Discovery of Holocene ooid shoals in a siliciclastic delta, De Grey River, North West Shelf, Australia

Onshore and offshore site investigations along the dryland tide-dominated De Grey River delta (northwestern Australia) led to the unexpected discovery of the largest yet-known marine ooid shoals in the Indo-Pacific region. Ooids exhibit up to 60 tangential aragonitic laminae that were formed around...

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Bibliographic Details
Published in:Geology (Boulder) 2023-04, Vol.51 (4), p.366-371
Main Authors: Lebrec, Ulysse, Lang, Simon C, Paumard, Victorien, O'Leary, Michael, Yokoyama, Yusuke, Hacker, Jorg, Webster, Jody
Format: Article
Language:English
Subjects:
absolute age
Aragonite
Arid lands
Arid zones
Australasia
Australia
Beach ridges
C-14
carbon
Carbonates
Cenozoic
Chemical precipitation
De Grey River delta
deltaic environment
East Indian Ocean
Fluvial sediments
Geochronology
Geology
Geomorphology
Geophysical data
Holocene
Indian Ocean
isotopes
Laminates
lithofacies
North West Shelf
Offshore
Ooids
oolite
paleoenvironment
petrography
Precipitation
Quaternary
Quaternary geology
radioactive isotopes
Ridges
Rivers
Runoff
Shoals
upper Holocene
Western Australia
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Summary:Onshore and offshore site investigations along the dryland tide-dominated De Grey River delta (northwestern Australia) led to the unexpected discovery of the largest yet-known marine ooid shoals in the Indo-Pacific region. Ooids exhibit up to 60 tangential aragonitic laminae that were formed around fluvial sediment grains during the late Holocene. Covering an area >1250 km2, their spatial extent rivals in size individual ooid shoals from the Bahamas. Shoals appear to be spatially linked with the De Grey River, suggesting that fluvial outputs, combined with a macrotidal range, facilitated the precipitation of the ooids. Following their formation, ooids were reworked through tidal and wave processes along the delta. As a result, the delta sedimentary features, including beach ridges, mouth bars, and distributary channels, are composed of ooids. This discovery broadens the range of depositional and climatic environments in which ooids can form and demonstrates that fluvial runoff may not inhibit aragonite precipitation. Such a configuration also provides a unique analogue for ancient ooids found in association with siliciclastic grains and further indicates that the interpretation of typical siliciclastic geomorphologies from geophysical data does not preclude the presence of carbonate grains.
ISSN:0091-7613
1943-2682
DOI:10.1130/G50840.1