Seafloor environments of the northern Lord Howe Rise, Eastern Australia: Extractable metal concentrations in seabed sediments.
Geoscience Australia marine reconnaissance survey TAN0713 to the Lord Howe Rise offshore eastern Australia was completed as part of the Federal Government's Offshore Energy Security Program between 7 October and 22 November 2007 using the New Zealand Government's research vessel Tangaroa. The survey was designed to sample key, deep-sea environments on the east Australian margin (a relatively poorly-studied shelf region in terms of sedimentology and benthic habitats) to better define the Capel and Faust basins, which are two major sedimentary basins beneath the Lord Howe Rise. Samples recovered on the survey contribute to a better understanding of the geology of the basins and assist with an appraisal of their petroleum potential. They also add to the inventory of baseline data on deep-sea sediments in Australia. The principal scientific objectives of the survey were to: (1) characterise the physical properties of the seabed associated with the Capel and Faust basins and Gifford Guyot; (2) investigate the geological history of the Capel and Faust basins from a geophysical and geological perspective; and (3) characterise the abiotic and biotic relationships on an offshore submerged plateau, a seamount, and locations where fluid escape features were evident. This dataset comprises Fe, Co, Cd, Cu, Zn, Ni and Mn concentrations after extraction of seabed sediments in cold, dilute HCl.
Some relevant publications which pertain to these datasets include:
1. Heap, A.D., Hughes, M., Anderson, T., Nichol, S., Hashimoto, T., Daniell, J., Przeslawski, R., Payne, D., Radke, L., and Shipboard Party, (2009). Seabed Environments and Subsurface Geology of the Capel and Faust basins and Gifford Guyot, Eastern Australia - post survey report. Geoscience Australia, Record 2009/22, 166pp.
2. Radke, L.C. Heap, A.D., Douglas, G., Nichol, S., Trafford, J., Li, J., and Przeslawski, R. 2011. A geochemical characterization of deep-sea floor sediments of the northern Lord Howe Rise. Deep Sea Research II 58: 909-921
Simple
Identification info
- Date (Publication)
- 2014-01-01T00:00:00
- Citation identifier
- Geoscience Australia Persistent Identifier/https://pid.geoscience.gov.au/dataset/ga/82535
- Citation identifier
- Digital Object Identifier/http://dx.doi.org/10.4225/25/54B86625BB64C
- Cited responsible party
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Role Organisation / Individual Name Details Publisher Geoscience Australia
Canberra Author Radke, L.C.
1 Author Trafford, J.
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- Point of contact
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Role Organisation / Individual Name Details Custodian EGD
Owner Commonwealth of Australia (Geoscience Australia)
Custodian Commonwealth of Australia (Geoscience Australia)
Voice
- Topic category
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- Oceans
Extent
))
- Maintenance and update frequency
- As needed
- Keywords
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Marine Data
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- Theme
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marine survey
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- Theme
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Continental Shelf
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- Theme
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seabed
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geochemistry
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- Theme
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marine
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AU-QLD
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- Australian and New Zealand Standard Research Classification (ANZSRC)
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Marine Geoscience
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Published_External
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Resource constraints
- Title
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Creative Commons Attribution 4.0 International Licence
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CC-BY
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4.0
- Access constraints
- License
- Use constraints
- License
Resource constraints
- Title
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Australian Government Security ClassificationSystem
- Edition date
- 2018-11-01T00:00:00
- Classification
- Unclassified
- Language
- English
- Character encoding
- UTF8
Distribution Information
- Distributor contact
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Role Organisation / Individual Name Details Distributor Commonwealth of Australia (Geoscience Australia)
Voice
- OnLine resource
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File download
Download the data (xlsx)
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xlsx
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Resource lineage
- Statement
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Bottom sediments were collected using either a box core, benthic sled or Van Veen Grab. Cold dilute hydrochloric acid (1M) metal digests of freeze dried sediments were undertaken following the protocol of Snape et al. (2004). The HCl extracts were analysed by quadrupole ICP-MS at the University of Canberra. All major interfering elements/compounds (i.e., Cl on V, Cr, As and Se) were corrected for. Average %RSD for two stations run in duplicate were 44.1% (Fe), 6.4% (Co), 8.2% (Cd), 1.6% (Cu), 6% (Zn), 12.9% (Ni) and 15.1% (Mn).
Snape, I., Scouller, R.C., Stark, S.C., Stark, J., Riddle, M.J., and Gore, D.B., 2004. Characterisation of the dilute HCl extraction method for the identification of metal contamination in Antarctic marine sediment. Chemosphere 57, 491-504.
Thanks to the crew of the RV Solander for help with sample collection, and Frank Krykowa (University of Canberra) for elemental analysis.
- Hierarchy level
- Dataset
- Description
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Source data not available.
Metadata constraints
- Title
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Australian Government Security ClassificationSystem
- Edition date
- 2018-11-01T00:00:00
- Classification
- Unclassified
Metadata
- Metadata identifier
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urn:uuid/08e3f2c7-2df4-1da5-e054-00144fdd4fa6
- Title
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GeoNetwork UUID
- Language
- English
- Character encoding
- UTF8
- Contact
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Role Organisation / Individual Name Details Point of contact Commonwealth of Australia (Geoscience Australia)
Voice
Type of resource
- Resource scope
- Dataset
- Name
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dataset
Alternative metadata reference
- Title
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Geoscience Australia - short identifier for metadata record with
uuid
- Citation identifier
- eCatId/82535
- Date info (Revision)
- 2018-04-22T08:47:21
- Date info (Creation)
- 2014-11-28T00:00:00
Metadata standard
- Title
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AU/NZS ISO 19115-1:2014
Metadata standard
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ISO 19115-1:2014
Metadata standard
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ISO 19115-3
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Geoscience Australia Community Metadata Profile of ISO 19115-1:2014
- Edition
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Version 2.0, September 2018
- Citation identifier
- https://pid.geoscience.gov.au/dataset/ga/122551