Relating sediment impacts on coral reefs to watershed sources, processes and management: A review

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• 作者：Rebecca Bartley ; Zoe T. Bainbridge ; Stephen E. Lewis ; Frederieke J. Kroon ; Scott N. Wilkinson ; Jon E. Brodie ; D. Mark Silburn
• 关键词：Burdekin ; Great Barrier Reef ; Land management ; Soil erosion ; Water quality
• 刊名：Science of the Total Environment
• 出版年：15 January, 2014
• 年：2014
• 卷：468-469
• 期：Complete
• 页码：1138-1153
• 全文大小：1870 K

文摘

Modification of terrestrial sediment fluxes can result in increased sedimentation and turbidity in receiving waters, with detrimental impacts on coral reef ecosystems. Preventing anthropogenic sediment reaching coral reefs requires a better understanding of the specific characteristics, sources and processes generating the anthropogenic sediment, so that effective watershed management strategies can be implemented. Here, we review and synthesise research on measured runoff, sediment erosion and sediment delivery from watersheds to near-shore marine areas, with a strong focus on the Burdekin watershed in the Great Barrier Reef region, Australia. We first investigate the characteristics of sediment that pose the greatest risk to coral reef ecosystems. Next we track this sediment back from the marine system into the watershed to determine the storage zones, source areas and processes responsible for sediment generation and run-off.

The review determined that only a small proportion of the sediment that has been eroded from the watershed makes it to the mid and outer reefs. The sediment transported > 1 km offshore is generally the clay to fine silt (< 4-16 渭m) fraction, yet there is considerable potential for other terrestrially derived sediment fractions (< 63 渭m) to be stored in the near-shore zone and remobilised during wind and tide driven re-suspension. The specific source of the fine clay sediments is still under investigation; however, the Bowen, Upper Burdekin and Lower Burdekin sub-watersheds appear to be the dominant source of the clay and fine silt fractions. Sub-surface erosion is the dominant process responsible for the fine sediment exported from these watersheds in recent times, although further work on the particle size of this material is required. Maintaining average minimum ground cover > 75% will likely be required to reduce runoff and prevent sub-soil erosion; however, it is not known whether ground cover management alone will reduce sediment supply to ecologically acceptable levels.