{"title":"活性铁控制着沉积岩中黄铁矿与有机质之间的硫分配","authors":"Hadar Cohen-Sadon , Yoav Oved Rosenberg , Simon Emmanuel , Shimon Feinstein , Alon Amrani","doi":"10.1016/j.gca.2025.05.027","DOIUrl":null,"url":null,"abstract":"<div><div>Sulfur isotopic values (δ<sup>34</sup>S) of pyrite and organic matter (OM) in sediments are widely used for the reconstruction of the sulfur and oxygen cycles as well as pathways of OM preservation. Currently, significant uncertainties persist regarding the mechanism by which sulfur is partitioned between pyrite and OM and its effect on the δ<sup>34</sup>S record of rocks. Here, we present experimental analysis of iron, carbon, sulfur and δ<sup>34</sup>S values in marine and lacustrine rock samples. The experimental data was compared with published data of rock samples from the Mesoproterozoic era (1.6 Ga) to the Paleogene period (23 Ma). We also developed a kinetic model to simulate the evolution of δ<sup>34</sup>S of pyrite and OM under different environmental conditions. Our analysis reveals linear relationships between δ<sup>34</sup>S value of pyrite and its isotopic difference from δ<sup>34</sup>S value of organic sulfur (R<sup>2</sup> ranging from 0.43 to 0.96) for large δ<sup>34</sup>S ranges of pyrite (110 ‰) and organic sulfur (93 ‰). These ranges and linear trends cannot be explained by variations in the δ<sup>34</sup>S value of seawater sulfate or by the isotopic fractionation associated with microbial sulfate reduction. Rather, local conditions that change the ratio between reactive iron and sulfate are shown to control the δ<sup>34</sup>S values of organic sulfur and pyrite and their isotopic gap. This is because reactive iron pyritization rapidly captures isotopically light H<sub>2</sub>S generated by microbial sulfate reducers in the early stages of diagenesis, leaving behind heavy H<sub>2</sub>S that reacts with OM. In some environments, the isotopic gap between organic sulfur and pyrite correlates with the OM content in the rock, reflecting the critical role of reactive iron in OM preservation via sulfurization. Hence, the role of iron on the partitioning of sulfur between OM and pyrite in sedimentary environments is essential for reconstructing the sulfur cycle and its interaction with the carbon cycle in geological sequences.</div></div>","PeriodicalId":327,"journal":{"name":"Geochimica et Cosmochimica Acta","volume":"400 ","pages":"Pages 18-31"},"PeriodicalIF":4.5000,"publicationDate":"2025-05-22","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Reactive iron controls sulfur partitioning between pyrite and organic matter in sedimentary rocks\",\"authors\":\"Hadar Cohen-Sadon , Yoav Oved Rosenberg , Simon Emmanuel , Shimon Feinstein , Alon Amrani\",\"doi\":\"10.1016/j.gca.2025.05.027\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>Sulfur isotopic values (δ<sup>34</sup>S) of pyrite and organic matter (OM) in sediments are widely used for the reconstruction of the sulfur and oxygen cycles as well as pathways of OM preservation. Currently, significant uncertainties persist regarding the mechanism by which sulfur is partitioned between pyrite and OM and its effect on the δ<sup>34</sup>S record of rocks. Here, we present experimental analysis of iron, carbon, sulfur and δ<sup>34</sup>S values in marine and lacustrine rock samples. The experimental data was compared with published data of rock samples from the Mesoproterozoic era (1.6 Ga) to the Paleogene period (23 Ma). We also developed a kinetic model to simulate the evolution of δ<sup>34</sup>S of pyrite and OM under different environmental conditions. Our analysis reveals linear relationships between δ<sup>34</sup>S value of pyrite and its isotopic difference from δ<sup>34</sup>S value of organic sulfur (R<sup>2</sup> ranging from 0.43 to 0.96) for large δ<sup>34</sup>S ranges of pyrite (110 ‰) and organic sulfur (93 ‰). These ranges and linear trends cannot be explained by variations in the δ<sup>34</sup>S value of seawater sulfate or by the isotopic fractionation associated with microbial sulfate reduction. Rather, local conditions that change the ratio between reactive iron and sulfate are shown to control the δ<sup>34</sup>S values of organic sulfur and pyrite and their isotopic gap. This is because reactive iron pyritization rapidly captures isotopically light H<sub>2</sub>S generated by microbial sulfate reducers in the early stages of diagenesis, leaving behind heavy H<sub>2</sub>S that reacts with OM. In some environments, the isotopic gap between organic sulfur and pyrite correlates with the OM content in the rock, reflecting the critical role of reactive iron in OM preservation via sulfurization. Hence, the role of iron on the partitioning of sulfur between OM and pyrite in sedimentary environments is essential for reconstructing the sulfur cycle and its interaction with the carbon cycle in geological sequences.</div></div>\",\"PeriodicalId\":327,\"journal\":{\"name\":\"Geochimica et Cosmochimica Acta\",\"volume\":\"400 \",\"pages\":\"Pages 18-31\"},\"PeriodicalIF\":4.5000,\"publicationDate\":\"2025-05-22\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Geochimica et Cosmochimica Acta\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S0016703725002716\",\"RegionNum\":1,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q1\",\"JCRName\":\"GEOCHEMISTRY & GEOPHYSICS\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Geochimica et Cosmochimica Acta","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0016703725002716","RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"GEOCHEMISTRY & GEOPHYSICS","Score":null,"Total":0}
Reactive iron controls sulfur partitioning between pyrite and organic matter in sedimentary rocks
Sulfur isotopic values (δ34S) of pyrite and organic matter (OM) in sediments are widely used for the reconstruction of the sulfur and oxygen cycles as well as pathways of OM preservation. Currently, significant uncertainties persist regarding the mechanism by which sulfur is partitioned between pyrite and OM and its effect on the δ34S record of rocks. Here, we present experimental analysis of iron, carbon, sulfur and δ34S values in marine and lacustrine rock samples. The experimental data was compared with published data of rock samples from the Mesoproterozoic era (1.6 Ga) to the Paleogene period (23 Ma). We also developed a kinetic model to simulate the evolution of δ34S of pyrite and OM under different environmental conditions. Our analysis reveals linear relationships between δ34S value of pyrite and its isotopic difference from δ34S value of organic sulfur (R2 ranging from 0.43 to 0.96) for large δ34S ranges of pyrite (110 ‰) and organic sulfur (93 ‰). These ranges and linear trends cannot be explained by variations in the δ34S value of seawater sulfate or by the isotopic fractionation associated with microbial sulfate reduction. Rather, local conditions that change the ratio between reactive iron and sulfate are shown to control the δ34S values of organic sulfur and pyrite and their isotopic gap. This is because reactive iron pyritization rapidly captures isotopically light H2S generated by microbial sulfate reducers in the early stages of diagenesis, leaving behind heavy H2S that reacts with OM. In some environments, the isotopic gap between organic sulfur and pyrite correlates with the OM content in the rock, reflecting the critical role of reactive iron in OM preservation via sulfurization. Hence, the role of iron on the partitioning of sulfur between OM and pyrite in sedimentary environments is essential for reconstructing the sulfur cycle and its interaction with the carbon cycle in geological sequences.
期刊介绍:
Geochimica et Cosmochimica Acta publishes research papers in a wide range of subjects in terrestrial geochemistry, meteoritics, and planetary geochemistry. The scope of the journal includes:
1). Physical chemistry of gases, aqueous solutions, glasses, and crystalline solids
2). Igneous and metamorphic petrology
3). Chemical processes in the atmosphere, hydrosphere, biosphere, and lithosphere of the Earth
4). Organic geochemistry
5). Isotope geochemistry
6). Meteoritics and meteorite impacts
7). Lunar science; and
8). Planetary geochemistry.