Detail of the Oesia fossil remains in margaretia ‘tube’.Credit: Karma Nanglu
The fossilised remnants of tube-like “dwellings” which housed a primitive type of prehistoric sea worm on the ocean floor have been identified in a new study.
According to researchers, the long, perforated tubes may have looked like narrow chimneys reaching up from the sea bed, and were made by a creature called Oesia, which lived a solitary existence inside them about 500 million years ago.
The findings emerge from a study undertaken by academics from Canada and the UK, in which they reassess fossils originally believed to have come from a type of seaweed called Margaretia. Instead, they found that these were the vestiges of tubular structures which protected these ancient worms.
The research, which is published in the journal BMC Biology, was carried out by academics from the Universities of Cambridge, Toronto and Montréal, and at the Royal Ontario Museum in Toronto.
Part of its importance is that it confirms Oesia was a primitive specimen from a group of creatures called hemichordates. These belong to a bigger group called deuterostomes, of which vertebrates (including humans) form a separate branch. By finding out more about these early creatures, researchers hope eventually to be able to identify and characterise a distant ancestor common to all deuterostomes, from sea worms to humans.
In particular, the research supports the increasingly common view that this ancestor was probably a “filter feeder,” which ate by sucking in water and straining out nutrients. Oesia was one such filter feeder, with gills down most of its body to expel water afterwards, and holes in the walls of its tubular home to let the water in and out.
Karma Nanglu, from the University of Toronto and the study’s lead author, said: “Hemichordates are central to our understanding of how deuterostomes evolved. Through them, we can get clues about the anatomy and lifestyle of the last common ancestor that we all share, and this adds further evidence to the hypothesis that the ancestor was a filter-feeder like Oesia.”
Professor Simon Conway Morris, from St John’s College, University of Cambridge and a co-author, said: “Oesia fossils are pretty enigmatic — they are very rare and until now we could not prove which group they belonged to. Now we know that they were primitive hemichordates — perhaps the most primitive of all.”
The study was possible thanks to the discovery of a rich source of fossilised remains near Marble Canyon, in the Canadian Rockies (Kootenay National Park, B.C.), which is run by Parks Canada.
“Marble Canyon is one of the most recently discovered fossil localities in the Burgess Shale, a geological formation known for its exceptional quality of fossil preservation,” said co-author Dr. Jean-Bernard Caron, Senior Curator of Invertebrate Palaeontology at the Royal Ontario Museum and Associate Professor at the University of Toronto. “Oesia has been known from an older Burgess Shale site for over 100 years, but the specimens from Marble Canyon are far more abundant and better preserved, giving us unprecedented details of the animal’s internal anatomy.”
The research establishes that Oesia was a rather phallic-shaped creature, similar to modern acorn worms with a proboscis, a collar, and a long trunk. Co-author Christopher B. Cameron, Associate Professor at the Université de Montréal said: “Acorn worms are notoriously sparse in the fossil record. Only a handful of fossil species have been described, making the recognition of such an ancient representative of the group particularly noteworthy.”
The average Oesia was about 53mm long, and rarely more than 10mm wide. Unusually, these worms had U-shaped gills running down most the length of their bodies to enable filter feeding. Gill slits seem to be a characteristic common to all deuterostomes; even humans have slits in their necks at an early stage in their embryonic development, and this is seen as evidence that all deuterostomes are related to a distant, common ancestor.
The researchers realised that Oesia must have lived in tubes because among the Marble Canyon finds there are dozens of examples where the fossil remains of the worm are found within those of Margaretia.
Since the 1920s, Margaretia has been classified as a type of algae, albeit one unlike any other known species from this period in prehistory. The direct association with Oesia explains why Margaretia looks so exotic: This was no seaweed, but rather a perforated tube-like structure that the worm inhabited.
The study suggests that in some cases these structures exceeded 50cm in height and that they were typically at least twice the width of the worm, giving it plenty of room. The ends were sealed off, making life inside a rather lonely experience. “Only single worms are found within tubes, suggesting a solitary mode of life,” Nanglu added.
At some point, the fossil record suggests that acorn worms underwent a transition, leaving their tubes and instead opting for a life under the sea bed. The study argues that as evolution gathered pace and more predators appeared on the scene, digging into the sea floor may simply have been a safer option. Certainly, modern-day acorn worms have adopted this lifestyle; rather than filter feeding they live in the sediment and eat nutrients within it.
“In its own depressing way this is a story of Darwinian competition,” Conway Morris explained. “The levels of competition and predation increased, life sped up and got harder, and animals had to protect themselves more. One way of doing this was to abandon life filter feeding in a tube, and instead to dig into the sediment and eat mud. Once there, they found a new niche and were able to make a perfectly good life for themselves.”
Source: St John’s College, University of Cambridge
- Karma Nanglu, Jean-Bernard Caron, Simon Conway Morris, Christopher B. Cameron. Cambrian suspension-feeding tubicolous hemichordates. BMC Biology, 2016; 14 (1) DOI: 10.1186/s12915-016-0271-4