Encyclopedia Titanica

Rusticle magnetotaxis elucidating Rustflower formations in RMS Titanic’s Turkish Baths

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During his bio-archaeological Last Mysteries of the Titanic expedition in 2005, explorer James Cameron observed the RMS Titanic’s Turkish Baths, an anoxic chamber secluded from currents deep within the wreck’s remote interior, utilizing the ROV Skipper. There, Cameron discovered anomalously thin, vertical, and bifurcating rus- ticle formations he termed “Rustflowers.” Proposing magnetotaxis as the involved mechanism, this study analyzed rusticles salvaged from Titanic’s #8 davit bitt utilizing ferromagnetic resonance, which demonstrated an asymmetric spectrum featuring prominent uniaxial over magnetocrystalline anisotropy fields of Buni = 110 mT and Bcub = -23 mT, linewidth parameters of ΔB = 200 mT, ΔBFWHM = 144 mT, ΔBhigh = 37 mT, ΔBlow = 107 mT, and asymmetry ratio of A = 0.35, and α = 0.20. These represent the established signature of biogenic magnetofossil chains synthesized by former magnetotactic bacteria, enduring within the rusticle cortex. Electron microscopy and chemical analysis identified single-domain range magnetite nanocrystals, and crystalline elemental sulfur inclusions, respectively. Chemosynthetic microbial iron oxy-hydroxide accretions guided up- ward along geomagnetic field lines by north-seeking magnetotaxis, under reducing conditions exhibited in Ti- tanic’s Turkish Baths, may account for the distinctive morphology of its Rustflowers; adding dimension to the bacterial application of iron assimilated from deep-sea sources, including shipwrecks.

by Anthony El-Khouri, Charles Pellegrino & James Cameron
Key Points

Introduction

  • The RMS Titanic sank on April 15, 1912, and its wreck is covered with rusticles, which are iron oxy-hydroxide precipitates formed by microbial activity.
  • During a 2005 expedition, James Cameron discovered unique rusticle formations called “Rustflowers” in the Titanic’s Turkish Baths.

Methods and Materials

  • Rusticles were collected from the Titanic’s #8 davit bitt for analysis.
  • Techniques used included ferromagnetic resonance (FMR) spectroscopy, scanning electron microscopy (SEM), and transmission electron microscopy (TEM).

Findings

  1. Rusticle Composition:

    • Rusticles are composed of various iron oxy-hydroxides, including goethite and lepidocrocite.
    • They contain crystalline sulfur inclusions, indicating chemosynthetic microbial activity.
  2. Magnetotaxis:

    • Magnetotactic bacteria (MTB) in rusticles use magnetosomes to align with Earth’s geomagnetic field, guiding their movement.
    • FMR analysis showed the presence of biogenic magnetofossil chains, indicating former MTB activity.
  3. Rustflower Formation:

    • Rustflowers are thin, vertical rusticle formations found exclusively in the Turkish Baths.
    • Their unique morphology is influenced by magnetotaxis, with rusticles growing upward along geomagnetic field lines.

Discussion

  • The anoxic and reducing environment of the Turkish Baths preserves the rusticles and supports unique microbial communities.
  • The presence of magnetofossils suggests that MTB played a significant role in the formation of Rustflowers.
  • Rusticles contribute to the biogeochemical iron cycle and may influence seafloor magnetism.

Conclusion

  • Rusticles on the Titanic are microbially-mediated corrosion products that harvest iron from the wreck.
  • Magnetotaxis and the bacterial growth environment contribute to the distinctive Rustflower formations.
  • Further analysis of Rustflowers and the Titanic’s microbial composition could provide more insights into these processes.

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Rusticles Biodeterioration Titanic Wreck James Cameron Turkish Baths

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