2013
DOI: 10.1007/978-94-007-7019-5_9
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South Australia’s Large Inverse Estuaries: On the Road to Ruin

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Cited by 21 publications
(6 citation statements)
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“…The demography of southern Australian bottlenose dolphins in the inner area of Coffin Bay is characterized by high year‐round abundance (265; 95% CI: 253–278), and low temporary emigration rates (0.02; 95% CI: 0.01–0.11; Passadore et al., ). Shallow, sheltered, inverse estuaries like Coffin Bay are highly productive (Kämpf, ); and reports of water quality indicate high nutrients loads particularly in the inner area of Coffin Bay (EPA, ). Moreover, Coffin Bay is an important nursery and feeding area for several fish and cephalopod species (DENR, ) that are known to constitute part of the diet of bottlenose dolphins in South Australia (Gibbs, Harcourt, & Kemper, ).…”
Section: Introductionmentioning
confidence: 99%
“…The demography of southern Australian bottlenose dolphins in the inner area of Coffin Bay is characterized by high year‐round abundance (265; 95% CI: 253–278), and low temporary emigration rates (0.02; 95% CI: 0.01–0.11; Passadore et al., ). Shallow, sheltered, inverse estuaries like Coffin Bay are highly productive (Kämpf, ); and reports of water quality indicate high nutrients loads particularly in the inner area of Coffin Bay (EPA, ). Moreover, Coffin Bay is an important nursery and feeding area for several fish and cephalopod species (DENR, ) that are known to constitute part of the diet of bottlenose dolphins in South Australia (Gibbs, Harcourt, & Kemper, ).…”
Section: Introductionmentioning
confidence: 99%
“…Interference between M2 and S2 tidal constituents on their own give rise to pronounced neap tides that, at times, can result in extremely small tidal ranges of ,20 cm. In the neighbouring gulfs, Spencer Gulf and Gulf St. Vincent, this tidal feature is historically known as ''dodge tide'' (e.g., Kämpf, 2014).…”
Section: Tidal Currentsmentioning
confidence: 99%
“…Most inverse estuaries are found in hot arid climates. Examples include the Persian Gulf (Kämpf and Sadrinasab, 2006;Sadrinasab and Kämpf, 2004), South Australian gulfs: Spencer Gulf and Gulf St. Vincent (De Silva Samarasinghe, 1998;Kämpf, Brokensha, and Bolton, 2009;Kämpf, Payne, and Malthouse, 2010;Nunes and Lennon, 1986;Nunes Vaz, Lennon, and Bowers, 1990), the upper Gulf of California (Lav, God, and Alvarez, 1998), the upper reaches of San Diego Bay (Largier, 2010), and various smaller systems such as Laguna Ojo de Liebre (Postma, 1965), Laguna de Guyamas (Valle-Levinson, Delgado, and Atkinson, 2001), Laguna San Ignacio (Winant and de Velasco, 2011), the Coorong lagoon (Kämpf, 2014), Mission Bay (Largier, Hearn, and Chadwick, 1996), Shark Bay (Burling, Ivey, and Pattiaratchi, 1999), Hervey Bay (Ribbe, 2006), and the Great Barrier Reef (Andutta, Ridd, and Wolanski, 2011). Largier (2010) gives a comprehensive overview of the general dynamics that govern such low-inflow estuaries.…”
Section: Introductionmentioning
confidence: 98%
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