JSON RDF ISO19115-3 XML

Determining the grainsize of sediment with increasing depth in core GC14, located in the Capricorn Channel

Created 24/06/2017

Updated 24/06/2017

JSON RDF ISO19115-3 XML

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.

Files and APIs

Tags

Additional Info

Field Value
Title Determining the grainsize of sediment with increasing depth in core GC14, located in the Capricorn Channel
Language English
Licence Creative Commons Attribution 2.5 Australia
Landing Page https://devweb.dga.links.com.au/data/dataset/2f630cb9-fafb-42c8-88d0-270db750e6ea
Contact Point
National Institute of Water and Atmosphere (NIWA)
h.bostock@niwa.co.nz
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-caprico

Original dataset
Dataset copies

No duplicate datasets found.