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Paleodictyon nodosum

Extinct burrowing sea creature

  • 5 min read
  • 4 chapters

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Through Burrow, Fossil and Protist

  • Adolf Seilacher who discovered the original fossils of Paleodictyon nodosum hypothesizes that the creature is a worm-like species that burrows into the sediment around hydrothermal vents and deflects water flow through the burrows to catch food or farm its own food.
  • Peter A. Rona, discoverer of the modern burrows, suggests that Paleodictyon nodosum may actually be a large protist. There are other known examples of protists reaching the sizes that Paleodictyon reaches, and they are known to be infaunal.

Scientists ran various tests on the burrows of Paleodictyon and were unable to reach a single conclusion as to the form of Paleodictyon. The one thing that they can agree upon is that there are many markers that suggest that these forms are caused by a creature, and not by geological forces.

Distribution/discovery

Paleodictyon nodosum burrows were originally photographed in 1976 on the Galapagos Rift between 2400–3700m depth. Later, Seilacher and Rona used the deep-water submersible DSV Alvin to recover samples of the same form near the Mid-Atlantic Ridge. These samples were collected between 3430m and 3575m depth, around 26°N and 45°W. These burrows were found in very similar conditions as the ones found along the Galapagos Rift. The biggest similarity between the habitats of all Paleodictyon nodosum is that they are all found along divergent plate boundaries at both active and extinct hydrothermal vents.

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