|29 March 2013||Share this article|
Deep-sea vent animals not as isolated as they seem
When researchers first discovered hydrothermal vents in 1977, many speculated that vent animals could be "living fossils" that hadn't changed much for hundreds of millions of years. If these odd creatures were as isolated from outside pressures as they appeared to be, scientists theorized, then they may never have needed to evolve.
Vrijenhoek, who has studied the evolution of vent animals for more than two decades, believes otherwise.
"Sometimes there are these charismatic stories that develop a life of their own," Vrijenhoek said. "Even if they are based on flimsy evidence... the myth lives on."
Scientists have debated this "antiquity hypothesis" since the late 1970s. In recent years, it has slowly lost credibility, due in part to Vrijenhoek's research. His most recent work shows that new species of common vent animals—including worms, mussels, and snails—evolved around the same time as catastrophic environmental events that affected life on land and in the upper ocean. The mass extinction that killed off the dinosaurs roughly 65 million years ago, for example, as well as a drastic warming event roughly 55 million years ago, both appear to have coincided with the onset of new vent species, Vrijenhoek reported in a December 2012 paper in Deep-Sea Research II."We can't assume that these things are protected from what's happening at the surface of the planet," said Vrijenhoek. "They are every bit as susceptible as the surface organisms."
One cause for this vulnerability is their reliance on bacteria to convert vent chemicals into food. This process, called chemosynthesis, calls for particular ocean chemical conditions, including a distinct boundary between oxygen-rich and oxygen-poor water. Vrijenhoek suggests that extreme global environmental changes could have shifted global ocean chemistry enough to disrupt chemosynthesis, even on the deep seafloor.
"If you look at one of these worms, 60 to 70 percent of its mass is bacteria," said Vrijenhoek. "There's more bacteria than there is worm. If you change the [chemical] nature of that zone, you're basically going to knock [the bacteria] out."
To assess whether global events have perturbed vent ecosystems through time, Vrijenhoek analyzed evolutionary evidence from modern and fossilized animals. Though he used the most sophisticated statistical methods available, these analyses are inherently prone to errors. Fossil remains, for example, are often damaged and difficult to identify."When you take a snail and reduce it to something that looks like nothing more than a tiny Chinese hat, there's not a lot of morphology left," said Vrijenhoek. "They have converged on these very simple body plans."
Researchers must also consider that older fossils may exist, but have not been studied, and that some vent animals may not have been preserved in the rock record at all. Evolutionary ages based on fossils, therefore, carry large margins of error.
Another way scientists track evolution is by identifying differences in DNA between two closely related modern species. Researchers have developed calculations to estimate how long each change in DNA takes to arise in different species, providing a rough estimate of the time that has passed since related species diverged from a common ancestor.
Vrijenhoek used such "molecular clocks" to show that many modern vent animals have changed significantly since the first vent animals arose 500 million years ago.
"No matter how hard we work on the molecular clocks," Vrijenhoek said, "we can't think of any way that most of these lineages of vent animals are more than 60 million years old."
Vrijenhoek plans to continue collecting samples from new vent fields to confirm his evidence against the antiquity hypothesis. For now, his results suggest that the families of modern vent animals might be ancient by human standards, but are relatively young in the scheme of Earth's long and tumultuous history.
Article by Laura Poppick
Vrijenhoek, R.C., (2013). On the instability and evolutionary age of deep-sea chemosynthetic communities. Deep-Sea Research Part II: Topical Studies in Oceanography. DOI 10.1016/j.dsr2.2012.12.004 (published online in December 2012).
For more information on this article, please contact Kim Fulton-Bennett:
(831) 775-1835, email@example.com
- Bob Vrijenhoek's research web page
- Web pages describing Vrijenhoek's research on deep-sea hydrothermal vents