In the frigid surface waters of the Arctic Ocean, a single species of bacteria has been found to blur one of biology's oldest boundaries — the line between organisms that make their own food and those that consume it. Porticoccus arcticus, abundant enough to constitute nearly a tenth of local microbial communities, has evolved a pathway that couples sunlight harvesting with the breakdown of acetone to capture atmospheric carbon and weave it into its own body. Discovered through genomic and transcriptomic analysis aboard a Canadian research vessel, this metabolic innovation invites us to recons
Arctic bacteria use acetone and sunlight to fix CO2, revealing novel carbon cycle pathway
A bacterium that fixes carbon while breaking down acetone in sunlight
So this bacterium is doing something new with acetone and sunlight. What exactly is it doing that we didn't know about before?
It's fixing CO2—pulling carbon dioxide out of the water and building it into its own body—while it's simultaneously breaking down acetone and using sunlight for energy. The combination is what's novel. We knew bacteria could do each of these things separately, but this particular pathway, this acetone carboxylation coupled with light harvesting, hadn't been documented before.
How confident are we that this is actually happening in the cells, not just that the genes are present? The evidence is genomic and transcriptomic, right?
Right. They found the genes in the DNA, and they found those genes being actively expressed—the RNA was there—in Arctic water samples. That's strong evidence the pathway is operating, but you're right to push back. This is inference from genetic data, not a direct observation of the enzyme working in a test tube.
And this bacterium, P. arcticus, is actually common up there? It's not some rare oddity?
It shows up consistently in samples collected over multiple years, and in some cases it makes up 9 percent of the entire microbial community. For a single species in open ocean, that's significant. It suggests this metabolism is actually useful in Arctic conditions.
But we don't know why acetone specifically. Is acetone abundant in Arctic waters? Is it a byproduct of something else happening up there?
That's not addressed in the study. The source material doesn't explain where the acetone is coming from or how abundant it is. That's a real gap.
What does this mean for how we understand the carbon cycle in the Arctic?
It suggests there's a pathway for CO2 fixation we weren't accounting for. In nutrient-poor Arctic waters, if these bacteria can fix carbon while also harvesting light and degrading organic compounds, they might be playing a bigger role in carbon cycling than we realized.
But again, we're talking about one species in one region. We don't know if this is happening elsewhere, or how much carbon is actually moving through this pathway compared to other routes.
True. This is a discovery of a mechanism, not a quantification of its global importance. That work would come next.
El Pulso
- A foundational assumption in microbiology — that carbon fixation belongs either to sunlight-driven autotrophs or organic-matter-consuming heterotrophs — has been quietly overturned by a bacterium thriving beneath Arctic ice.
- Porticoccus arcticus doesn't merely carry the genes for acetone carboxylation and light-harvesting rhodopsins; metatranscriptomic data show these are among its most actively expressed genes, meaning this is a live, working survival strategy, not an evolutionary relic.
- The bacterium accounts for up to 9% of microbial life in Arctic surface waters — a striking dominance for a single species in an open ocean — suggesting its unusual metabolism confers a genuine competitive advantage in nutrient-starved conditions.
- Researchers now face urgent new questions: how widespread is this pathway, which other polar microbes may employ it, and how will a warming Arctic reshape the communities built around these metabolic innovations?
In the frigid surface waters of the Arctic Ocean, a single species of bacteria has been found to blur one of biology's oldest boundaries — the line between organisms that make their own food and those that consume it. Porticoccus arcticus, abundant enough to constitute nearly a tenth of local microbial communities, has evolved a pathway that couples sunlight harvesting with the breakdown of acetone to capture atmospheric carbon and weave it into its own body. Discovered through genomic and transcriptomic analysis aboard a Canadian research vessel, this metabolic innovation invites us to reconsider how life sustains itself at the edges of the habitable world — and how much of the carbon cycle remains unwritten.
In the cold surface waters of the Arctic Ocean, researchers have found a bacterium that quietly defies one of biology's long-held categories. Porticoccus arcticus is photoheterotrophic — it feeds on organic matter while also harvesting energy from sunlight — but it has gone a step further by evolving an acetone carboxylation pathway that allows it to fix inorganic carbon from the atmosphere while breaking down acetone. The result is a metabolic strategy that sits at the intersection of autotrophy and heterotrophy, a boundary scientists had not previously seen crossed in this way.
The discovery emerged from DNA sequencing of water samples collected along a latitudinal transect of the Arctic Ocean aboard the CCGS Louis S. St-Laurent, in collaboration with Fisheries and Oceans Canada and the Beaufort Gyre Exploration Program at Woods Hole Oceanographic Institution. Despite carrying a streamlined genome relative to its relatives, P. arcticus had preserved a complete acetone carboxylation pathway and had also acquired multiple genes for proteorhodopsin — light-harvesting proteins — likely through lateral gene transfer from unrelated organisms.
What made the finding especially striking was the bacterium's apparent commitment to this strategy. Metatranscriptomic analysis — a real-time snapshot of gene activity in Arctic waters — showed that the genes for acetone carboxylase and the rhodopsin proteins were among the most highly expressed in P. arcticus, indicating active deployment rather than dormant inheritance. Multiyear tracking of microbial populations using 16S rRNA markers confirmed the species is not a rare curiosity: it comprises up to 9 percent of microbial communities in Arctic surface waters, a substantial presence for any single species in the open ocean.
The ecological logic becomes clear in context. Arctic summers bring abundant sunlight but scarce organic nutrients. By simultaneously harvesting light energy and fixing atmospheric carbon through acetone degradation, P. arcticus may be able to build the molecules it needs to grow and reproduce more efficiently than competitors. As the Arctic warms and its microbial communities shift, understanding metabolic innovations like this one will be essential for predicting how the region's biology — and its role in the global carbon cycle — will evolve.
In the cold waters of the Arctic Ocean, researchers have identified a metabolic pathway that rewrites what we thought we knew about how bacteria fix carbon from the atmosphere. The discovery centers on a single bacterial species, Porticoccus arcticus, which appears to have evolved an unusual strategy: it breaks down acetone while simultaneously harvesting energy from sunlight, and in the process, it captures inorganic carbon and incorporates it into its own biomass.
Carboxylases—enzymes that catalyze the fixation of CO2—are foundational to life on Earth. They drive the global carbon cycle, converting atmospheric carbon into organic compounds that fuel ecosystems. Scientists have long understood these enzymes in two contexts: autotrophic organisms like plants and algae that use them to build themselves from scratch using only CO2 and sunlight, and heterotrophic organisms that use them to process organic compounds they consume. What makes the Arctic finding unusual is that P. arcticus appears to blur this boundary. The bacterium is photoheterotrophic, meaning it uses light as an energy source while also feeding on organic matter. But it has gone further: it has wired an acetone carboxylation pathway into its metabolism, allowing it to fix CO2 while degrading acetone—a small organic molecule—in the presence of light.
The evidence comes from genomic analysis of samples collected along a latitudinal transect of the Arctic Ocean aboard the CCGS Louis S. St-Laurent, a research vessel operated in collaboration with Fisheries and Oceans Canada and the Beaufort Gyre Exploration Program at Woods Hole Oceanographic Institution. When researchers sequenced the DNA from these Arctic waters, they found that P. arcticus had maintained a complete acetone carboxylation pathway despite having a streamlined genome compared to its relatives. The bacterium had also acquired multiple genes for proteorhodopsin—light-harvesting proteins—likely through lateral gene transfer, a process in which organisms acquire genetic material from other species rather than inheriting it vertically from ancestors.
What struck the researchers most was how active this pathway appeared to be. When they analyzed metatranscriptomes—essentially a snapshot of which genes were being actively expressed in the Arctic water column—the genes for acetone carboxylase and the rhodopsin proteins ranked among the most highly transcribed in P. arcticus. This suggested the bacterium was not merely carrying these genes as evolutionary baggage but actively deploying them as a core part of its survival strategy in the nutrient-poor surface waters of the Arctic.
The ecological significance became clear when researchers examined a multiyear time-series of 16S rRNA data, a standard genetic marker used to track microbial populations. P. arcticus sequences appeared consistently throughout the dataset, and in many cases they were abundant—comprising up to 9 percent of the microbial community in Arctic surface waters. This is a substantial fraction for a single bacterial species in an open ocean environment, suggesting that whatever metabolic advantage this acetone carboxylation pathway confers, it is conferring a real competitive edge in Arctic conditions.
The mechanism itself represents a novel metabolic module in the ocean. By coupling CO2 assimilation with proteorhodopsin-based photoheterotrophy, P. arcticus may be able to enhance its biosynthetic capacity—the ability to build the molecules it needs to grow and reproduce—in environments where nutrients are scarce and competition is fierce. In the Arctic, where sunlight is abundant during summer months but organic nutrients are limited, this dual strategy of harvesting light energy while simultaneously fixing atmospheric carbon could be a significant advantage.
The discovery opens new questions about how widespread this pathway might be, whether other Arctic bacteria employ similar strategies, and what role this previously unknown carbon fixation mechanism plays in the overall cycling of carbon through polar ocean ecosystems. As the Arctic continues to warm and its microbial communities shift in response to changing conditions, understanding these metabolic innovations becomes increasingly important for predicting how the region's biology will respond.
Citas Notables
This metabolic module may allow photoheterotrophic bacteria to enhance their biosynthetic capacity via CO2 assimilation— Study findings