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The percentage of calcium carbonate in samples taken from various depths in core GC09, located in the Capricorn Channel.

Created 24/06/2017

Updated 24/06/2017

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A gravity core (GC09) was collected from a depth of 166m within the Capricorn Channel, southern Great Barrier Reef (GBR). The percentage of calcium carbonate in samples collected from different depths was analysed, along with other parameters, to determine changes in carbonate mineralogy and terrestrial influx. The lowest percentage of calcium carbonate was recorded at ~60cm depth corresponding to the Last Glacial Maximum (LGM). The increase in the percentage of silt and mud during the LGM relates to a reduction in bioclastic carbonate production.

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Title The percentage of calcium carbonate in samples taken from various depths in core GC09, located in the Capricorn Channel.
Language English
Licence Creative Commons Attribution 2.5 Australia
Landing Page https://devweb.dga.links.com.au/data/dataset/be1e0a69-4828-4f8d-b07e-ce2020707bc7
Contact Point
National Institute of Water and Atmosphere (NIWA)
h.bostock@niwa.co.nz
Geospatial Coverage {"type": "Polygon", "coordinates": [[[151.5, -24.5], [153.0, -24.5], [153.0, -23.0], [151.5, -23.0], [151.5, -24.5]]]}
Data Portal data.gov.au

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This dataset was originally found on data.gov.au "The percentage of calcium carbonate in samples taken from various depths in core GC09, located in the Capricorn Channel.". Please visit the source to access the original metadata of the dataset:
https://devweb.dga.links.com.au/data/dataset/the-percentage-of-calcium-carbonate-in-samples-taken-from-various-depths-in-core-gc09-located-i

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