Published December 2018 | Version v1
Journal article

Variation in Detrital Resource Stoichiometry Signals Differential Carbon to Nutrient Limitation for Stream Consumers Across Biomes

  • 1. Virginia Tech, Department of Biological Sciences (United States)
  • 2. University of Georgia, Odum School of Ecology (United States)
  • 3. Florida International University, Department of Biological Sciences (United States)
  • 4. Southern Illinois University, Department of Zoology (United States)
  • 5. École Polytechnique Fédérale de Lausanne, Stream Biofilm and Ecosystem Research (Switzerland)
  • 6. University of New Hampshire, Department of Natural Resources and the Environment (United States)
  • 7. University of Alaska Fairbanks, Department of Biology and Wildlife (United States)
  • 8. University of Notre Dame, Department of Biological Sciences (United States)

Description

Stoichiometric ratios of resources and consumers have been used to predict nutrient limitation across diverse terrestrial and aquatic ecosystems. In forested headwater streams, coarse and fine benthic organic matter (CBOM, FBOM) are primary basal resources for the food web, and the distribution and quality of these organic matter resources may therefore influence patterns of secondary production and nutrient cycling within stream networks or among biomes. We measured carbon (C), nitrogen (N), and phosphorus (P) content of CBOM and FBOM and calculated their stoichiometric ratios (C/N, C/P, N/P) from first- to fourth-order streams from tropical montane, temperate deciduous, and boreal forests, and tallgrass prairie, to compare the magnitude and variability of these resource types among biomes. We then used the ratios to predict nutritional limitations for consumers of each resource type. Across biomes, CBOM had consistently higher %C and %N, and higher and more variable C/N and C/P than FBOM, suggesting that microbial processing results in more tightly constrained elemental composition in FBOM than in CBOM. Biome-specific differences were observed in %P and N/P between the two resource pools; CBOM was lower in %P but higher in N/P than FBOM in the tropical montane and temperate deciduous forest biomes, while CBOM was higher in %P but similar in N/P than FBOM in the grassland and boreal forest biomes. Stable 13C isotopes suggest that FBOM likely derives from CBOM in tropical and temperate deciduous forest, but that additional non-detrital components may contribute to FBOM in boreal forests and grasslands. Comparisons of stoichiometric ratios of CBOM and FBOM to estimated needs of aquatic detritivores suggest that shredders feeding on CBOM are more likely to experience nutrient (N and/or P) than C limitation, whereas collector–gatherers consuming FBOM are more likely to experience C than N and/or P limitation. Our results suggest that differences in basal resource elemental content and stoichiometric ratios have the potential to affect consumer production and ecosystem rates of C, N, and P cycling in relatively consistent ways across diverse biomes.

Additional details

Publishing Information

Journal Title
Ecosystems (New York. Print)
Journal Volume
21
Journal Issue
8
Journal Page Range
p. 1676-1691
ISSN
1432-9840

INIS

Country of Publication
United States
Country of Input or Organization
International Atomic Energy Agency (IAEA)
INIS RN
54097494
Subject category
S54: ENVIRONMENTAL SCIENCES;
Descriptors DEI
AQUATIC ECOSYSTEMS; CARBON; FORESTS; NUTRIENTS; ORGANIC MATTER; RANGELANDS; SIGNALS; STOICHIOMETRY
Descriptors DEC
ECOSYSTEMS; ELEMENTS; MATTER; NONMETALS; TERRESTRIAL ECOSYSTEMS

Optional Information

Copyright
Copyright (c) 2018 Springer Science+Business Media, LLC, part of Springer Nature
Notes
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