Stabilization of fine gravels by net-spinning caddisfly larvae
Article first published online: 13 NOV 2008
Copyright © 2008 John Wiley & Sons, Ltd.
Earth Surface Processes and Landforms
Volume 34, Issue 3, pages 413–423, 15 March 2009
How to Cite
Johnson, M. F., Reid, I., Rice, S. P. and Wood, P. J. (2009), Stabilization of fine gravels by net-spinning caddisfly larvae. Earth Surf. Process. Landforms, 34: 413–423. doi: 10.1002/esp.1750
- Issue published online: 18 FEB 2009
- Article first published online: 13 NOV 2008
- Manuscript Accepted: 29 JUL 2008
- Manuscript Revised: 16 JUL 2008
- Manuscript Received: 14 MAR 2008
- ecosystem engineering;
- entrainment threshold;
- Shields parameter;
We examined the impact of Hydropsychidae caddisfly larvae on the incipient motion of two sizes of narrowly graded fine-gravel (4–6 and 6–8 mm). This impact was assessed relative to the collective impact of other abiotic and biotic processes that are potentially important conditioning agents of fine-gravels. Trays of gravel were placed in the River Soar, Leicestershire, UK, where they were colonized to natural densities by caddisfly larvae. Identical trays that were surrounded by a 250 µm mesh were also deployed, preventing colonization but allowing field conditioning of sediments, including minor reworking of grains and biofilm development. After 21 days in the river, trays were removed to a laboratory flume where grain entrainment stresses were established. In addition to the colonized and conditioned treatments, critical shear stresses were measured for identical sediments that were not placed in the river (laboratory gravels). Gravels that were colonized by Hydropsychidae required significantly greater shear stresses for entrainment than conditioned trays (p ≤ 0·002), however, there was no significant difference between conditioned and laboratory gravels. This implies that the presence of caddisfly can be a more important influence on fine-gravel stability than some conditioning processes. Shields parameter was compared across treatments and across the two gravel size-fractions using two-way ANOVA. No significant differences or interactions were observed, indicating that 4–6 mm gravel was stabilized to a similar degree as 6–8 mm gravel by conditioning and colonization processes. Our results extend earlier studies in two important ways: (1) entrainment stresses were established for fine gravels that were colonized at natural densities, under natural stream conditions; and (2) the caddisfly effect was measured relative to both field-conditioned and unconditioned laboratory controls. The temporal and spatial distribution of silk-spinning caddisfly larvae suggests that they have the potential to influence fine-sediment mobility in many rivers, worldwide. Copyright © 2008 John Wiley & Sons, Ltd.