Astrobiology Researcher Finds New Microbes
This graphic shows the innovative technology that allowed the scientists to collect samples of water from an aquifer two miles below the ocean without contaminating the samples with ocean water. Courtesy of USC.
Two miles below the surface of the ocean, researchers have discovered new microbes that “breathe” sulfate. The microbes, which have yet to be classified and named, exist in massive undersea aquifers—networks of channels in porous rock beneath the ocean where water continually churns. About one-third of Earth’s biomass is thought to exist in this largely uncharted environment.
“It was surprising to find new bugs, but when we go to warmer, relatively old and isolated fluids, we find a unique microbial community,” said Alberto Robador, the lead author of the paper on the findings who began the project while he was a UH NASA Astrobiology Institute (NAI) postdoctoral fellow.
“Finding diverse microbial life here on Earth helps us understand what kinds of life may exist elsewhere in our solar system and on planets orbiting other stars,” explained IfA astronomer Karen Meech, the head of UH NAI.
Sulfate is a compound of sulfur and oxygen that occurs naturally in seawater. It is used commercially in everything from car batteries to bath salts and can be aerosolized by the burning of fossil fuels, increasing the acidity of the atmosphere.
Microbes that breathe sulfate—that is, gain energy by reacting sulfate with organic (carbon-containing) compounds—are thought to be some of the oldest types of organisms on Earth. Other species of sulfate-breathing microbes can be found in marshes and hydrothermal vents.
Researchers from UH and the University of Southern California took their samples from the Juan de Fuca Ridge (off the coast of Washington state), where previous teams had placed underwater laboratories, drilled into the ocean floor. To place the labs, they lowered a drill through two miles of ocean and bored through several hundred feet of ocean sediment and into the rock where the aquifer flows.
Like the microbes on the forest floor that break down leaf litter and dead organisms, the microbes in the ocean also break down organic (carbon-based) material such as dead fish and algae. Unlike their counterparts, however, the microbes beneath the ocean crust often lack the oxygen that is used on land to effect the necessary chemical reaction.
Instead, these microbes can use sulfate to break down carbon from decaying biological material that sinks to the sea bottom and makes its way into the crustal aquifer, producing carbon dioxide.
Learning how these new microbes function will be important to getting a more accurate, quantified understanding of the overall global carbon cycle—a natural cycling of carbon through the environment in which it is consumed by plants, exhaled by animals and enters the ocean via the atmosphere. This cycle is currently being disrupted by man-made carbon dioxide emissions.
“This is the first direct account of microbial activity in these type of environments, and shows the potential of these organisms to respire organic carbon,” said Robador, who is now a postdoctoral research associate at USC’s Center for Dark Energy Biosphere Investigations (C-DEBI).