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Cited by 154Soil and Water Nutrient DynamicsIsotope Analysis in EcologyFreshwater macroinvertebrate diversity and ecology

The DOI matches its Crossref record; 46 of the 46 references it cites were found in a registry or an index.

Quantification of the nitrogen cycle in a prairie stream.

Dodds, Walter K., Evans-White, Michelle A., Gerlanc, Nicole M., Gray, Lawrence, Gudder, Dolly A., Kemp, Melody J., López, Amanda L., Stagliano, David, Strauss, Eric A., Tank, Jennifer L., Whiles, Matt R., Wollheim, Wilfred M.·2000·Ecosystems
DOI 10.1007/s100210000050
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Abstract

Nitrogen (N) was added for 35 days in the form of ¹⁵NH₄Cl to Kings Creek on Konza Prairie, Kansas. Standing stocks of N in key compartments (that is, nutrients, detritus, organisms) were quantified, and the amount of labeled N entering the compartments was analyzed. These data were used to calculate turnover and flux rates of N cycling through the food web, as well as nutrient transformation rates. Inorganic N pools turned over much more rapidly in the water column of this stream than in pelagic systems where comparable measurements have been made. As with other systems, the mass of ammonium was low but it was the key compartment mediating nutrient flux through the ecosystem, whereas dissolved organic N, the primary component of N flux through the system, is not actively cycled. Nitrification was also a significant flux of N in the stream, with rates in the water column and surface of benthos accounting for approximately 10% of the total ammonium uptake. Primary consumers assimilated 67% of the inorganic N that entered benthic algae and microbes. Predators acquired 23% of the N that consumers obtained. Invertebrate collectors, omnivorous crayfish (Orconectes spp.), and invertebrate shredders dominated the N flux associated with primary consumers. Mass balance calculations indicated that at least 23% of the 309 mg of ¹⁵N added during the 35 days of release was retained within the 210-m stream reach during the release. Overall, the rates of turnover of N in organisms and organic substrata were significantly greater when C:N was low. This ratio may be a surrogate for biological activity with regard to N flux in streams.

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Crossref · 10.1007/s100210000050

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Metadata

Authors
Dodds, W. K., Evans-White, M. A., Gerlanc, N. M., Gray, L., Gudder, D. A., Kemp, M. J., López, A. L., Stagliano, D., Strauss, E. A., Tank, J. L., Whiles, M. R., & Wollheim, W. M.
Affiliations
  • Kansas State University (US)
  • Utah Valley University (US)
  • University of Notre Dame (US)
  • Marine Biological Laboratory (US)
ORCID
Venue
Ecosystems
Publisher
Springer Science and Business Media LLC
Published
2000-11
Volume
3
Issue
6
Pages
574-589
ISSN
1432-9840 (ISSN-L)
DOI
10.1007/s100210000050
OpenAlex
W2064284501
Cited by
154
References
46
Citations by year
2026: 5 · 2025: 5 · 2024: 1 · 2023: 1 · 2022: 5 · 2021: 5 · 2020: 6 · 2019: 9 · 2018: 3 · 2017: 6 · 2016: 5 · 2015: 6 · 2014: 6 · 2013: 5 · 2012: 8
FWCI
5.22
Type
journal article
Language
en
Open access
closed
Licence
www.springer.com/tdm (tdm)
Locations
Ecosystems (publishedVersion)
Topics
  • Physical Sciences › Environmental Science › Environmental Chemistry › Soil and Water Nutrient Dynamics
  • Physical Sciences › Environmental Science › Ecology › Isotope Analysis in Ecology
  • Physical Sciences › Environmental Science › Ecology › Freshwater macroinvertebrate diversity and ecology
Keywords
nitrogen cycling, prairie streams, 15N tracer, nitrogen turnover, nitrogen fluxes, ammonium, dissolved organic nitrogen, nitrification, food webs, mass balance, C/N ratio, benthic invertebrates, crayfish, detritus, Konza Prairie

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