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 Nordic Special

Through a Glass Darkly
Organisms colonize glass in order to extract energy, “eating” metals such as iron or manganese contained within.
By Leslie Mullen

Plucking Daisyworld
On the hypothetical planet Daisyworld, flowers control the climate. Black daisies absorb sunlight and warm the planet.
By Leslie Mullen

Seeing Life in Viruses
We all try to avoid viruses due to the havoc they can wage on our health. Some viruses do more than create temporary discomfort.
By Leslie Mullen

Iceland Brings Astrobiology Down to Earth
If you want to learn about the role of water on Mars and Europa, Iceland is a good place to start.
By Simon Mitton

Mini-Sub for Tight Spaces
The water locked underneath icecaps or glaciers can tell us about our planet's past and its possibly warmer future. Similar environments on distant worlds could tell us whether life can originate in these harsh conditions. To study the icy depths, a Swedish team of researchers is designing a tiny submersible that can slip down a narrow borehole.
By Michael Schirber

Related links

Glass Munchers under the Sea

Rocking the Cradle of Life

Geomicrobiology in oceanography: microbe-mineral interactions at and below the ocean seafloor

Norwegian Centre for Geobiology

Through a Glass Darkly

By Leslie Mullen

Stained glass windows decorate the world’s most beautiful cathedrals, and the jewel-colored panels often depict religious stories.  According to ongoing research, life may have its own tales to tell in ancient glass. 

St Catherine Stained glass

A life told in stained glass.  This window (c.1300) in St Mary's Church in the village of Deerhurst, England depicts Saint Catherine of Alexandria. The Roman Emperor Maxentius condemned her to death on the breaking wheel (an instrument of torture), but the wheel broke when she touched it, so she was instead beheaded.

Microbes may have lived in volcanic glasses that date back to the Archaean era (3.8 to 2.5 billion years ago).  These organisms colonize glass in order to extract energy, “eating” metals such as iron or manganese contained within.  As they do so, the chemolithoautrophs in volcanic glass may create etchings that remain long after their bodies decay and disappear. 

Volcanic glass forms when hot lava is quickly quenched by cooler waters.  A centimeters-thin veneer of glass forms on the outside of pillow lavas, and when they cool further and are buried the glass on the outside fractures.

microscopic view of tubular structures inside volcanic glass

This is a microscopic view of the tubular structures in a 25-micrometer-thick, polished slice of brown volcanic glass. These are thought to be the borings made by autolithotrophic microbes inside the oceanic crust.
Credit: Scripps Institution of Oceanography

“It’s like making toffee apples,” says Nicola McLoughlin, a researcher at the University of Bergen in Norway. “ It’s brittle, and when the hot glass hits water, it falls to pieces.” These fractures may provide a way for microbes to enter the glass and set up shop.

The connection between microbes and volcanic glass was first made by Ingunn Thorseth and Harald Furnes of the University of Bergen, who noticed dimples and depressions on the surface of volcanic breccias from Iceland.  The sizes and shapes of the pits were similar to the microbes that they found on the same pieces of glass, so they figured the microbes were somehow dissolving the glass. 

But some scientists question whether these marks left in glass are in fact “trace fossils” created by microbes.  Water moving through fractures in the glass can ferry microbes inside, but scientists still debate exactly how the organisms survive within the glass, or how they go about dissolving the glass.  Critics suggest that the pits, grooves and tubular channels could be created by processes such as glass fracturing, fluid moving through the glass, or maybe even crystals growing within the glass. In other words, microbes live in glass houses, but they may not build them.

For McLoughlin, there is little doubt that the structures in volcanic glass are created by microbes.  “The morphologies are so intricate -- the really well-preserved modern examples show spiral and branched shapes -- that I think we can discount bubbles or crystals moving through glass to make channels,” she says.  “I’ve convinced myself these are biological.”

In glasses formed recently on the seafloor, the organic remains of microbes can be found plastered on the walls of the tiny glass structures, and there are still traces of DNA.  Sequence analysis of this DNA has found bacteria and archea which are 1,000 to 10,000 times more abundant than microbial cells found in the overlying deep sea water.  The glass microorganisms include those which use iron and manganese oxidation pathways to produce energy (basaltic glass is rich in this food source).

Barbeton fieldwork

Structures found in basalt from the Indian Ocean.  The structures are believed to have been created by bacteria, which dissolve the glass in order to extract minerals.

By studying the microbes in modern glasses, scientists can compare the structures they may create to those found in more ancient rocks where all physical traces of the organisms are long gone. Similar-shaped granular and tubular textures radiating in from the edges of rims and fractures are preserved in volcanic glass that is millions of years in age.

Even if the structures within the glass are formed by life, how can scientists know if the glass was munched on by ancient or modern microbes?  The most ancient glass McLoughlin has studied comes from the Barberton Greenstone belt in South Africa, which dates back to 3.48 billion years ago.  She has also looked at Australian rocks dating back to 3.35 billion years ago.  Even though the rocks are old, that doesn’t necessarily mean the microbes who dined on them were as well. 

McLoughlin says that titanium-bearing minerals in the glass help to preserve the structures, and also can indicate when the microbes were at work.  As the glass was altered on the ancient seafloor a mineral called titanite was precipitated out of the glass and filled the tubular channels left by the microbes, preserving the structures.

“It makes a cast, like pouring Plaster of Paris into a footprint,” says McLoughlin. 

The ancient glass subsequently went through crystallization changes as it was buried under the seafloor, metamorphosed, and eventually turned into chlorite.  (Chlorite is green, which is why layers of these metamorphosed glasses are known as Greenstone belts).  If the titanite had not filled in the structures before the glass was altered, they would have transformed into chlorite as well.  “So it preserves the textures, and not only that, because it contains minor amounts of radioactive uranium, it can be dated,” says McLoughlin. 

Radiometric dating of the titanite found in Archean pillow lavas by Neil Banerjee and Antonio Simonetti confirmed that the structures also formed in the Archean era.  If microbes made these structures, they had to be nearly as ancient as the once glassy lavas they lived in.

Pilow Lava

These pillow lavas weren’t made for sleeping, but mountaineer Tim Burton still gives it a try.  Note the shiny glassy rind formed by rapid quenching as hot lava came into contact water during emplacement.  Photo credit: Thom Wilch.

These investigations of structures made by microbial life in volcanic glass have implications for studies of the origins of life on Earth and perhaps beyond. Traditionally, scientists who look for life in old rocks focus on cherts, which can preserve fine scale details of delicate organisms. Cherts are sedimentary rocks, formed in places like the tidal zone of a sunny beach or on the ancient seafloor -- just the sort of place where it is thought that early life liked to hang out.  However, if fossils can be found in volcanic rock as well, then this vastly increases the number of potential discoveries that could be made of ancient life, especially since in some parts of the world as much as 60 percent of the Archaean rocks are of volcanic origin.

“The idea of hydrothermal vents as the cradle of life has been around for some time, but when considering volcanic lavas most people thought these were too hot and uninhabitable” says McLoughlin.  “Traditionally trace fossils have been found in muds and sediments, and so we’re now opening up a new field of looking for trace fossils in volcanic environments.”

Barbeton fieldwork

A cliff containing Archean pillow lavas, in the Barberton Greenstone belt of South Africa.  Credit: Nicola McLoughlin.

McLoughlin and her colleagues are continuing work on structures found in volcanic glasses, trying to understand where and how they are distributed in the earliest seafloor. They are also trying to refine the dates on some of the earliest examples, and to better understand precisely how they formed. "We are hoping to see more clearly through this glassy window into the early Earth," says McLoughlin.

By Leslie Mullen