Encyclopedia Titanica

Mesoscale ocean eddies determine dispersal and connectivity of corals at the RMS Titanic wreck site

Deep-Sea Research

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The sinking of the RMS Titanic on 15 April 1912 remains one of most iconic maritime disasters in history. Today, the wreck site lies in waters 3800 m deep approximately 690 km south southeast of Newfoundland, Atlantic Canada. The wreck and debris field have been colonized by many marine organisms including the octocoral Chrysogorgia agassizii. Because of the rapid deterioration of the Titanic and the vulnerability of natural deep-sea coral populations to environmental changes, it is vital to understand the role the Titanic as well as other such structures could play in connecting ecosystems along the North American slope. Based on Lagrangian experiments with more than one million virtual particles and different scenarios for larval behavior, given the uncertainties around the biology of chrysogorgiids, the dispersal of larvae spawned at the Titanic wreck is studied in a high-resolution numerical ocean model. While the large-scale bathymetry shields the Titanic from a strong mean flow, mesoscale ocean eddies can considerably affect the deep circulation and cause a significant speed up, or also a reversal, of the circulation. As a consequence, the position of upper and mid-ocean eddies in the model largely controls the direction and distance of larval dispersal, with the impact of eddies outweighing the importance of active larval swimming in our experiments. Although dependent on larval buoyancy and longevity, we find that the Titanic could be reached by larvae spawned on the upper slope east of the Grand Banks. Therefore, the Titanic could act as a stepping stone connecting the upper to the deep continental slope off Newfoundland. From the Titanic, larvae then spread into deep Canadian waters and areas beyond national jurisdiction.

by Tobias Schulzki, Lea-Anne Henry b, J. Murray Roberts, Maria Rakka, Steve W. Ross, Arne Biastoch
Key Points

Introduction

  • The RMS Titanic wreck, located 3800 meters deep, serves as a hard substratum for marine organisms, including the octocoral Chrysogorgia agassizii.
  • Understanding the Titanic’s role in connecting ecosystems is crucial due to its rapid deterioration and the vulnerability of deep-sea coral populations.

Methods and Materials

  • The study used high-resolution numerical ocean models and Lagrangian experiments with over one million virtual particles to simulate larval dispersal from the Titanic.
  • Various scenarios for larval behaviour were considered, given the uncertainties around the biology of Chrysogorgia species.

Findings

  1. Dispersal Pathways:
    • Larvae from the Titanic follow two main pathways: westward along the 3500-meter isobath and southward between the 3500 and 4000-meter isobaths.
    • Mesoscale ocean eddies significantly influence these pathways, outweighing the effects of mean flow and larval swimming behaviour.
  2. Role of Eddies:
    • Eddies can cause a significant speed-up or reversal of the deep circulation, affecting larval dispersal.
    • The position of eddies largely controls the direction and distance of larval dispersal.
  3. Connectivity:
    1. The Titanic could act as a stepping stone, connecting the upper continental slope off Newfoundland to deeper waters.
    2. Larvae from the Titanic can spread into deep Canadian waters and areas beyond national jurisdiction.

Discussion

  • The study highlights the importance of mesoscale eddies in determining larval dispersal patterns.
  • The Titanic’s role in marine connectivity is influenced by stochastic processes on subseasonal timescales.
  • Further research on larval biology and behaviour is needed to refine these findings.

Conclusion

  • The Titanic plays a significant role in ecosystem connectivity, potentially acting as a stepping stone for coral dispersal.
  • Understanding the interaction between ocean dynamics and larval behavior is crucial for conservation efforts.

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This item is not available to read on Encyclopedia Titanica, but we have included it as a reference, provided a brief summary of the key points, and linked to the original source to help readers interested in the finer details of the Titanic story.

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