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- W2153296768 abstract "A sedimentological and stratigraphic study of Low Isles Reef off northern Queensland, Australia was carried out to improve understanding of factors that have governed Late Holocene carbonate deposition and reef development on the inner to middle shelf of the northern Great Barrier Reef. Low Isles Reef is one of 46 low wooded island-reefs unique to the northern Great Barrier Reef, which are situated in areas that lie in reach of river flood plumes and where inter-reef sediments are dominated by terrigenous mud. Radiocarbon ages from surface and subsurface sediment samples indicate that Low Isles Reef began to form at ca 3000 y BP, several thousand years after the Holocene sea-level stillstand, and reached sea-level soon after (within ∼500 years). Maximum reef productivity, marked by the development of mature reef flats that contributed sediment to a central lagoon, was restricted to a narrow window of time, between 3000 and 2000 y BP. This interval corresponds to: (i) a fall in relative sea-level, from ∼1 ..." @default.
- W2153296768 created "2016-06-24" @default.
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- W2153296768 date "2008-07-01" @default.
- W2153296768 modified "2023-10-16" @default.
- W2153296768 title "Late Holocene island reef development on the inner zone of the northern Great Barrier Reef: insights from Low Isles Reef" @default.
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- W2153296768 doi "https://doi.org/10.1080/08120090801982835" @default.
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