2011
DOI: 10.1016/j.ecss.2011.05.024
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Resistance among wild invertebrate populations to recurrent estuarine acidification

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Cited by 32 publications
(42 citation statements)
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“…These species may also gain advantage over oysters and gastropods with weakened shells by exposure to estuarine acidification. Such increased susceptibility of weakened oysters and gastropods to predation by a multitude of generalist predators may account for the reduced abundance and skewed sizefrequency distributions we have found for these species at acidified sites (Amaral et al 2011).…”
Section: Discussionmentioning
confidence: 88%
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“…These species may also gain advantage over oysters and gastropods with weakened shells by exposure to estuarine acidification. Such increased susceptibility of weakened oysters and gastropods to predation by a multitude of generalist predators may account for the reduced abundance and skewed sizefrequency distributions we have found for these species at acidified sites (Amaral et al 2011).…”
Section: Discussionmentioning
confidence: 88%
“…Eshky et al 1995, Skov & Hartnoll 2001. Previously, we found no difference in the abundances or size-structures of crabs between acidified and reference sites (Amaral et al 2011) and Russell & Helmke (2002) reported that acidic waters from ASS runoff did not negatively affect the survival of mud crabs Scylla serrata in the wild.…”
Section: Discussionmentioning
confidence: 97%
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“…Following rainfall events, the pH of estuarine waters in the vicinity of these point sources may drop to as low as 2-6 ( Dent and Pons 1995;Sammut et al 1996;NSW DPI 2007). During intervening drier periods, the pH in the vicinity of drains is typically higher (6.5-7.0), although still depressed relative to sites away from drains (7.7-7.9; Amaral et al 2011a). …”
Section: Introductionmentioning
confidence: 99%
“…Estuarine and coastal habitats, the ocean's hotspots for biological diversity and productivity, may be especially vulnerable to ocean acidification. They often receive acidic inputs from freshwater and land run-off, upwelling of the CO 2 -enriched acidified waters as well as from biological CO 2 production, leading to large fluctuations in pH and carbonate chemistry (Mook and Koene, 1975;Cai and Wang, 1998; Thomsen et al, 2010;Amaral et al, 2011). Moreover, the buffering capacity of estuarine waters is considerably lower than that of the open ocean (Mook and Koene, 1975;Cai and Wang, 1998).…”
Section: Introductionmentioning
confidence: 99%