Related Experiment Video
Updated: Aug 9, 2026

09:31
Preparation of Authigenic Pyrite from Methane-bearing Sediments for In Situ Sulfur Isotope Analysis Using SIMS
Published on: August 31, 2017
Sulfur and iron in shipwrecks cause conservation concerns
Yvonne Fors1, Magnus Sandström
1Department of Structural Chemistry, University of Stockholm, SE-106 91 Stockholm, Sweden.
Chemical Society Reviews
|April 26, 2006
Summary
Marine-archaeological wood from shipwrecks contains sulfur compounds and iron sulfides. Conservation efforts focus on removing acidity and iron, and stabilizing sulfur to prevent wood degradation.
Area of Science:
- Materials Science
- Archaeological Science
- Chemistry
Background:
- Marine-archaeological wood, like that from the Vasa and Mary Rose shipwrecks, accumulates significant organosulfur, pyrite, and iron(II) sulfides when preserved in seawater.
- In museum environments, the oxidation of these sulfur compounds, particularly in the presence of iron ions, leads to severe acidity within the moist wood.
- This acidity poses a significant threat to the long-term preservation of these invaluable historical artifacts.
Purpose of the Study:
- To review and discuss advancements in conservation methodologies for marine-archaeological wood.
- To address the challenges posed by acid and iron accumulation and sulfur compound degradation.
- To provide insights into the analysis and stabilization techniques for sulfur compounds in waterlogged wood.
Main Methods:
- Synchrotron-based sulfur X-ray absorption spectroscopy was employed to identify and quantify sulfur species.
- Analysis of organosulfur compounds, pyrite, and iron(II) sulfides in archaeological wood samples.
- Review of existing and emerging conservation treatments for acid and iron removal.
Main Results:
- Demonstrated considerable accumulation of organosulfur (e.g., thiols), pyrite, and iron(II) sulfides in marine-archaeological wood.
- Identified the potential for severe acidity generation due to sulfur compound oxidation in museum conditions.
- Highlighted the critical role of iron ions in exacerbating the degradation process.
Conclusions:
- Effective conservation strategies must address the removal of both acid and iron from degraded archaeological wood.
- Analysis and stabilization of sulfur compounds are crucial for preventing further deterioration.
- Understanding sulfur chemistry is key to preserving submerged wooden heritage.
Related Concept Videos
Acid Mine Drainage
Mining activities that disturb sulfide-rich rocks, particularly those containing pyrite (FeS₂), initiate a cascade of geochemical and microbiological processes with serious environmental implications. When exposed to air and water, pyrite undergoes oxidation, releasing sulfate, ultimately forming sulfuric acid and mobilizing heavy metals into surrounding water systems. This phenomenon, known as acid mine drainage (AMD), results in low pH waters laden with toxic elements that threaten aquatic...
The Sulfur Cycle
Sulfur, an important element in the chemical makeup of proteins, is recycled through the atmosphere and aquatic and terrestrial environments. Found in the atmosphere as sulfur dioxide (SO2), sulfur is released by decaying organisms, weathered rocks, geothermal vents, volcanos, and burning fossil fuels. It is deposited into the ecosystem, cycled through the biotic community, and either released back into the atmosphere as gas or deposited in marine sediment for long-term storage and eventual...
Corrosion
The degradation of metals due to natural electrochemical processes is known as corrosion. Rust formation on iron, tarnishing of silver, and the blue-green patina that develops on copper are examples of corrosion. Corrosion involves the oxidation of metals. Sometimes it is protective, such as the oxidation of copper or aluminum, wherein a protective layer of metal oxide or its derivatives forms on the surface, protecting the underlying metal from further oxidation. In other cases, corrosion is...
Microbes and Other Elemental Cycles
Microbial activity plays a pivotal role in the biogeochemical cycling of iron and manganese, especially at the redox gradients characteristic of stratified aquatic environments. These cycles are driven by microbial transformations between oxidized and reduced forms of the metals, allowing organisms to exploit them for metabolic energy and structural purposes.Iron Cycling Across Redox GradientsIn neutral, oxygen-rich surface waters, iron is predominantly found in its oxidized, insoluble ferric...
Microbes and the Sulfur Cycle
Sulfur is a vital element in Earth's biogeochemical systems. It transitions through various inorganic states, including sulfate (SO₄²⁻), elemental sulfur (S⁰), and sulfide (S²⁻). Abiotic and biological mechanisms across oxic and anoxic environments intricately mediate these transformations. Sulfate, the most oxidized form of sulfur, is predominantly stored in rocks, marine sediments, and oceanic waters, acting as a long-term reservoir in the global sulfur cycle.In oxic environments,...
Microbial Corrosion
Microbiologically Influenced Corrosion (MIC) is a significant form of material degradation caused by the metabolic activities of microorganisms. This phenomenon poses substantial challenges across various industries, including oil and gas, maritime, and water treatment sectors.MIC occurs when microorganisms, such as bacteria, archaea, and fungi, colonize metal surfaces, forming biofilms that alter the local electrochemical environment. These biofilms can lead to the production of corrosive...

