Behind the iron curtain: How methane-making microbes kept the early Earth warm

April 17, 2017, Georgia Institute of Technology
Tiny incubators were used to simulate early Earth conditions, tracking microbial diversity and methane emissions over a period of 500 days. Credit: Rob Felt, Georgia Tech

For much of its first two billion years, Earth was a very different place: oxygen was scarce, microbial life ruled, and the sun was significantly dimmer than it is today. Yet the rock record shows that vast seas covered much of the early Earth under the faint young sun.

Scientists have long debated what kept those seas from freezing. A popular theory is that potent gases such as methane—with many times more warming power than carbon dioxide—created a thicker greenhouse atmosphere than required to keep water liquid today.

In the absence of oxygen, built up in ancient oceans. Under the right chemical and biological processes, this iron rusted out of seawater and cycled many times through a complex loop, or "ferrous wheel." Some microbes could "breathe" this rust in order to outcompete others, such as those that made methane. When rust was plentiful, an "iron curtain" may have suppressed methane emissions.

"The ancestors of modern methane-making and rust-breathing microbes may have long battled for dominance in habitats largely governed by iron chemistry," said Marcus Bray, a biology Ph.D. candidate in the laboratory of Jennifer Glass, assistant professor in the Georgia Institute of Technology's School of Earth and Atmospheric Sciences and principal investigator of the study funded by NASA's Exobiology and Evolutionary Biology Program. The research was reported in the journal Geobiology on April 17, 2017.

Marcus Bray (left), a biology Ph.D. candidate and Jennifer Glass, assistant professor in the Georgia Institute of Technology's School of Earth and Atmospheric Sciences, are shown in the laboratory where tiny incubators simulated early Earth conditions. Credit: Rob Felt, Georgia Tech

Using mud pulled from the bottom of a tropical lake, researchers at Georgia Tech gained a new grasp of how ancient microbes made methane despite this "iron curtain."

Collaborator Sean Crowe, an assistant professor at the University of British Columbia, collected mud from the depths of Indonesia's Lake Matano, an anoxic iron-rich ecosystem that uniquely mimics early oceans. Bray placed the mud into tiny incubators simulating early Earth conditions, and tracked microbial diversity and over a period of 500 days. Minimal methane was formed when rust was added; without rust, microbes kept making methane through multiple dilutions.

Extrapolating these findings to the past, the team concluded that could have persisted in rust-free patches of ancient seas. Unlike the situation in today's well-aerated oceans, where most natural gas produced on the seafloor is consumed before it can reach the surface, most of this ancient would have escaped to the atmosphere to trap heat from the early sun.

Explore further: A rusty green early ocean? Lab recreates one mechanism by which today's ore deposits originally formed

More information: M. S. Bray et al, Shifting microbial communities sustain multiyear iron reduction and methanogenesis in ferruginous sediment incubations, Geobiology (2017). DOI: 10.1111/gbi.12239

Related Stories

Probing the depths of the methane world

May 2, 2014

In 2011, Jennifer Glass joined a scientific cruise to study a methane seep off of Oregon's coast. In these cold, dark depths, microbes buried in the sediment feast on methane that seeps through the seafloor.

Bursts of methane may have warmed early Mars

January 24, 2017

The presence of water on ancient Mars is a paradox. There's plenty of geographical evidence that rivers periodically flowed across the planet's surface. Yet in the time period when these waters are supposed to have run—three ...

Recommended for you

Arctic wintertime sea ice extent is among lowest on record

March 23, 2018

Sea ice in the Arctic grew to its annual maximum extent last week, and joined 2015, 2016 and 2017 as the four lowest maximum extents on record, according to scientists at the NASA-supported National Snow and Ice Data Center ...

Germany was covered by glaciers 450,000 years ago

March 23, 2018

The timing of the Middle Pleistocene glacial-interglacial cycles and the feedback mechanisms between climatic shifts and earth-surface processes are still poorly understood. This is largely due to the fact that chronological ...

Wood pellets: Renewable, but not carbon neutral

March 22, 2018

A return to firewood is bad for forests and the climate. So reports William Schlesinger, President Emeritus of the Cary Institute of Ecosystem Studies, in an Insights article published today in the journal Science.

The tradeoffs inherent in earthquake early warning systems

March 22, 2018

A team of researchers with the U.S. Geological Survey and the California Institute of Technology has found that modern earthquake early warning (EEW) systems require those interpreting their messages to take into consideration ...


Please sign in to add a comment. Registration is free, and takes less than a minute. Read more

Click here to reset your password.
Sign in to get notified via email when new comments are made.