MIT scientists kept growing ocean microbes that clung to test tubes; the sticky share rose from 6% to 85%, revealing a hidden way they release carbon into water
Prochlorococcus, a small but abundant marine microbe, was thought to exist mainly as solitary cells. New research findings reveal that it can form biofilms and attach to particles. This discovery has implications for understanding the biological c...

An AI-generated image of test tubes containing laboratory cultures of Prochlorococcus, a microscopic marine cyanobacterium, showing the greenish cellular deposits adhering to the inner glass walls. Image credits: ChatGPT
Small cell, big job
Prochlorococcus is the smallest and most abundant photosynthetic organism in our seas and is responsible for approximately 10% of the carbon taken from the atmosphere by land and oceans every year, per MIT News. According to NOAA’s National Ocean Service, around half of the world’s oxygen is produced by the ocean, mostly by plankton. Most of that ocean-produced oxygen, however, is consumed by marine life itself, and most of what we breathe comes from oxygen that has built up in the atmosphere over hundreds of millions of years. So, Prochlorococcus's real significance lies elsewhere: in carbon capture, not oxygen supply.

Same genome, different mood
You might assume there would have been a mutation to cause them to attach. However, after sequencing, there was no mutation found. Within a given strain, genetically identical cells can switch between being attached or free-floating, it's like having one wardrobe and two completely different outfits. (The exact proportions that switch do vary somewhat from strain to strain, but the switching itself happens without any underlying genetic difference.) Attached cells also had more chlorophyll and slower growth rates. But they released nearly double the dissolved organic carbon into the surrounding water, compared with free-floating cells. Some detached to create new free-floating populations.
Why carbon scientists are interested
The ocean has a biological pump to convert carbon dioxide into organic carbon in sunlit waters, as per the Woods Hole Oceanographic Institution. Much of this carbon sinks to form marine snow. If it can sink deep enough into the ocean, it won’t be mixed back into the atmosphere and can be taken out of circulation for up to thousands of years.

A big number with an asterisk
If Prochlorococcus can attach to sinking particles, this could result in around half a billion metric tons of carbon being transported to deeper waters every year. However, this is a very crude estimate based on how much Prochlorococcus is present at the surface, how much attaches to particles and how much is consumed, as Anjur-Dietrich mentions.
What’s still unanswered
The team is already looking to see how much of Prochlorococcus overall is particle-associated. Early experiments are looking into whether the attached cells help neighbouring cells and how this affects the rate at which particles degrade. The "loner" label, it turns out, doesn't tell the whole story; even a single species of microbe can hold more than one way of life.
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