Isotopic data of pyrite (δ34S) and barite (δ34S, δ18O) in the Canol Formation (Selwyn Basin, Canada)
The stable isotopic composition of pyrite (δ34Spyrite) and barite (δ34Sbarite, δ18Obarite) in marine sedimentary rocks provides a valuable archive for reconstructing the biogeochemical processes that link the sulfur, carbon, and iron cycles. Highly positive δ34Spyrite values that exceed coeval unmod...
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GFZ Data Services
2021
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Online Access: | https://dx.doi.org/10.5880/gfz.3.1.2021.006 https://dataservices.gfz-potsdam.de/panmetaworks/showshort.php?id=2b55b861-f511-11eb-9603-497c92695674 |
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ftdatacite:10.5880/gfz.3.1.2021.006 |
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record_format |
openpolar |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
unknown |
topic |
Pyrite Barite in-situ isotope analyses sulfur microbial sulfate reduction anaerobic oxidation of methane Late Devonian Selwyn Basin biochemical process > anaerobic process chemical > isotope compound material > rock > sedimentary rock > generic mudstone > mudstone EARTH SCIENCE > SOLID EARTH > GEOCHEMISTRY > GEOCHEMICAL PROCESSES > OXIDATION/REDUCTION EARTH SCIENCE > SOLID EARTH > GEOCHEMISTRY > GEOCHEMICAL PROPERTIES > ISOTOPE MEASUREMENTS EARTH SCIENCE > SOLID EARTH > ROCKS/MINERALS/CRYSTALS > MINERALS > MINERAL PHYSICAL/OPTICAL PROPERTIES > COMPOSITION/TEXTURE In Situ/Laboratory Instruments > Spectrometers/Radiometers > SIMS Phanerozoic > Paleozoic > Devonian > Late/Upper Devonian |
spellingShingle |
Pyrite Barite in-situ isotope analyses sulfur microbial sulfate reduction anaerobic oxidation of methane Late Devonian Selwyn Basin biochemical process > anaerobic process chemical > isotope compound material > rock > sedimentary rock > generic mudstone > mudstone EARTH SCIENCE > SOLID EARTH > GEOCHEMISTRY > GEOCHEMICAL PROCESSES > OXIDATION/REDUCTION EARTH SCIENCE > SOLID EARTH > GEOCHEMISTRY > GEOCHEMICAL PROPERTIES > ISOTOPE MEASUREMENTS EARTH SCIENCE > SOLID EARTH > ROCKS/MINERALS/CRYSTALS > MINERALS > MINERAL PHYSICAL/OPTICAL PROPERTIES > COMPOSITION/TEXTURE In Situ/Laboratory Instruments > Spectrometers/Radiometers > SIMS Phanerozoic > Paleozoic > Devonian > Late/Upper Devonian Grema, Haruna M. Magnall, Joseph M. Whitehouse, Martin J. Gleeson, Sarah A. Schulz, Hans -M. Isotopic data of pyrite (δ34S) and barite (δ34S, δ18O) in the Canol Formation (Selwyn Basin, Canada) |
topic_facet |
Pyrite Barite in-situ isotope analyses sulfur microbial sulfate reduction anaerobic oxidation of methane Late Devonian Selwyn Basin biochemical process > anaerobic process chemical > isotope compound material > rock > sedimentary rock > generic mudstone > mudstone EARTH SCIENCE > SOLID EARTH > GEOCHEMISTRY > GEOCHEMICAL PROCESSES > OXIDATION/REDUCTION EARTH SCIENCE > SOLID EARTH > GEOCHEMISTRY > GEOCHEMICAL PROPERTIES > ISOTOPE MEASUREMENTS EARTH SCIENCE > SOLID EARTH > ROCKS/MINERALS/CRYSTALS > MINERALS > MINERAL PHYSICAL/OPTICAL PROPERTIES > COMPOSITION/TEXTURE In Situ/Laboratory Instruments > Spectrometers/Radiometers > SIMS Phanerozoic > Paleozoic > Devonian > Late/Upper Devonian |
description |
The stable isotopic composition of pyrite (δ34Spyrite) and barite (δ34Sbarite, δ18Obarite) in marine sedimentary rocks provides a valuable archive for reconstructing the biogeochemical processes that link the sulfur, carbon, and iron cycles. Highly positive δ34Spyrite values that exceed coeval unmodified seawater sulfate (δ34Spyrite > δ34SSO4(SW)), have been recorded in both modern sediments and ancient sedimentary records and are interpreted to result from various biotic and abiotic processes under a range of environmental conditions. A host of processes, including basin restriction, euxinia, low seawater sulfate, dissimilatory microbial sulfate reduction, sulfide reoxidation, and sulfur disproportionation, have been suggested to account for the formation of highly positive δ34Spyrite values in marine environments. Significantly, determining which of these factors was responsible for the pyrite formation is impeded by a lack of constraints for coeval sulfate, with relatively few examples available where δ34Spyrite and proxies for δ34Ssulfate values (e.g., barite) have been paired at high resolution. In the Selwyn Basin, Canada, the Late Devonian sedimentary system is host to large, mudstone-hosted bedded barite units. These barite units have been interpreted in the past as distal expressions of SEDEX mineralization. However, recent studies on similar settings have highlighted how barite may have formed by diagenetic processes before being subsequently replaced during hydrothermal sulfide mineralization. Coincidentally, highly positive δ34Sbarite values have been recorded in such barite occurring coevally with pyrite in diagenetic redox front, where sulfate reduction is coupled to anaerobic oxidation of methane (SR-AOM) at the sulfate methane transition zone (SMTZ). The mechanisms of sulfur cycling and concurrent processes are, nevertheless, poorly constrained. Grema et al. (2021) integrate high-resolution scanning electron microscopy petrography of barite (+ associated barium phases) and pyrite, together with microscale isotopic microanalyses of δ34Spyrite, δ34Sbarite, and δ18Obarite of selected samples from the Late Devonian Canol Formation of the Selwyn Basin. Samples containing both barite and pyrite were targeted to develop paired isotopic constraints on the evolution of sulfur during diagenesis. We have focused on the precise mechanism by which highly positive δ34Spyrite values developed in the Canol Formation and discuss the implications for interpreting sulfur isotopes in similar settings. This data report comprises microscale secondary ion mass spectrometry (SIMS) analyses of the isotopic compositions of pyrite (δ34Spyrite; n= 200) and barite (δ34Sbarite; n= 485, δ18Obarite; n= 338) in nine stratigraphic sections of the Northwest Territories’ part of the Selwyn Basin. Microdrills of regions of interest (n= 54) were made on polished sections to obtain suitable subsamples, using a 4 mm diameter diamond core drill. Several representative subsamples were cast into 25 mm epoxy pucks, together with reference materials (RMs) of pyrite S0302A (δ34S V-CDT = 0.0 ± 0.2‰ (Liseroudi et al., 2021)) and barite S0327 (δ34SV-CDT = 11.0 ± 0.5 ‰; δ18OV-SMOW = 21.3 ± 0.2 ‰ (Magnall et al., 2016)). Microscale isotopic analyses were carried out using Cameca IMS1280 large-geometry secondary ion mass spectrometer (SIMS) operated in multi-collector mode at the NordSIMS laboratory, Stockholm, Sweden. External analytical reproducibility (1 σ) was typically ± 0.04‰ δ34S for pyrite, ± 0.15‰ δ34S, and ± 0.12‰ δ18O for barite. The sample identification, location, and depth are reported in the data files. |
format |
Dataset |
author |
Grema, Haruna M. Magnall, Joseph M. Whitehouse, Martin J. Gleeson, Sarah A. Schulz, Hans -M. |
author_facet |
Grema, Haruna M. Magnall, Joseph M. Whitehouse, Martin J. Gleeson, Sarah A. Schulz, Hans -M. |
author_sort |
Grema, Haruna M. |
title |
Isotopic data of pyrite (δ34S) and barite (δ34S, δ18O) in the Canol Formation (Selwyn Basin, Canada) |
title_short |
Isotopic data of pyrite (δ34S) and barite (δ34S, δ18O) in the Canol Formation (Selwyn Basin, Canada) |
title_full |
Isotopic data of pyrite (δ34S) and barite (δ34S, δ18O) in the Canol Formation (Selwyn Basin, Canada) |
title_fullStr |
Isotopic data of pyrite (δ34S) and barite (δ34S, δ18O) in the Canol Formation (Selwyn Basin, Canada) |
title_full_unstemmed |
Isotopic data of pyrite (δ34S) and barite (δ34S, δ18O) in the Canol Formation (Selwyn Basin, Canada) |
title_sort |
isotopic data of pyrite (δ34s) and barite (δ34s, δ18o) in the canol formation (selwyn basin, canada) |
publisher |
GFZ Data Services |
publishDate |
2021 |
url |
https://dx.doi.org/10.5880/gfz.3.1.2021.006 https://dataservices.gfz-potsdam.de/panmetaworks/showshort.php?id=2b55b861-f511-11eb-9603-497c92695674 |
long_lat |
ENVELOPE(-138.287,-138.287,62.799,62.799) |
geographic |
Northwest Territories Canol Canada Selwyn |
geographic_facet |
Northwest Territories Canol Canada Selwyn |
genre |
Northwest Territories |
genre_facet |
Northwest Territories |
op_relation |
https://dx.doi.org/10.3389/feart.2021.784824 https://dx.doi.org/10.1144/jgs2020-175 https://dx.doi.org/10.1016/j.gca.2016.02.015 |
op_rights |
Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.5880/gfz.3.1.2021.006 https://doi.org/10.3389/feart.2021.784824 https://doi.org/10.1144/jgs2020-175 https://doi.org/10.1016/j.gca.2016.02.015 |
_version_ |
1766150707144032256 |
spelling |
ftdatacite:10.5880/gfz.3.1.2021.006 2023-05-15T17:46:50+02:00 Isotopic data of pyrite (δ34S) and barite (δ34S, δ18O) in the Canol Formation (Selwyn Basin, Canada) Grema, Haruna M. Magnall, Joseph M. Whitehouse, Martin J. Gleeson, Sarah A. Schulz, Hans -M. 2021 https://dx.doi.org/10.5880/gfz.3.1.2021.006 https://dataservices.gfz-potsdam.de/panmetaworks/showshort.php?id=2b55b861-f511-11eb-9603-497c92695674 unknown GFZ Data Services https://dx.doi.org/10.3389/feart.2021.784824 https://dx.doi.org/10.1144/jgs2020-175 https://dx.doi.org/10.1016/j.gca.2016.02.015 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 CC-BY Pyrite Barite in-situ isotope analyses sulfur microbial sulfate reduction anaerobic oxidation of methane Late Devonian Selwyn Basin biochemical process > anaerobic process chemical > isotope compound material > rock > sedimentary rock > generic mudstone > mudstone EARTH SCIENCE > SOLID EARTH > GEOCHEMISTRY > GEOCHEMICAL PROCESSES > OXIDATION/REDUCTION EARTH SCIENCE > SOLID EARTH > GEOCHEMISTRY > GEOCHEMICAL PROPERTIES > ISOTOPE MEASUREMENTS EARTH SCIENCE > SOLID EARTH > ROCKS/MINERALS/CRYSTALS > MINERALS > MINERAL PHYSICAL/OPTICAL PROPERTIES > COMPOSITION/TEXTURE In Situ/Laboratory Instruments > Spectrometers/Radiometers > SIMS Phanerozoic > Paleozoic > Devonian > Late/Upper Devonian dataset Dataset 2021 ftdatacite https://doi.org/10.5880/gfz.3.1.2021.006 https://doi.org/10.3389/feart.2021.784824 https://doi.org/10.1144/jgs2020-175 https://doi.org/10.1016/j.gca.2016.02.015 2022-02-08T18:05:53Z The stable isotopic composition of pyrite (δ34Spyrite) and barite (δ34Sbarite, δ18Obarite) in marine sedimentary rocks provides a valuable archive for reconstructing the biogeochemical processes that link the sulfur, carbon, and iron cycles. Highly positive δ34Spyrite values that exceed coeval unmodified seawater sulfate (δ34Spyrite > δ34SSO4(SW)), have been recorded in both modern sediments and ancient sedimentary records and are interpreted to result from various biotic and abiotic processes under a range of environmental conditions. A host of processes, including basin restriction, euxinia, low seawater sulfate, dissimilatory microbial sulfate reduction, sulfide reoxidation, and sulfur disproportionation, have been suggested to account for the formation of highly positive δ34Spyrite values in marine environments. Significantly, determining which of these factors was responsible for the pyrite formation is impeded by a lack of constraints for coeval sulfate, with relatively few examples available where δ34Spyrite and proxies for δ34Ssulfate values (e.g., barite) have been paired at high resolution. In the Selwyn Basin, Canada, the Late Devonian sedimentary system is host to large, mudstone-hosted bedded barite units. These barite units have been interpreted in the past as distal expressions of SEDEX mineralization. However, recent studies on similar settings have highlighted how barite may have formed by diagenetic processes before being subsequently replaced during hydrothermal sulfide mineralization. Coincidentally, highly positive δ34Sbarite values have been recorded in such barite occurring coevally with pyrite in diagenetic redox front, where sulfate reduction is coupled to anaerobic oxidation of methane (SR-AOM) at the sulfate methane transition zone (SMTZ). The mechanisms of sulfur cycling and concurrent processes are, nevertheless, poorly constrained. Grema et al. (2021) integrate high-resolution scanning electron microscopy petrography of barite (+ associated barium phases) and pyrite, together with microscale isotopic microanalyses of δ34Spyrite, δ34Sbarite, and δ18Obarite of selected samples from the Late Devonian Canol Formation of the Selwyn Basin. Samples containing both barite and pyrite were targeted to develop paired isotopic constraints on the evolution of sulfur during diagenesis. We have focused on the precise mechanism by which highly positive δ34Spyrite values developed in the Canol Formation and discuss the implications for interpreting sulfur isotopes in similar settings. This data report comprises microscale secondary ion mass spectrometry (SIMS) analyses of the isotopic compositions of pyrite (δ34Spyrite; n= 200) and barite (δ34Sbarite; n= 485, δ18Obarite; n= 338) in nine stratigraphic sections of the Northwest Territories’ part of the Selwyn Basin. Microdrills of regions of interest (n= 54) were made on polished sections to obtain suitable subsamples, using a 4 mm diameter diamond core drill. Several representative subsamples were cast into 25 mm epoxy pucks, together with reference materials (RMs) of pyrite S0302A (δ34S V-CDT = 0.0 ± 0.2‰ (Liseroudi et al., 2021)) and barite S0327 (δ34SV-CDT = 11.0 ± 0.5 ‰; δ18OV-SMOW = 21.3 ± 0.2 ‰ (Magnall et al., 2016)). Microscale isotopic analyses were carried out using Cameca IMS1280 large-geometry secondary ion mass spectrometer (SIMS) operated in multi-collector mode at the NordSIMS laboratory, Stockholm, Sweden. External analytical reproducibility (1 σ) was typically ± 0.04‰ δ34S for pyrite, ± 0.15‰ δ34S, and ± 0.12‰ δ18O for barite. The sample identification, location, and depth are reported in the data files. Dataset Northwest Territories DataCite Metadata Store (German National Library of Science and Technology) Northwest Territories Canol Canada Selwyn ENVELOPE(-138.287,-138.287,62.799,62.799) |