Fossilized microbes have provided scientists many clues about origins of life. By comparison, little attention is given to viruses in the fossil record. Although technically non-living, there is no question these tiny packets of protein-sheathed DNA have shaped the evolution of most life on earth, including humans. But can viral particles, a fractional size of even the smallest bacteria, actually become fossils? A study recently published in the journal Geobiology argues they can. Here, scientists present the first experimental evidence of silicification– the encasement in silicate minerals- of viruses living in hot spring biofilms. Moreover, these viruses can become fossils while still inside their host cells.
Before we get into viral fossilization, let’s back up for a minute and briefly review what a virus is. Viruses are simple beings that strip the notion of life down to a single, fundamental purpose: propagation of genetic code. While sharing this feature with all life on Earth, viruses are not considered living because they lack the means to carry out genetic reproduction on their own. Instead, viruses propagate by injecting their genetic material into a host cell. One inside a host, a virus uses one of two strategies, or “life cycles”, to reproduce. In the lysogenic cycle, viral DNA integrates with host DNA, lying low and allowing itself to be replicated along with the oblivious host cell. In our own chromosomes, many introns, or non-coding pieces of “junk DNA”, are thought to be ancient viral particles that “went to sleep” inside our cells and never woke up. In the more active (and deadly) lytic cycle, the virus co-opts the host cell’s replication machinery, creating a virus factory that eventually spews forth thousands of baby viruses which proceed to infect other cells.
Which of these cycles a virus chooses depends a lot on the external environment. If conditions are good in the host cell, it may be advantageous to hunker down and stay put. If, on the other hand, the host cell is already sick or dying, the virus may prefer to replicate as much as possible before abandoning ship.
Hot springs host communities of highly specialized extremeophiles. These bugs are not only hyperthermophilic, or super heat-tolerating, but often cope with extremely acid or alkali conditions. One way they do so is by modifying the pH within their cells, making it closer to neutral. Perhaps unsurprisingly, most hot spring viruses follow a lysogenic cycle, enjoying the less-extreme environment offered by their host.
It was in one such strange habitat, the Gumingquan hot spring in the Yunnan province of southern China, that Dr. Brian Jones and colleagues decided to investigate viral silicification. Why study fossilization in a geothermal hot spring? Geothermal waters, heated by subsurface magma from the Earth’s mantle, are often rich in silica and other minerals, such as calcium and iron, that promote fossilization. Moreover, thick, diverse biofilms hosting “virus-like” particles are known to inhabit the Gumingquan hot spring.
For their study, the researchers collected samples of these biofilms and brought them back to the lab. From biofilms containing many different Bacteria and Archaea, the scientists isolated Geobacillus lituanicus, a thermophilic, aerobic (oxygen-breathing) bacteria belonging to the phylum Firmicutes. They also isolated viral particles by liquifying samples of biofilm, separating out and removing all cells, and filtering the remaining liquid through a 0.22 µm filter- large enough to include viruses but small enough to remove most other microbial debris. Spherical, “virus-like” particles were further isolated and purified by infecting G.lituanicus cells with “viral extract”, and growing the infected cells on agar.
Once the researchers had purified both a host and virus-like particles, they set up a rather clever experiment to test for viral fossilization. They concocted a growth media for G. lituanicus containing sodium metasilicate, a silica-rich mineral. After adding G.lituanicus cells and virus-like particles to this media, they incubated the mixture for 22 days. At regular intervals, the scientists took samples and used transmission electron microscopy (TEM) to search for silicified viruses.
Using TEM, the scientists found numerous silica nanoparticles both inside and outside G. lituanicus cells. These circular particles consist of a core roughly 35-60 nanometers (nm) in diameter, surrounded by an outer shell approximately 30 nm thick. While these particles may just be small, silicified fragments of cellular detritus, there is good reason to think many of them are fossil viruses. For one, the fossil “cores” are similar in size and shape to the spherical virus-like particles used in the experiment. The silica nanoparticles had a “near normal”, or bell-curve, size distribution, another hallmark of biology. Finally, some of the silica nanoparticles had tails.
A few of you might be scratching your heads at this point, thinking something seems amiss. Remember, I told you most hot spring viruses are lysogenic (integrated into host DNA) most of the time. But in order for a virus to fossilize, it must have its own, independent structure. In other words, it must be lytic.
Does the discovery of fossil viruses within host cells negate the idea that hot spring viruses are typically dormant? Not necessarily. Actually, it may offer an explanation for when and why viral dormancy occurs. You see, all cells eventually die due to accumulated environmental stress. When a hot spring bacteria like G. lituanicus dies, its cell wall breaks open, causing hot, mineral-rich geothermal fluids to rush in. Suddenly, any viruses inside are exposed to all sorts of elements- heat, acid, etc.- they can’t necessarily tolerate. By precipitating a silica shell, these viruses may be able to survive long enough to find a new host.
Some of the proteins on a virus’s outer surface contain chemically-reactive molecules, such as carboxyl groups, that may aid in silica encrustation. The host cell itself may inadventently promote viral fossilization. Many alkaliphiles, like those in the alkaline Gumingquan waters, maintain their cellular pH at two or more units lower than the external environment. Geothermal waters that are undersaturated with silica at pH 12 may become supersaturated at pH 9 or 10, causing silicates to precipitate out as solids.
The strong evidence for viral silicification presented in this experiment suggests viruses may be preserved in the fossil record, particularly in rocks associated with alkaline geothermal systems. Some of the features of virus-like fossils noted in this study- distinct cores and shells, fossil “tails”, a concentration of fossil-like particles inside a host cell- may be useful for identifying the footprints of ancient viruses in the wild.
Peng, X., Xu, H., Jones, B., Chen, S., & Zhou, H. (2013). Silicified virus-like nanoparticles in an extreme thermal environment: implications for the preservation of viruses in the geological record Geobiology DOI: 10.1111/gbi.12052