From Australian Oceans Data Network
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Determining the grainsize of sediment with increasing depth in core GC14, located in the Capricorn Channel

Created 13/03/2025

Updated 13/03/2025

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A gravity core (GC14) was collected from a depth of 2004 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. There are small peaks in the coarser grained material at the bottom of the core which relate to pteropod layers in the sediment.

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Title Determining the grainsize of sediment with increasing depth in core GC14, located in the Capricorn Channel
Language eng
Licence notspecified
Landing Page https://devweb.dga.links.com.au/data/dataset/b8e0d74d-9b73-4696-86e8-6f3c575acf6b
Contact Point
CSIRO Oceans & Atmosphere
h.bostock@niwa.co.nz
Reference Period 01/01/1997 - 01/01/1997
Geospatial Coverage {"type": "Polygon", "coordinates": [[[154.0, -24.0], [154.5, -24.0], [154.5, -23.5], [154.0, -23.5], [154.0, -24.0]]]}
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 GC14, 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-gc14-located-in-the-caprico1

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No duplicate datasets found.