2008
DOI: 10.1016/j.margeo.2008.02.013
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Influence of climate fluctuations and changes in catchment land use on Late Holocene and modern beach-ridge sedimentation on a tropical macrotidal coast: Keppel Bay, Queensland, Australia

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Cited by 63 publications
(40 citation statements)
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“…OSL has also been used successfully to date relict foredune ridge plains in Australia since the early 2000's (Brooke et al, 2008a(Brooke et al, , 2008bForsyth et al, 2010;Forsyth et al, 2012;Goodwin et al, 2006;Murray-Wallace et al, 2002;Nott et al, 2009). These studies have focused on northern NSW and Queensland, with the exception of Guichen Bay in South Australia.…”
Section: Luminescence Dating Of Coastal Faciesmentioning
confidence: 99%
“…OSL has also been used successfully to date relict foredune ridge plains in Australia since the early 2000's (Brooke et al, 2008a(Brooke et al, , 2008bForsyth et al, 2010;Forsyth et al, 2012;Goodwin et al, 2006;Murray-Wallace et al, 2002;Nott et al, 2009). These studies have focused on northern NSW and Queensland, with the exception of Guichen Bay in South Australia.…”
Section: Luminescence Dating Of Coastal Faciesmentioning
confidence: 99%
“…Accumulation rates along Transects A, B, and C range between 16 and 54 m 3 m −1 yr −1 ( Table 2). The calculated average accumulation rate is exceptionally high compared to that reported for other large beachridge systems, such as 0.05 million m 3 yr −1 at Guichen Bay, Australia (Bristow and Pucilllo, 2006), 0.14 million m 3 yr −1 at Keppel Bay, Australia (Brooke et al, 2008a), and 1.7 million m 3 yr −1 at Kujukuri, Japan (Tamura et al, 2010). As these systems are much shorter than the UsumacintaGrijalva plain, accumulation rates are more similar when expressed in m 3 m −1 yr −1 .…”
Section: Volumetric Growth Rate Of the Beach-ridge Plainmentioning
confidence: 51%
“…Combined 14 C and OLS dating provided a robust and consistent chronological framework for these phases, which substantially improved the existing chronology based on radiocarbon-dated shell material (Aguayo et al, 1999 Figure 12. Periodicities of beach-ridge formation for the Usumacinta-Grijalva (Us-Gr) system compared with reported or estimated values for other large beach-ridge systems: Rockingham Bay (Forsyth et al, 2010), Beachmere (Brooke et al, 2008b), Moruya (Oliver et al, 2015), Guichen Bay (Murray Wallace et al, 2002;Bristow and Pucillo, 2006), Keppel Bay (Brooke et al, 2008a), Shark Bay (Nott, 2011), Cowley Beach (Nott et al, 2009), Lake Michigan (Thompson, 1992), St. Vincent Island (Lopez and Rink, 2008;Rink and Lopez, 2010), Jerup (Nielsen et al, 2006), Nayarit (Curray et al, 1969), and Rio Grande do Sul (Milana et al, 2017).…”
Section: Discussionmentioning
confidence: 99%
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“…Low inorganic nitrogen concentrations in the water column together with moderate concentrations of iron and available-P in the sediment (Table 3), may account for the apparent occurrence of benthic N-fixation in this region. Webster and Radke (2006) have estimated that benthic N-fixation supplies 3,200 ± 1,700 t N year -1 to inner Keppel Bay, which is nearly half of the amount delivered from the catchment (Brooke et al 2008). However, the implied Nfixation rates in this study were high (up to 3.5 mmol day -1 ), and were based on correlations between sediment Fe 3?…”
Section: The Coastal Transition Zonementioning
confidence: 66%