Clifford E. Kraft1, William S. Keeton2, and Dana R. Warren1. (1) Dept. of Natural Resources, Cornell University, Ithaca, NY 14853-3001, (2) Rubenstein School of Environment and Natural Resources, University of Vermont, 343 Aiken Center, Burlington, VT 05405
We identified structural attributes of old-growth hardwood-conifer riparian forests in the Adirondack Mountains of New York that influenced in-stream wood recruitment and dynamics along 1st and 2nd order streams. Sites were classified as mature forest (6 sites), mature with remnant old-growth trees (3 sites), and old-growth (10 sites). Forest structure was characterized over stream channels and at varying distances from each stream bank. Large logs, debris dams and pools were surveyed; a line-intercept method was used to measure wood volume in streams and on the riparian forest floor. In-stream wood volumes were significantly greater at old-growth sites (200 m3/ha) compared to mature sites (34 m3/ha) and were strongly influenced by the basal area of adjacent forests. In-stream large-log densities correlated strongly with debris-dam densities. AIC models that included large-log density, debris-dam density, boulder density, and bankfull width provided the most support for predicting pool density. A greater proportion of wood-formed pools was found at old-growth sites by comparison with mature sites that were dominated by boulder-formed pools. Old-growth riparian forests provide in-stream habitat features that have not been widely recognized in eastern North America, representing another potential benefit of riparian forest management upon in-stream processes.