气候变化领域集成服务门户(CCPortal): Multiple sulfur isotope signals associated with the late Smithian event and the Smithian/Spathian boundary

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DOI	10.1016/j.earscirev.2018.06.019
	Multiple sulfur isotope signals associated with the late Smithian event and the Smithian/Spathian boundary
	Thomazo C.; Brayard A.; Elmeknassi S.; Vennin E.; Olivier N.; Caravaca G.; Escarguel G.; Fara E.; Bylund K.G.; Jenks J.F.; Stephen D.A.; Killingsworth B.; Sansjofre P.; Cartigny P.
发表日期	2019
ISSN	00128252
起始页码	96
结束页码	113
卷号	195
英文摘要	The Early Triassic is generally portrayed as a time of various, high ecological stresses leading to a delayed biotic recovery after the devastating end-Permian mass extinction. This interval is notably characterized by repeated biotic crises (e.g., during the late Smithian), large-scale fluctuations of the global carbon, nitrogen and sulfur cycles as well as harsh marine conditions including a combination of ocean acidification, anoxia, extreme seawater temperatures and shifting productivity. Observations from different paleolatitudes suggest that sulfidic (H2S-rich) conditions may have developed widely during the Early Triassic, possibly reaching up to ultra-shallow environments in some places. However, the existence and the spatio-temporal extent of such redox swings remain poorly constrained. In order to explore Early Triassic paleoceanographic redox changes and their potential influences on the biotic recovery, we analyzed multiple sulfur isotopes (32S, 33S, 34S, and 36S) of sedimentary pyrite and carbonate associated sulfate (δ34SCAS) from the Mineral Mountains section, Utah. Sediments from this section were mainly deposited in shallow waters and span the Smithian and lower Spathian. We report a 68‰ range of variations in δ34Spy associated with Δ33Spy varying from −0.01‰ to +0.12‰, whereas the δ34SCAS varies between +19.5‰ and + 34.8‰. We interpret the observed signal of multiple sulfur isotopes as reflecting the operation of pore-water synsedimentary microbial sulfate reduction in open system with respect to sulfates before the late Smithian, evolving to a closed system, sulfate limited, Rayleigh-type distillation across the Smithian/Spathian boundary (SSB) and immediately after the SSB. We argue that this marked change is driven by the effectiveness of the connection between the sedimentary pore waters and the overlying water column, which is, in this case, controlled by the local sedimentological conditions such as the bioturbation intensity and the sedimentation rate. Therefore, our results suggest that changes in the sulfur cycle before and across the SSB at Mineral Mountains is probably a local consequence of the loss of the mixed sedimentary layer during the late Smithian extinction event, as opposed to reflecting the development of a lethal anoxic ocean at the global scale. © 2018 Elsevier B.V.
英文关键词	carbonate; hydrogen sulfide; marine environment; paleoceanography; paleoenvironment; paleolatitude; Permian-Triassic boundary; pyrite; redox conditions; sulfate; sulfur isotope; Mineral Mountains; United States; Utah
语种	英语
来源期刊	Earth Science Reviews
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/203571
作者单位	Laboratoire Biogéosciences, UMR 6282, CNRS, Université Bourgogne Franche-Comté, Dijon, 21000, France; Université Clermont Auvergne, CNRS, Laboratoire Magmas et Volcans, Clermont-Ferrand, F-63000, France; Laboratoire d'Ecologie des Hydrosystèmes Naturels et Anthropisés, UMR 5023, CNRS, Université de Lyon, Villeurbanne Cedex, 69622, France; 140 South 700 East, Spanish Fork, UT 84660, United States; 1134 Johnson Ridge Lane, West Jordan, UT 84084, United States; Department of Earth Science, Utah Valley Univ., Orem, UT 84058, United States; CNRS-UMR6538 Lab. Géosciences Océan, Université de Bretagne Occidentale, Plouzané, 29280, France; Institut de Physique du Globe de Paris, Sorbonne-Paris Cité, Univ. Paris Diderot, CNRS, Paris Cedex 05, 75238, France
推荐引用方式 GB/T 7714	Thomazo C.,Brayard A.,Elmeknassi S.,et al. Multiple sulfur isotope signals associated with the late Smithian event and the Smithian/Spathian boundary[J],2019,195.
APA	Thomazo C..,Brayard A..,Elmeknassi S..,Vennin E..,Olivier N..,...&Cartigny P..(2019).Multiple sulfur isotope signals associated with the late Smithian event and the Smithian/Spathian boundary.Earth Science Reviews,195.
MLA	Thomazo C.,et al."Multiple sulfur isotope signals associated with the late Smithian event and the Smithian/Spathian boundary".Earth Science Reviews 195(2019).