Seasonal shifts in bacterioplankton community composition in Toolik Lake, a tundra lake on the North Slope of Alaska, were related to shifts in the source (terrestrial versus phytoplankton) and lability of dissolved organic matter (DOM). A shift in community composition, measured by denaturing gradient gel electrophoresis (DGGE) of 16S rRNA genes, occurred at 4°C in near-surface waters beneath seasonal ice and snow cover in spring. This shift was associated with an annual peak in bacterial productivity ([ 14 C]leucine incorporation) driven by the large influx of labile terrestrial DOM associated with snow meltwater. A second shift occurred after the flux of terrestrial DOM had ended in early summer as ice left the lake and as the phytoplankton community developed. Bacterioplankton communities were composed of persistent populations present throughout the year and transient populations that appeared and disappeared. Most of the transient populations could be divided into those that were advected into the lake with terrestrial DOM in spring and those that grew up from low concentrations during the development of the phytoplankton community in early summer. Sequencing of DNA in DGGE bands demonstrated that most bands represented single ribotypes and that matching bands from different samples represented identical ribotypes. Bacteria were identified as members of globally distributed freshwater phylogenetic clusters within the ␣-and ␤-Proteobacteria, the Cytophaga-Flavobacteria-Bacteroides group, and the Actinobacteria.

Sulfate reduction, mediated by sulfate-reducing bacteria (SRB), is the dominant remineralization pathway in sediments of New England salt marshes. High sulfate reduction rates are associated with the rhizosphere of Spartina alterniflora when plants elongate aboveground. The growth process concurrently produces significant amounts of new rhizome material belowground and the plants leak dissolved organic compounds. This study investigated the diversity of SRB in a salt marsh over an annual growth cycle of S. alterniflora by exploring the diversity of a functional gene, dissimilatory sulfite reductase (dsrAB). Because the dsrAB gene is a key gene in the anaerobic sulfate-respiration pathway, it allows the identification of microorganisms responsible for sulfate reduction. Conserved dsrAB primers in polymerase chain reaction (PCR) generated full-length dsrAB amplicons for cloning and DNA sequence analysis. Nearly 80% of 380 clone sequences were similar to genes from Desulfosarcina and Desulfobacterium species within Desulfobacteraceae. This reinforces the hypothesis that complete oxidizers with high substrate versatility dominate the marsh. However, the phylotypes formed several clades that were distinct from cultured representatives, indicating a greater diversity of SRB than previously appreciated. Several dsrAB sequences were related to homologues from gram-positive, thermophilic and non-thermophilic Desulfotomaculum species. One dsrAB lineage formed a sister group to cultured members of the delta-proteobacterial group Syntrophobacteraceae. A deeply branching dsrAB lineage was not affiliated with genes from any cultured SRB. The sequence data from this study will allow for the design of probes or primers that can quantitatively assess the diverse range of sulfate reducers present in the environment.

We used molecular techniques to assess the phylogenetlc afflnlty of cultured and uncultured m~croorganis~ns from Toolik Lake, an ol~gotrophic lake In a r c t~c Alaska USA The phylogenetlc positions of cloned cultures of bacteria were determined by sequence analysls of PCR ampl~fled ribosomal RNA genes The Toollk Lake bacterial isolates showed a high degree of slmllarlty, 0 94 to 0 99, to a wlde variety of phyla that are well represented in the ribosomal RNA database The occurrence of species normally associated with a terrestrial habltat (Arthrobacter globiforn~is and B~~r k h o l d e n a solanacearum) or a more nutrient-rich environment (Cytophaga aquatills and Zoogloea r a m~y e r a ) suggests a particle-associated origln for these cell types consistent with the fact that w e used an unflltered sample In contrast, the analysls of rRNA genes cloned from a complex natural DNA community indlcated the predominance of beta-proteobacteria closely related to the rRNA hamology group I1 pseudomonads Alcalrgenes eutrophus and Pseudomonaspickett~l However, 2 of therRNA g e n e clones are deeply branching relatives (s~rnllarity = 0 88) of the alpha-proteobacteria SARI 1 cluster, previously detected only In marine environments Thls finding lndlcates a widespread aquatic dlstnbutlon for thls recently descnbed group KEY WORDS: Bactel-]a 1 6 s rRNA. Arctic. SARll

The biogeochemistry of North Atlantic salt marshes is characterized by the interplay between the marsh grass Spartina and sulphate-reducing bacteria (SRB), which mineralize the diverse carbon substrates provided by the plants. It was hypothesized that SRB populations display high diversity within the sediment as a result of the rich spatial and chemical structuring provided by Spartina roots. A 2000-member 16S rRNA gene library, prepared with delta-proteobacterial SRB-selective primers, was analysed for diversity patterns and phylogenetic relationships. Sequence clustering detected 348 16S rRNA sequence types (ribotypes) related to delta-proteobacterial SRB, and it was estimated that a total of 623 ribotypes were present in the library. Similarity clustering showed that approximately 46% of these sequences fell into groups with < 1% divergence; thus, microheterogeneity accounts for a large portion of the observable genetic diversity. Phylogenetic comparison revealed that sequences most frequently recovered were associated with the Desulfobacteriaceae and Desulfobulbaceae families. Sequences from the Desulfovibrionaceae family were also observed, but were infrequent. Over 80% of the delta-proteobacterial ribotypes clustered with cultured representatives of Desulfosarcina, Desulfococcus and Desulfobacterium genera, suggesting that complete oxidizers with high substrate versatility dominate. The large-scale approach demonstrates the co-existence of numerous SRB-like sequences and reveals an unexpected amount of microdiversity.

–  Movement and habitat use by bull trout (Salvelinus confluentus) was examined using radio telemetry in the Morice River watershed, north‐western British Columbia, between April 2000 and November 2001. Bull trout principally utilised mainstem habitat. Throughout the watershed, little movement was observed during the winter months. From June to September, movement increased and was correlated with migration into tributaries. We directly observed spawning bull trout only in tributaries of the Morice River and never in the mainstem. Many of the fish (N = 48) migrated to the nearest potential spawning sites, but a few fish (N = 7) made extensive migrations to other regions of the watershed to spawn. Fish that spawned in both years of the study returned to the same spawning location. Variation in spatial and movement data, therefore, appears to be linked to availability of suitable habitat and not differences in life history that have been observed in large bull trout.