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Shifting modes of iron sulfidization at the onset of OAE-2 drive regional shifts in pyrite δ34S records

Journal Article · · Chemical Geology
 [1];  [2];  [3];  [4];  [2]
  1. Washington Univ., St. Louis, MO (United States); Univ. of Chicago, IL (United States); Washington Univ., St. Louis, MO (United States)
  2. Washington Univ., St. Louis, MO (United States)
  3. Washington Univ., St. Louis, MO (United States); Univ. of California, Santa Barbara, CA (United States)
  4. Florida State Univ., Tallahassee, FL (United States). National High Magnetic Field Lab. (MagLab)
We report total reduced inorganic S isotope ratios (δ34SCRS) shift toward more negative values across much of the southern North Atlantic just before the onset of the Cenomanian-Turonian Ocean Anoxic Event (OAE-2). At the same time, there is no parallel isotopic change in the significantly larger pool of kerogen (organic) S, which indicates that the distribution and S-isotope composition of sulfide in the environment likely did not drive the change in δ34SCRS. Here, we investigate possible explanations for the negative shift in δ34SCRSvalues and their divergence from organic S by isolating iron sulfides for morphological identification and grain-specific isotopic analysis using secondary ion mass spectrometry (SIMS). In pre- and syn-OAE-2 sedimentary rocks from Demerara Rise, we find four distinct morphologies of iron sulfides: pyrite framboids (1–20 μm diameter), irregular pyrite aggregates (1–38 μm diameter), large cemented pyrite aggregates (~60 μm diameter), and irregular and cemented aggregates of the pyrite polymorph marcasite (1–45 μm diameter). These different textural groups have distinct S-isotopic compositions that are largely consistent through the onset of OAE-2. As such, the secular change in bulk δ34SCRS values likely reflects the changing proportions of these phases stratigraphically across OAE-2. All textural groups feature resolvable intra-grain δ34S variability, suggesting that the environments in which they formed were characterized by dynamic sulfide δ34S values and/or by partial closed-system distillation. We use grain-specific δ34S distributions to rule out shoaling of the chemocline within the sediments as a mechanism for the observed decrease in δ34SCRS. Instead, we propose that changes in the reactivity of the iron species delivered to Demerara Rise over the ~200 kyr leading up to the onset of OAE-2 impacted the relative contributions of pyrite with S-isotope signatures reflecting the water column, shallow sediments, and deeper sediments to the bulk sedimentary δ34SCRS value. Specifically, the change in iron reactivity at the onset of OAE-2 favored the production of 34S-depleted large, cemented aggregates and framboids at the expense of more 34S-enriched irregular aggregates. Our results underscore that bulk δ34SCRS measurements integrate multiple reduced phases that form via distinct reaction mechanisms and potentially in different parts of the depositional environment. Grain-specific SIMS analyses dramatically enrich our ability to interpret pyrite isotopic patterns in the geologic record.
Research Organization:
Washington Univ., St. Louis, MO (United States)
Sponsoring Organization:
American Chemical Society Petroleum Research; National Science Foundation (NSF); State of Florida; USDOE Office of Science (SC), Biological and Environmental Research (BER); Washington University
Grant/Contract Number:
SC0014613
OSTI ID:
1851965
Alternate ID(s):
OSTI ID: 1810899
Journal Information:
Chemical Geology, Journal Name: Chemical Geology Journal Issue: C Vol. 553; ISSN 0009-2541
Publisher:
ElsevierCopyright Statement
Country of Publication:
United States
Language:
English

References (65)

Geochemical characterization of black shales from the Tarfaya Basin collection January 2002
Biogeochemical sulfur cycling during Cretaceous oceanic anoxic events: A comparison of OAE1a and OAE2: CRETACEOUS OCEAN ANOXIA AND SULFUR journal February 2016
Investigation of the quasi-simultaneous arrival (QSA) effect on a CAMECA IMS 7f-GEO: Investigation of the QSA effect on a CAMECA IMS 7f-GEO journal March 2017
Sulfur isotope analysis of microcrystalline iron sulfides using secondary ion mass spectrometry imaging: Extracting local paleo-environmental information from modern and ancient sediments journal February 2019
Determination of the absolute32S/34S ratio of IAEA-S-1 reference material and V-CDT sulfur isotope standard journal August 1999
The use of chromium reduction in the analysis of reduced inorganic sulfur in sediments and shales journal January 1986
Kinetic controls on depth variations in localised pyrite formation journal July 1993
A warm, equable Cretaceous: The nature of the problem journal August 1983
A theoretical model of the stable sulfur isotope distribution in marine sediments journal March 1979
Marcasite precipitation from hydrothermal solutions journal December 1986
The size distribution of framboidal pyrite in modern sediments: An indicator of redox conditions journal October 1996
Biogeochemical cycles of carbon and sulfur and their effect on atmospheric oxygen over phanerozoic time journal January 1989
Sulfide oxidation and iron dissolution kinetics during the reaction of dissolved sulfide with ferrihydrite journal December 2003
Reaction pathways in the Fe–S system below 100°C journal June 2000
Modeling atmospheric O2 over Phanerozoic time journal March 2001
Oxidation of detrital pyrite as a cause for Marcasite Formation in marine lag deposits from the Devonian of the eastern US journal June 2007
Amino acid biogeochemistry and organic matter degradation state across the Pakistan margin oxygen minimum zone journal March 2009
Experimental syntheses of framboids—a review journal August 2005
Empirical links between trace metal cycling and marine microbial ecology during a large perturbation to Earth's carbon cycle journal September 2016
Quantifying the missing sink for global organic carbon burial during a Cretaceous oceanic anoxic event journal October 2018
Paired organic matter and pyrite δ34S records reveal mechanisms of carbon, sulfur, and iron cycle disruption during Ocean Anoxic Event 2 journal April 2019
Cretaceous black shales as active bioreactors: A biogeochemical model for the deep biosphere encountered during ODP Leg 207 (Demerara Rise) journal January 2006
Effect of electron donors on the fractionation of sulfur isotopes by a marine Desulfovibrio sp. journal August 2011
Basin-scale controls on the molybdenum-isotope composition of seawater during Oceanic Anoxic Event 2 (Late Cretaceous) journal April 2016
Theoretical estimates of equilibrium sulfur isotope effects in aqueous sulfur systems: Highlighting the role of isomers in the sulfite and sulfoxylate systems journal December 2016
Microscale reservoir effects on microbial sulfur isotope fractionation journal April 2017
Oxygen and sulfur isotopes in sulfate in modern euxinic systems with implications for evaluating the extent of euxinia in ancient oceans journal May 2017
Fe(III):S(-II) concentration ratio controls the pathway and the kinetics of pyrite formation during sulfidation of ferric hydroxides journal November 2017
Dynamics of pyrite formation and organic matter sulfurization in organic-rich carbonate sediments journal November 2018
Reprint of “The effect of biogeochemical processes on pH” journal July 2007
Paleo-redox conditions during OAE 2 reflected in Demerara Rise sediment geochemistry (ODP Leg 207) journal March 2009
Crystal Growth of Pyrite in Aqueous Solutions. Inhibition by Organophosphorus Compounds journal February 1998
Stable organic carbon isotope stratigraphy across Oceanic Anoxic Event 2 of Demerara Rise, western tropical Atlantic: CARBON ISOTOPE STRATIGRAPHY journal June 2005
Geochemistry of oceanic anoxic events: REVIEW journal March 2010
The mid-Cretaceous North Atlantic nutrient trap: Black shales and OAEs: MID-CRETACEOUS N. ATLANTIC NUTRIENT TRAP journal October 2010
Black shale deposition, atmospheric CO 2 drawdown, and cooling during the Cenomanian-Turonian Oceanic Anoxic Event: CO 2 DRAWDOWN AND COOLING DURING OAE2 journal July 2011
Iron isotope and trace metal records of iron cycling in the proto-North Atlantic during the Cenomanian-Turonian oceanic anoxic event (OAE-2): OAE-2 Fe ISOTOPES journal August 2012
Evaluating structure selection in the hydrothermal growth of FeS2 pyrite and marcasite journal December 2016
A unifying model for Neoproterozoic–Palaeozoic exceptional fossil preservation through pyritization and carbonaceous compression journal December 2014
Hydrothermal vents as a kinetically stable source of iron-sulphide-bearing nanoparticles to the ocean journal May 2011
Warm saline intermediate waters in the Cretaceous tropical Atlantic Ocean journal May 2008
Volcanic triggering of a biogeochemical cascade during Oceanic Anoxic Event 2 journal January 2010
Global niche of marine anaerobic metabolisms expanded by particle microenvironments journal March 2018
Influence of sulfate reduction rates on the Phanerozoic sulfur isotope record journal June 2013
Sulfur isotopes track the global extent and dynamics of euxinia during Cretaceous Oceanic Anoxic Event 2 journal October 2013
SQUID-SIMS is a useful approach to uncover primary signals in the Archean sulfur cycle journal April 2014
Intracellular metabolite levels shape sulfur isotope fractionation during microbial sulfate respiration journal October 2014
Phanerozoic cycles of sedimentary carbon and sulfur journal August 1981
Secondary Ion Mass Spectrometry Methodology for Isotopic Ratio Measurement of Micro‐Grains in Thin Sections: True Grain Size Estimation and Deconvolution of Inter‐Grain Size Gradients and Intra‐Grain Radial Gradients journal December 2018
Geochemical Characterization of Cenomanian/Turonian Black Shales from the Tarfaya Basin (sw Morocco). Relationships Between Palaeoenvironmental Conditions and Early Sulphurization of Sedimentary Organic Matter1 journal July 2002
Constraining the rate of oceanic deoxygenation leading up to a Cretaceous Oceanic Anoxic Event (OAE-2: ~94 Ma) journal August 2017
Seawater Sulfur Isotope Fluctuations in the Cretaceous journal June 2004
Large Sulfur Isotope Fractionation Does Not Require Disproportionation journal June 2011
Pyritization of soft-bodied fossils: Beecher's Trilobite Bed, Upper Ordovician, New York State journal January 1991
Pyrite formation in the water column and sediments of a meromictic lake journal January 1998
Nd isotopic excursion across Cretaceous ocean anoxic event 2 (Cenomanian-Turonian) in the tropical North Atlantic journal January 2008
Evolution of middle to Late Cretaceous oceans—A 55 m.y. record of Earth's temperature and carbon cycle journal February 2012
Rethinking the Ancient Sulfur Cycle journal May 2015
Variability in the Raman Spectrum of Unpolished Growth and Fracture Surfaces of Pyrite Due to Laser Heating and Crystal Orientation journal October 2017
Marcasite in Black Shales--a Mineral Proxy for Oxygenated Bottom Waters and Intermittent Oxidation of Carbonaceous Muds journal June 2011
Questioning the biogenicity of Neoproterozoic superheavy pyrite by SIMS journal September 2018
Kinetics and mechanism of pyrite formation at low temperatures journal June 1975
Pyrite texture, isotopic composition and the availability of iron journal October 1982
The reactivity of sedimentary iron minerals toward sulfide journal November 1992
The evolution of the Earth surface sulfur reservoir journal December 2004

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