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
G. Braker et al., 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, APPL ENVIR, 67(4), 2001, pp. 1893-1901
Steep vertical gradients of oxidants (O-2 and NO3-) in Puget Sound and Wash
ington continental margin sediments indicate that aerobic respiration and d
enitrification occur within the top few millimeters to centimeters. To syst
ematically explore the underlying communities of denitrifiers, Bacteria, an
d Archaea along redox gradients at distant geographic locations, nitrite re
ductase (nirS) genes and bacterial and archaeal 16S rRNA genes (rDNAs) were
PCR amplified and analyzed by terminal restriction fragment length polymor
phism (T-RFLP) analysis, The suitablility of T-RFLP analysis for investigat
ing communities of nirS-containing denitrifiers was established by the corr
espondence of dominant terminal restriction fragments (T-RFs) of nirS to co
mputer-simulated T-RFs of nirS 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, Micr
obiol, 66:2096-2104, 2000), T-RFLP analysis of nirS and bacterial rDNA reve
aled a high level of functional and phylogenetic diversity, whereas the lev
el of diversity of Archaea was lower, A comparison of T-RFLPs based on the
presence or absence of T-RFs and correspondence analysis based on the frequ
encies and heights of T-RFs allowed us to group sediment samples according
to the sampling location and thus clearly distinguish Puget Sound and the W
ashington margin populations. However, changes in community structure withi
n sediment core sections during the transition from aerobic to anaerobic co
nditions were minor, Thus, within the top layers of marine sediments, redox
gradients seem to result from the differential metabolic activities of pop
ulations of similar communities, probably through mixing by marine inverteb
rates rather than from the development of distinct communities.