ArticleMicrobial ecology2009
Habitat heterogeneity and associated microbial community structure in a small-scale floodplain hyporheic flow path.
Article in Microbial ecology, 2009. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 9 papers.
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Who cites it
9 citing papers in PubMed, 46 citations in OpenAlex.
- Temporal Variation in Bacterial Community Characteristics Shaped by Habitat in a Reservoir Buffer Strip in China.Ecology and evolution · 2025Article
- Convergence in floodplain pond communities indicates different pathways to community assembly.Aquatic sciences · 2023Article
- Geochemical and Microbial Community Attributes in Relation to Hyporheic Zone Geological Facies.Scientific reports · 2017Article
- Groundwater-surface water mixing shifts ecological assembly processes and stimulates organic carbon turnover.Nature communications · 2016Article
- Impact of a wastewater treatment plant on microbial community composition and function in a hyporheic zone of a eutrophic river.Scientific reports · 2015Article
- Spatial and temporal dynamics of the microbial community in the Hanford unconfined aquifer.The ISME journal · 2012Article
- Bacterial community dynamics in the hyporheic zone of an intermittent stream.The ISME journal · 2012Article
- Application of meta-transcriptomics and -proteomics to analysis of in situ physiological state.Frontiers in microbiology · 2012Article
- Water-sediment exchanges control microbial processes associated with leaf litter degradation in the hyporheic zone: a microcosm study.Microbial ecology · 2011Article
Corrections and comments
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Authors and funding
6 authors at 1 institution in 1 country.
Funding
No grant is acknowledged in the PubMed record.
Abstract
The Nyack floodplain is located on the Middle Fork of the Flathead River, an unregulated, pristine, fifth-order stream in Montana, USA, bordering Glacier National Park. The hyporheic zone is a nutritionally heterogeneous floodplain component harboring a diverse array of microbial assemblages essential in fluvial biogeochemical cycling, riverine ecosystem productivity, and trophic interactions. Despite these functions, microbial community structure in pristine hyporheic systems is not well characterized. The current study was designed to assess whether physical habitat heterogeneity within the hyporheic zone of the Nyack floodplain was sufficient to drive bacterial beta diversity between three different hyporheic flow path locations. Habitat heterogeneity was assessed by measuring soluble reactive phosphorous, nitrate, dissolved organic carbon, dissolved oxygen, and soluble total nitrogen levels seasonally at surface water infiltration, advection, and exfiltration zones. Significant spatial differences were detected in dissolved oxygen and nitrate levels, and seasonal differences were detected in dissolved oxygen, nitrate, and dissolved organic carbon levels. Denaturing gradient gel electrophoresis (DGGE) and cell counts indicated that bacterial diversity increased with abundance, and DGGE fingerprints covaried with nitrate levels where water infiltrated the hyporheic zone. The ribosomal gene phylogeny revealed that hyporheic habitat heterogeneity was sufficient to drive beta diversity between bacterial assemblages. Phylogenetic (P) tests detected sequence disparity between the flow path locations. Small distinct lineages of Firmicutes, Actinomycetes, Planctomycetes, and Acidobacteria defined the infiltration zone and alpha- and beta-proteobacterial lineages delineated the exfiltration and advection zone communities. These data suggest that spatial habitat heterogeneity drives hyporheic microbial community development and that attempts to understand functional differences between bacteria inhabiting nutritionally heterogeneous hyporheic environments might begin by focusing on the biology of these taxa.
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