The DOI matches its Crossref record; 1 of the 1 references it cites were found in a registry or an index.
THE FUNCTIONAL SIGNIFICANCE OF THE HYPORHEIC ZONE IN STREAMS AND RIVERS
Abstract
▪ Abstract The hyporheic zone is an active ecotone between the surface stream and groundwater. Exchanges of water, nutrients, and organic matter occur in response to variations in discharge and bed topography and porosity. Upwelling subsurface water supplies stream organisms with nutrients while downwelling stream water provides dissolved oxygen and organic matter to microbes and invertebrates in the hyporheic zone. Dynamic gradients exist at all scales and vary temporally. At the microscale, gradients in redox potential control chemical and microbially mediated nutrient transformations occurring on particle surfaces. At the stream-reach scale, hydrological exchange and water residence time are reflected in gradients in hyporheic faunal composition, uptake of dissolved organic carbon, and nitrification. The hyporheic corridor concept describes gradients at the catchment scale, extending to alluvial aquifers kilometers from the main channel. Across all scales, the functional significance of the hyporheic zone relates to its activity and connection with the surface stream.
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Cites
Poff, N. L. (1997) · Journal of the North American Benthological Society · doi:10.2307/1468026 · Cited by 1,833
Cited by
Groffman, P. M., Butterbach-Bahl, K., Fulweiler, R. W., Gold, A. J., Morse, J. L., Stander, E. K., Tague, C., Tonitto, C., & Vidon, P. (2009) · Biogeochemistry · doi:10.1007/s10533-008-9277-5 · Cited by 677
Stegen, J. C., Fredrickson, J. K., Wilkins, M. J., Konopka, A. E., Nelson, W. C., Arntzen, E. V., Chrisler, W. B., Chu, R. K., Danczak, R. E., Fansler, S. J., et al. (2016) · Nature Communications · doi:10.1038/ncomms11237 · Cited by 409
Hydrological connectivity for riverine fish: measurement challenges and research opportunities
FULLERTON, A. H., BURNETT, K. M., STEEL, E. A., FLITCROFT, R. L., PESS, G. R., FEIST, B. E., TORGERSEN, C. E., MILLER, D. J., & SANDERSON, B. L. (2010) · Freshwater Biology · doi:10.1111/j.1365-2427.2010.02448.x · Cited by 379
Phosphorus Retention in Riparian Buffers: Review of Their Efficiency
Hoffmann, C. C., Kjaergaard, C., Uusi‐Kämppä, J., Hansen, H. C. B., & Kronvang, B. (2009) · Journal of Environmental Quality · doi:10.2134/jeq2008.0087 · Cited by 379
Covino, T. (2017) · Geomorphology · doi:10.1016/j.geomorph.2016.09.030 · Cited by 328
Metadata
- Authors
- Boulton, A. J., Findlay, S., Marmonier, P., Stanley, E. H., & Valett, H. M.
- Venue
- Annual Review of Ecology and Systematics
- Publisher
- Annual Reviews
- Published
- 1998-11
- Volume
- 29
- Issue
- 1
- Pages
- 59-81
- ISSN
- 0066-4162 (ISSN-L)
- OpenAlex
- W1974322213
- Cited by
- 1,191
- References
- 1
- FWCI
- 16.86
- Type
- journal article
- Language
- en
- Open access
- closed
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- CoChat. (2026). Citation check: THE FUNCTIONAL SIGNIFICANCE OF THE HYPORHEIC ZONE IN STREAMS AND RIVERS. https://app.cochat.ai/papers/10.1146/annurev.ecolsys.29.1.59
- The paper
- Boulton, A. J., Findlay, S., Marmonier, P., Stanley, E. H., & Valett, H. M. (1998). THE FUNCTIONAL SIGNIFICANCE OF THE HYPORHEIC ZONE IN STREAMS AND RIVERS. Annual Review of Ecology and Systematics. https://doi.org/10.1146/annurev.ecolsys.29.1.59
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Bibliographic data: Semantic Scholar, OpenAlex, Crossref.
Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).
Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.
