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Determining the grainsize of sediment with increasing depth in core GC11, located in the Capricorn Channel

Created 24/06/2017

Updated 24/06/2017

JSON RDF ISO19115-3 XML

A gravity core (GC11) was collected from a depth of 502 mbsl within the Capricorn Channel, southern Great Barrier Reef (GBR). Samples were separated into different size fractions to determine the % of each grainsize at each sample depth. Although not overly accurate, the information is correlated with analyses of other parameters to impart clues to the environmental changes within the core. The smallest size fraction (<100µm) dominates at all depths, and is particularly pronounced during glacial periods, at 460cm (MIS 10) and at 330cm (MIS 8).

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Title Determining the grainsize of sediment with increasing depth in core GC11, located in the Capricorn Channel
Language English
Licence Creative Commons Attribution 2.5 Australia
Landing Page https://devweb.dga.links.com.au/data/dataset/7fdb4048-876b-4d18-a5c2-44249cafc9ad
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

Data Source

This dataset was originally found on data.gov.au "Determining the grainsize of sediment with increasing depth in core GC11, 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/determining-the-grainsize-of-sediment-with-increasing-depth-in-core-gc11-located-in-the-caprico

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