Aeonophiles
by Karen G. Lloyd
The sediments underlying the world's oceans contain about a third of the total number of microbial cells on the planet. This is a vast biosphere, mostly comprised of deep branches on the tree of life that no one has yet figured out how to grow in a laboratory. Since growing microbes in a laboratory is the best way we can learn about them, this means that there's a lot of mystery about what makes this strange ecosystem tick. Probably the strangest thing about these ecosystems is that they are essentially cut off from both the surface world and subsurface sources of energy for chemosynthesis, like in hydrothermal vents. Yes, there are plenty of vents scattered around the seafloor, and other good sources of energy like methane cold seeps and volcanic eruptions, but I'm not talking about those places. I'm talking about the great, boring expanses of sedentary muck whose most notable feature is that nothing ever happens. This means that one of the largest microbial ecosystems on the planet gets no fresh food deliveries for millions of years. Every living being that we commonly interact with, including pretty much all our laboratory cultures, would die if you didn't feed them for that long.
So, why is there a highly diverse, metabolically active biosphere hanging out where no one can eat? Roberto Kolter, and his former lab members Steve Finkel, Erik Zinser and others, showed us that even common bacteria actually have a surprising tolerance to starvation. Even E. coli, which can't shut down into metabolically inactive spores continues with subpopulations growing, dying, and competing with each other long after you remove the food. After starving for months or even years, they become grizzled old tough guys who actually outcompete younger cells under starvation conditions. Roberto and his folks called this the Growth Advantage in Stationary Phase, which has about the most adorable acronym ever for a strain desperately fighting for life: GASP.
It's much harder to run an experiment for a thousand years (although I recently had the pleasure of seeing an experiment set up by Charles Cockell, at the University of Edinburgh, that will run for 500 years – someone else is going to have to write the blog post about that one). However, if we extrapolate from the experiments run by nature underneath our oceans all over the world, the most reasonable conclusion is that the bacteria, archaea, and possibly eukaryotes in these marine sediment ecosystems have somehow adapted to have cells that survive the whole lengthy process of burial. This means these microbes might be evolutionarily adapted to live for hundreds of thousands of years. I'm not talking about the age of their lineage. I'm talking about THE ACTUAL CELLS being that old.

The ultra-long-lived aeonophiles! Source.
It recently occurred to my colleague Drew Steen and I that we need a word to describe organisms that have adapted to live for a million (I mean, maybe?) years, especially since the fact that their lifespans are this long has to remain a hypothesis, so we need to be able to talk about them as we test it. We came up with aeonophiles. It means that they love long time periods. It seems hard to pronounce, but it's ee-ohn-oh-files. Like someone who loves wine, but with an extra syllable. I don't know for certain that cells can actually achieve this feat of living for a million years, while slowly replacing broken bits but never dividing. But currently, all evidence suggests this is a reasonable hypothesis. Now that they have a name, I'm hoping people will go forth and study these little weirdos!

Karen G. Lloyd is the Wrigley Professor of Earth Sciences, and Marine and Environmental Biology at the University of Southern California. She discovers strange types of microbial life deeply-buried inside Earth's crust, and wrote Intraterrestrials: Discovering the Strangest Life on Earth, long-listed for the PEN EO Wilson Literary Award.
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