2010
DOI: 10.2112/jcoastres-d-10-00079.1
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Dynamic Assessment of Oceanic Connectivity in a Coastal Lagoon—the Coorong, Australia

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Cited by 5 publications
(3 citation statements)
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“…Freshwater flow interacts with marine sediments at the mouth of estuaries. Turbulent wave action in the coastal surf zone resuspends sediments which are transported by flood tides and deposited in the mouths of estuaries, forming sand bars (Webster 2010;Whitfield et al, 2012). Scouring by freshwater flows can reduce sand bar development and maintain a connection to the sea (#3c Figure 1; Kjerfve, 1994;Webster, 2010;Whitfield et al, 2012).…”
Section: Sediment Dynamicsmentioning
confidence: 99%
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“…Freshwater flow interacts with marine sediments at the mouth of estuaries. Turbulent wave action in the coastal surf zone resuspends sediments which are transported by flood tides and deposited in the mouths of estuaries, forming sand bars (Webster 2010;Whitfield et al, 2012). Scouring by freshwater flows can reduce sand bar development and maintain a connection to the sea (#3c Figure 1; Kjerfve, 1994;Webster, 2010;Whitfield et al, 2012).…”
Section: Sediment Dynamicsmentioning
confidence: 99%
“…Turbulent wave action in the coastal surf zone resuspends sediments which are transported by flood tides and deposited in the mouths of estuaries, forming sand bars (Webster 2010;Whitfield et al, 2012). Scouring by freshwater flows can reduce sand bar development and maintain a connection to the sea (#3c Figure 1; Kjerfve, 1994;Webster, 2010;Whitfield et al, 2012). An open connection to the sea allows for flushing of sediments, nutrients and contaminants out of the estuary (Adams et al, 2020).…”
Section: Sediment Dynamicsmentioning
confidence: 99%
“…In these systems, geomorphological processes originate geoforms (e.g., lagoons, mouths and channels), which are habitats with different physical attributes (e.g., depth, width, substrate) that influence the patterns of composition, richness, abundance, migration and the size-specific spatial use by organisms (Bartholomew et al, 2000;Saintilan, 2004;Franco et al, 2006;França et al, 2009; _________________ Corresponding editor: Yassir Torres Hicks et al, 2010). For example, the mouth and its tidal channels are ecotones connecting the marine with the brackish environment (Webster, 2011;Lacerda et al, 2014). Furthermore, other geoforms such as lagoons, which are partially enclosed areas with low water circulation and more structural complexity (e.g., muddy bottoms, riverine and submerged vegetation), are reported as critical habitat for juvenile fish feeding and nurseries (Neves et al, 2013;Verdiell-Cubedo et al, 2013).…”
Section: Introductionmentioning
confidence: 99%