Coastal Restoration Trust of New Zealand

Coastal Dune Ecosystem Reference Database

The role of waves in the colonisation of terrestrial sediments deposited in the marine environment. Journal Paper

Author
Hewitt, J.E., Cummings, V.J., Ellis, J.I., Funnell, G., Norkko, A., Talley, T.S., Thrush, S.F.
Year
2003
Journal / Source
Journal of Experimental Marine Biology and Ecology
Publisher / Organisation
Elsevier
Number
290
Pages
19-47
Keywords
Bioturbation; Macrobenthic recovery dynamics; Sedimentation; Terrestrial impacts; Wind waves; Bedload transport
Summary
Elevated rates of sediment run-off, as a result of changes in land-use and climate, are a significant threat to marine coastal communities, with a potential to cause broad-scale, long-term alteration of habitats. Individual sedimentation events can smother estuarine flats with terrigenous sediments, creating a significant disturbance to local benthic communities. Variations in the degree to which a habitat is altered, the rate at which mixing occurs, and species-specific dispersal and responses to the altered habitat, suggest that colonisation of terrestrial sediment depositions will vary with location, both between and within estuaries. This study was designed to explore the effect that variations in wave-induced hydrodynamics would have on long-term colonisation of terrestrial sediment depositions on intertidal flats. Sites for the experimental deposition of terrestrial sediment were located along a gradient in wave exposure, with only limited variation in immersion times (30 min) and ambient sediment particle sizes (predominantly fine sand). Over 20 months, periodic measurements were made of factors predicted to affect colonisation: the sediment characteristics of the deposited sediment; local-scale wave climate; bioturbation of the deposited sediment; and local populations of benthic invertebrates. Neither opportunistic use of the new resource, progressive recovery or facilitation by colonising macrofauna was observed. Little vertical mixing of the deposited and existing sediment by either waves or bioturbators occurred; instead bedload transport was the dominant process. Local differences in hydrodynamic conditions and macrobenthic communities resulted in site-specific colonisation of the experimental plots. The strength and duration of the macrofaunal response to deposited sediment observed in this study suggest that chronic small-scale (m’s) patchy deposition of terrestrial sediment in the intertidal marine environment has a strong potential to alter both habitats and communities.