Landscape Ecology

, Volume 28, Issue 4, pp 685–698

Ecosystem-scale spatial heterogeneity of stable isotopes of soil nitrogen in African savannas


    • Department of Earth SciencesIndiana University-Purdue University, Indianapolis (IUPUI)
    • Water Research Center, School of Civil and Environmental EngineeringUniversity of New South Wales
  • Gregory S. Okin
    • Department of GeographyUniversity of California, Los Angeles
  • Paolo D’Odorico
    • Department of Environmental SciencesUniversity of Virginia
  • Kelly K. Caylor
    • Department of Civil and Environmental EngineeringPrinceton University
  • Stephen A. Macko
    • Department of Environmental SciencesUniversity of Virginia
Research Article

DOI: 10.1007/s10980-012-9776-6

Cite this article as:
Wang, L., Okin, G.S., D’Odorico, P. et al. Landscape Ecol (2013) 28: 685. doi:10.1007/s10980-012-9776-6


Soil 15N is a natural tracer of nitrogen (N) cycling. Its spatial distribution is a good indicator of processes that are critical to N cycling and of their controlling factors integrated both in time and space. The spatial distribution of soil δ15N and its underlying drivers at sub-kilometer scales are rarely investigated. This study utilizes two sites (dry vs. wet) from a megatransect in southern Africa encompassing locations with similar soil substrate but different rainfall and vegetation, to explore the effects of soil moisture and vegetation distribution on ecosystem-scale patterns of soil δ15N. A 300-m long transect was set up at each site and surface soil samples were randomly collected for analyses of δ15N, %N and nitrate content. At each soil sampling location the presence of grasses, woody plants, Acacia species (potential N fixer) as well as soil moisture levels were recorded. A spatial pattern of soil δ15N existed at the dry site, but not at the wet site. Woody cover distribution determined the soil δ15N spatial pattern at ecosystem-scale; however, the two Acacia species did not contribute to the spatial pattern of soil δ15N. Grass cover was negatively correlated with soil δ15N at both sites owing to the lower foliar δ15N values of grasses. Soil moisture did not play a role in the spatial pattern of soil δ15N at either site. These results suggest that vegetation distribution, directly, and water availability, indirectly, affect the spatial patterns of soil δ15N through their effects on woody plant and grass distributions.


C3 plants C4 plants Geostatistics Isotope Kalahari Savannas Soil δ15N Soil nitrogen Stable isotopes

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© Springer Science+Business Media B.V. 2012