Not Science Fiction: Methane-Eating “Borgs” Have Been Assimilating Earth’s Microbes

Borg Illustration

A digital illustration inspired by methane-eating archaea and the Borgs that assimilate them. Credit: Jenny Nuss/Berkeley Lab

A newly discovered type of transferable DNA structure with a sci-fi name appears to play a role in balancing atmospheric methane.

In Star Trek, the Borg are a ruthless, hive-minded collective that assimilate other beings with the intent of taking over the galaxy. Here on nonfictional planet Earth, Borgs are DNA packages that could help humans fight climate change.

Last year, a team of scientists discovered DNA structures within a methane-consuming microbe called Methanoperedens that appear to supercharge the organism’s metabolic rate. They named the genetic elements “Borgs” because the DNA within them contains genes assimilated from many organisms. In a study published on October 19 in the journal Nature, the researchers, who were led by Jill Banfield, describe the curious collection of genes within Borgs. They also begin to investigate the role these DNA packages play in environmental processes, such as carbon cycling.

“Imagine a single cell that has the ability to consume methane. Now you add genetic elements within that cell that can consume methane in parallel and also add genetic elements that give the cell higher capacity. It basically creates a condition for methane consumption on steroids, if you will.” — Kenneth Williams

First contact

Methanoperedens are a type of archaea (unicellular organisms that resemble bacteria but represent a distinct branch of life) that break down methane (CH4) in soils, groundwater, and the atmosphere to support cellular metabolism. Although Methanoperedens and other methane-consuming microbes live in diverse ecosystems around the world, they are believed to be less common than microbes that use photosynthesis, oxygen, or fermentation for energy. However, they play an outsized role in Earth system processes by removing methane – the most potent greenhouse gas – from the atmosphere. Methane traps 30 times more heat than carbon dioxide and is estimated to account for about 30 percent of human-driven global warming. The gas is emitted naturally through geological processes and by methane-generating archaea; however, industrial processes are releasing stored methane back into the atmosphere in worrying quantities.

Banfield is a faculty scientist at Lawrence Berkeley National Laboratory (Berkeley Lab) and professor of Earth & Planetary Science and Environmental Science, Policy & Management at the University of California, Berkeley (UC Berkeley). She studies how microbial activities shape large-scale environmental processes and how, in turn, environmental fluctuations alter the planet’s microbiomes. As part of this work, she and her colleagues regularly sample microbes in different habitats to see what interesting genes microbes are using for survival, and how these genes might affect global cycles of key elements, such as carbon, nitrogen, and sulfur. The team looks at the genomes within cells as well as the portable packets of DNA known as extra-chromosomal elements (ECEs) that transfer genes between bacteria, archaea, and viruses. These elements allow microbes to quickly gain beneficial genes from their neighbors, including those that are only distantly related.

Jill Banfield and Kenneth Williams

Jill Banfield and Kenneth Williams collect a sample of water from the East River in Colorado to study the ecosystem’s microbial life. Credit: Roy Kaltschmidt/Berkeley Lab

The scientists discovered evidence of an entirely new type of ECE while studying Methanoperedens sampled from seasonal wetland pool soil in California. Unlike the circular strands of DNA that make up most plasmids, the most well-known type of extra-chromosomal element, the new ECEs are linear and very long – up to one-third the length of the entire Methanoperedens genome. After analyzing additional samples from underground soil, aquifers, and riverbeds in California and Colorado that contain methane-consuming archaea, the researchers uncovered a total of 19 distinct ECEs they dubbed Borgs. Using advanced genome analysis tools, the team determined that many of the sequences within the Borgs are similar to the methane-metabolizing genes within the actual Methanoperedens genome. Some of the Borgs even encode all the necessary cellular machinery to eat methane on their own, so long as they are inside a cell that can express the genes.

“Imagine a single cell that has the ability to consume methane. Now you add genetic elements within that cell that can consume methane in parallel and also add genetic elements that give the cell higher capacity. It basically creates a condition for methane consumption on steroids, if you will,” explained co-author Kenneth Williams, a senior scientist and Banfield’s colleague in Berkeley Lab’s Earth and Environmental Sciences Area. Williams led research at the Rifle, Colorado site where the best characterized Borg was recovered, and is also chief field scientist of a research site on the East River, near Crested Butte, Colorado, where some of Banfield’s current sampling takes place.

The East River field site is part of the Department of Energy’s Watershed Function Scientific Focus Area, a multidisciplinary research project led by Berkeley Lab that aims to link microbiology and biochemistry with hydrology and climate science. “Our expertise is bringing together what are often thought of and treated as completely disparate fields of inquiry – big science that links everything from genes all the way up to watershed and atmospheric processes.”

Resistance is futile a disadvantage

Banfield and her fellow researchers at UC Berkeley’s Innovative Genomics Institute, including co-author and longtime collaborator Jennifer Doudna, hypothesize that the Borgs could be residual fragments of entire microbes that were engulfed by Methanoperedens to aid metabolism, similar to how plant cells harnessed formerly free-living photosynthetic microbes to gain what we now call chloroplasts, and how an ancient eukaryotic cell consumed the ancestors of today’s mitochondria. Based on the similarities in sequences, the engulfed cell could have been a relative of Methanoperedens, but the overall diversity of genes found in the Borgs indicates that these DNA packages were assimilated from a wide range of organisms.

No matter the origin, it is clear that Borgs have existed alongside these archaea, shuttling genes back and forth, for a very long time.

Notably, some Methanoperedens were found with no Borgs. And, in addition to recognizable genes, the Borgs also contain unique genes encoding other metabolic proteins, membrane proteins, and extracellular proteins almost certainly involved in electron conduction required for energy generation, as well as other proteins that have unknown effects on their hosts. Until the scientists can culture Methanoperedens in a laboratory environment, they won’t know for sure what capabilities the different Borgs confer, why some microbes use them, and why others don’t.

One likely explanation is that Borgs act as a storage locker for metabolic genes that are only needed at certain times. Ongoing methane monitoring research has shown that methane concentrations can vary significantly throughout the year, usually peaking in the fall and dropping to the lowest levels in early spring. The Borgs therefore provide a competitive advantage to methane-eating microbes like Methanoperedens during periods of abundance when there is more methane than their native cellular machinery can break down.

Plasmids are known to serve a similar purpose, quickly spreading genes for resistance to toxic molecules (like heavy metals and antibiotics) when the toxins are present in high enough concentrations to exert evolutionary pressure.

“There is evidence that different types of Borgs sometimes coexist in the same host Methanopreredens cell.  This opens the possibility that Borgs could be spreading genes across lineages,” said Banfield.

Boldly exploring the (microbial) universe

Since posting their article as a pre-print last year, the team has begun follow-up work to better understand how Borgs may affect biological and geological processes. Some researchers are combing through data sets of genetic material from other microorganisms, looking for evidence that Borgs exist in association with other species.

While her colleagues are using lab-based methods, co-author Susan Mullen, a graduate student in Banfield’s lab, will be getting her feet wet with some very picturesque field work. She recently started a project to sample microbes from the floodplains of the East River throughout the year to assess how seasonal changes in Borg abundance and other microbes known to be involved in methane cycling correlate to seasonal fluxes of methane.

According to the authors, years down the line, carefully cultured microbes chock full of Borgs could be used to reduce methane and curb global warming. It’s all to benefit the collective – life on Earth.

Reference: “Borgs are giant genetic elements with potential to expand metabolic capacity” by Basem Al-Shayeb, Marie C. Schoelmerich, Jacob West-Roberts, Luis E. Valentin-Alvarado, Rohan Sachdeva, Susan Mullen, Alexander Crits-Christoph, Michael J. Wilkins, Kenneth H. Williams, Jennifer A. Doudna and Jillian F. Banfield, 19 October 2022, Nature.
DOI: 10.1038/s41586-022-05256-1

7 Comments on "Not Science Fiction: Methane-Eating “Borgs” Have Been Assimilating Earth’s Microbes"

  1. I’m pretty sure Borg is the plural form of Borg? “We are the Borgs, resistance is futile” said no Borg ever.
    Unless it’s like fishes and if there are multiple species of Borg we refer to them as Borgs, but it sure looks wrong in your headline.

  2. What are the waste products?

  3. “Methane traps 30 times more heat than carbon dioxide”

    It’s actually more around 80 times based on the most recent (and more refined) IPCC AR6 Global Warming Potentials (GWPs) for a 20-year reference.

    30 (more precisely 28) is the GWP for a 100-year reference but since the lifetime of methane in the atmosphere is about 10-15 years, it doesn’t make sense to use the 100-year reference. That is exactly why now most scientists are saying that it’s more critical to focus on methane (CH4) than on carbon dioxide (CO2).

    We spent too much time focusing on the “far future” (100 years) while doing next to nothing and we’re now stuck with the immediacy of the climate crisis (more like a 20-year period max.)

  4. What if we need methane to stay warm during the winter months.

  5. The T …just start storing your farts in a bottle.

  6. Stupid name from stupid researcher who are still living in their fifth grade fantasy land.

  7. Thomas A Marano | October 29, 2022 at 3:26 am | Reply

    How would they deploy them in the Atmosphere? Need to do it soon!

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