nitrate?Nature, 1995
- OrdinationPublished by Cambridge University Press (CUP) ,1995
- High abundance of Archaea in Antarctic marine picoplanktonNature, 1994
- Benthic fluxes and nitrogen cycling in sediments of the continental margin of the eastern North PacificJournal of Marine Research, 1993
- Importance of continental margins in the marine biogeochemical cycling of carbon and nitrogenNature, 1991
- PHYLOGENIES FROM MOLECULAR SEQUENCES: INFERENCE AND RELIABILITYAnnual Review of Genetics, 1988