Isotopic composition of sulphur in pyrite from sediment core CRP-2A

DOI

Sample: pyrite, largely oxidized to gypsum. The pyrite is cementing sandstone, interpreted to be an injected sandstone.Objective: as part of a larger survey of pyrite in injected sandstones, the pyrite was analysed for sulphur isotopic composition, to determine if microbial activity was involved in its precipitation. The analysis was done using standard methods at the Scottish Universities Environmental Research Centre, East Kilbride, Glasgow.Interpretation: the very light composition, compared to Oligocene seawater (~+20 per mil), is strong evidence for precipitation by microbial sulphate reduction. The fractionation between the two of over 30 per mil exceeds the 20 per mil maximum likely from non-biological processes.

Identifier
DOI https://doi.pangaea.de/10.1594/PANGAEA.761426
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.761426
Provenance
Creator Parnell, John
Publisher PANGAEA
Contributor Geology & Petroleum Geology, University of Aberdeen
Publication Year 2024
Rights Data access is restricted (moratorium, sensitive data, license constraints)
OpenAccess false
Representation
Resource Type Dataset
Format text/tab-separated-values
Size 2 data points
Discipline Earth System Research
Spatial Coverage (163.719 LON, -77.006 LAT); off Cape Roberts, Ross Sea, Antarctica
Temporal Coverage Begin 1998-10-16T07:30:00Z
Temporal Coverage End 1998-11-25T14:20:00Z