Origins of sulphide in sediments
Sulphide in sedimentary ore deposits may be derived directly from the mantle or by reduction of sulphate. Sulphide in modem hydrothermal deposits is thought to have formed abiologically by reactions between sulphate and ferrous iron or organic matter during deep circulation of sea water and meteoric waters through the crust at temperatures above about 200°C. Below about 70°C sulphate reduction is catalysed by bacteria. This process is widespread in anoxic basins and reducing sediments, and is dependent upon, and often controlled by, the supply of organic matter. The importance of sulphate reduction in carbon turnover has been demonstrated by comparisons of organic carbon production and sulphate reduction in marine sediments and by the discovery of several genera of sulphate-reducing bacteria capable of using a wide range of organic molecules. Recent kinetic studies of sulphate reduction in anoxic marine sediments have confirmed that sulphide accumulations equivalent to those in several major stratiform ores could be generated biologically. Fixed sulphide contents in normal unconsolidated reduced marine sediments, however, are generally an order of magnitude less than those of deposits such as at McArthur River and Mount Isa in the Northern Territory of Australia. The only modern examples of sediments with large fixed sulphide concentrations are those in which sulphide is of hydrothermal origin. One constraint on the concentration of fixed sulphides in sediments is the availability of reactable metals. It is possible that high concentrations of biogenic sulphides can be produced when metalliferous hydrothermal fluids are exhaled into biologically active anoxic basins or depressions.
Simple
Identification info
- Date (Publication)
- 1981-01-01T00:00:00
- Citation identifier
- Geoscience Australia Persistent Identifier/https://pid.geoscience.gov.au/dataset/ga/81087
- Cited responsible party
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Role Organisation / Individual Name Details Publisher Bureau of Mineral Resources, Geology and Geophysics
Canberra Author Trudinger, P.A.
1
- Name
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BMR Journal of Australian Geology and Geophysics
- Issue identification
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6:4:279-285
- Point of contact
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Role Organisation / Individual Name Details Custodian Corp
Owner Commonwealth of Australia (Geoscience Australia)
Custodian Commonwealth of Australia (Geoscience Australia)
Voice
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- Geoscientific information
- Maintenance and update frequency
- Unknown
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Product data repository: Various Formats
- Website
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Data Store directory containing the digital product files
Data Store directory containing one or more files, possibly in a variety of formats, accessible to Geoscience Australia staff only for internal purposes
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GA Publication
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Journal
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- Australian and New Zealand Standard Research Classification (ANZSRC)
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Earth Sciences
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- Keywords
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Published_External
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Resource constraints
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Creative Commons Attribution 4.0 International Licence
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CC-BY
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4.0
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Australian Government Security ClassificationSystem
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- 2018-11-01T00:00:00
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Distribution Information
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Role Organisation / Individual Name Details Distributor Commonwealth of Australia (Geoscience Australia)
Voice
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Journal article (pdf)
Journal article (pdf)
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pdf
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Resource lineage
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Unknown
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GA Publication
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Source data not available.
Metadata constraints
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Australian Government Security ClassificationSystem
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Metadata
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urn:uuid/fae9173a-701c-71e4-e044-00144fdd4fa6
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GeoNetwork UUID
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Role Organisation / Individual Name Details Point of contact Commonwealth of Australia (Geoscience Australia)
Voice
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AGSO BMR Journal
Alternative metadata reference
- Title
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Geoscience Australia - short identifier for metadata record with
uuid
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- eCatId/81087
- Date info (Revision)
- 2018-04-20T06:10:07
- Date info (Creation)
- 2014-06-03T00:00:00
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
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Version 2.0, September 2018
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