Up to 4 percent of the methane on Earth comes from
the ocean's oxygen-rich waters, but scientists have been unable to
identify the source of this potent greenhouse gas. Now researchers
report that they have found the culprit: a bit of "weird chemistry"
practiced by the most abundant microbes on the planet.
The findings appear in the journal Science.
The researchers who made the discovery did not set out to explain
ocean geochemistry. They were searching for new antibiotics. Their
research, funded by the National Institutes of Health, explores an
unusual class of potential antibiotic agents, called phosphonates,
already in use in agriculture and medicine.
Many microbes produce phosphonates to thwart their competitors.
Phosphonates mimic molecules the microbes use, but tend to be more
resistant to enzymatic breakdown. The secret of their success is the
durability of their
carbon-phosphorus bond.
"We're looking at all kinds of antibiotics that have this
carbon-phosphorus bond," said University of Illinois microbiology and
Institute for Genomic Biology (IGB) professor William Metcalf, who led the study with chemistry and IGB professor Wilfred van der Donk.
"So we found genes in a microbe that we thought would make an
antibiotic. They didn't. They made something different altogether."
The microbe was Nitrosopumilus maritimus, one of the most
abundant organisms on the planet and a resident of the oxygen-rich
regions of the open ocean. When scanning microbial genomes for promising
leads, Benjamin Griffin, a postdoctoral researcher in Metcalf's lab,
noticed that N. maritimus had a gene for an enzyme that resembled
other enzymes involved in phosphonate biosynthesis. He saw that the
microbe also contained genes to make a molecule, called HEP, which is an
intermediate in phosphonate biosynthesis.
To determine whether N. maritimus was actually producing a
desirable phosphonate antibiotic, chemistry postdoctoral researcher
Robert Cicchillo cloned the gene for the mysterious enzyme, expressed it
in a bacterium (E. coli), and ramped up production of the
enzyme. When the researchers added HEP to the enzyme, the chemical
reaction that ensued produced a long sought-after compound, one that
could explain the origin of methane in the aerobic ocean.
Scientists had been searching for this compound, methylphosphonic
acid, since 2008, when David Karl at the University of Hawaii, Edward
DeLong at MIT and their colleagues published
an elegant – yet unproven – hypothesis to explain how methane was
arising in the aerobic ocean. The only microbes known to produce methane
are anaerobes, unable to tolerate oxygen. And yet the aerobic ocean is
saturated with methane.
To explain this "methane paradox," Karl and DeLong noted that many
aerobic marine microbes host an enzyme that can cleave the
carbon-phosphorus bond. If that bond were embedded in a molecule with a
single carbon atom, methylphosphonic acid, one of the byproducts of this
cleavage would be methane. Karl and DeLong even showed that incubation
of seawater microbes with methylphosphonic acid led to methane
production.
"There was just one problem with this theory," van der Donk said.
"Methylphosphonic acid has never been detected in marine ecosystems. And
based on known chemical pathways, it was difficult to see how this
compound could be made without invoking unusual biochemistry."
Van der Donk's lab conducted further experiments that demonstrated that the N. maritimus was actually synthesizing phosphonic acids.
"The chemical analysis was a Herculean effort," Metcalf said. The
microbe is "one-tenth the size of the standard lab rat microbe, E. coli, and grows at much lower cell densities," he said. The team relied on N. maritimus discoverer David Stahl, of the University of Washington, to grow the microbe in culture for their analysis.
"So we grew 100 liters of culture to get a few, maybe 50 or 100
milligrams of cells, of which maybe 1 percent is phosphorus, of which
maybe 5 percent is methylphosphonate," Metcalf said.
The experiments indicated that the methylphosphonate was bound to
another molecule, likely a sugar attached to the microbe's surface, van
der Donk said. When N. maritimus dies, other marine microbes
break the carbon-phosphorus bond of the methylphosphonate to gobble up
the phosphorus, an element that is rare in the oceans but essential to
life. This encounter generates methane.
The biochemistry that allows N. maritimus to produce methylphosphonate is "unprecedented," Metcalf said.
"Organisms that make phosphonates tend to use weird chemistry for
all kinds of things," van der Donk said. "But this is very unusual. One
of the carbon atoms of the HEP is oxidized by four electrons and the
other is turned into a methyl group. I'm not aware of any other cases
where that happens."
The new findings will help those modeling the geochemistry of the ocean to understand climate change, Metcalf said.
"We know that about 20 percent of the greenhouse effect comes
from methane and 4 percent of that comes from this previously
unexplained source," he said. "You have to know where the methane comes
from and where it goes to understand what will happen when the system
changes."
Contact: Diana Yates
diya@illinois.edu
217-333-5802
University of Illinois at Urbana-Champaign
