, Volume 131, Issue 3, pp 444–452

The fate of nitrogen in gypsy moth frass deposited to an oak forest floor


  • Lynn M. Christenson
    • Institute of Ecosystem Studies, Millbrook, NY 12545, USA
  • Gary M. Lovett
    • Institute of Ecosystem Studies, Millbrook, NY 12545, USA
  • Myron J. Mitchell
    • SUNY College of Environmental and Science Forestry, Syracuse, NY 13210, USA
  • Peter M. Groffman
    • Institute of Ecosystem Studies, Millbrook, NY 12545, USA
Ecosystems Ecology

DOI: 10.1007/s00442-002-0887-7

Cite this article as:
Christenson, L.M., Lovett, G.M., Mitchell, M.J. et al. Oecologia (2002) 131: 444. doi:10.1007/s00442-002-0887-7


Forest defoliation by insects can lead to severe disruptions of the nitrogen (N) cycle resulting in elevated NO3 levels in stream water. To trace the movement of insect-mobilized N in a forest soil, 15N-labeled gypsy moth frass or 15N-labeled oak leaf litter was added to trenched plots in an oak forest over 29 months. Nitrogen movement from the frass or litter was measured in the available, mineralizable, microbial and total soil pools. Uptake of 15N by oak seedlings and inorganic N leaching losses were also measured. No significant differences were found between the frass or leaf treatments for total N in any of the pools. Significant differences were found among the treatments in the distribution of the 15N tracer. Forty percent of the 15N added as frass became incorporated in the soils, with less than 1% found in oak seedlings. Almost 80% of 15N added as leaves remained in the undecomposed leaf material after 2 years. Less than 0.001% of the added 15N was leached in both treatments. Our data indicate that N in frass is mobilized more quickly than N in leaf litter. However, this frass N may be largely unavailable to plants and microorganisms as little of it was found in the extractable, microbial, or readily mineralizable pools.

N cycling Insect defoliation Frass Gypsy moth 15N

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© Springer-Verlag 2002