Trapping of mangrove propagules due to density-driven secondary circulation in the Normanby River estuary, NE Australia
Stieglitz, Thomas, and Ridd, Peter V. (2001) Trapping of mangrove propagules due to density-driven secondary circulation in the Normanby River estuary, NE Australia. Marine Ecology-Progress Series, 211 . pp. 131-142.
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View at Publisher Website: http://dx.doi.org/10.3354/meps211131
The dispersal of mangrove propagules in the Normanby River estuary is dominated by secondary estuarine circulation. On flood tides, an axial surface convergence forms midstream, generated by a density-driven circulation cell. Floating material including mangrove propagules is trapped in the convergence, and moves upstream. On ebb tides, the circulation cell reverses, and propagules move towards the banks, where water velocities are much smaller than midstream. Over a tidal cycle, a net upstream drift of propagules occurs. This displacement effect occurs throughout the tropical dry season. Buoyant propagules of Rhizophora stylosa, Bruguiera gymnorrhiza, Xylocarpus mekongensis and Heritiera littoralis have been found to be transported upstream at a speed comparable to a net average speed of 3.2 km d-1, found in a drift-drogue experiment. The propagules subsequently accumulate in large numbers in hydrodynamic traps upstream from the convergence and, more importantly, upstream from the mangrove fringe. The hydrodynamic trapping conflicts with the temporal and spatial requirements of propagules to Œfind¹ a habitat suitable for development.
|Item Type:||Article (Refereed Research - C1)|
|Keywords:||convergence; dispersal; estuarine circulation; mangroves; propagules; salinity gradient|
|FoR Codes:||04 EARTH SCIENCES > 0405 Oceanography > 040503 Physical Oceanography @ 100%|
|SEO Codes:||97 EXPANDING KNOWLEDGE > 970102 Expanding Knowledge in the Physical Sciences @ 100%|
|Deposited On:||29 Jun 2012 16:16|
|Last Modified:||29 Jun 2012 18:02|
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