Life Is Bubbling Up to Seafloor with Petroleum from Deep Below
The COVID-19 pandemic is a stark reminder that we move through a world shaped by unseen life. Bacteria, viruses, and other microscopic organisms regulate the Earth’s vital functions and resources, from the air we breathe to all our food and most of our energy sources.
An estimated one-third of the Earth’s microbes are literally hidden, buried in sediments deep below the ocean floor. Now, scientists have shown that these “deep biosphere” microbes aren’t staying put but are bubbling up to the ocean floor along with fluids from buried petroleum reservoirs.
These hitchhikers in petroleum seeps are diversifying the microbial community that thrives at the seafloor, impacting deep-sea processes, such as carbon cycling, that have global implications.
“This study confirms that petroleum seeps are a conduit for transporting life from the deep biosphere to the seafloor,” says co-author Emil Ruff, a scientist at the Marine Biological Laboratory (MBL), Woods Hole. The study, led by Anirban Chakraborty and Casey Hubert of the University of Calgary, is published this week in Proceedings of the National Academy of Sciences.
The team analyzed 172 seafloor sediment samples from the eastern Gulf of Mexico that had been collected as part of a 2011 survey for the oil industry. A fraction of these samples contained migrated gaseous hydrocarbons, the chief components of oil and gas.
These petroleum seeps on the ocean floor harbored distinct microbial communities featuring bacteria and archaea that are well-known inhabitants of deep biosphere sediments.Hydrocarbon seep in the southern Gulf of Mexico emitting a viscous petroleum, much like asphalt.
Most animals found at hydrocarbon seeps, such as mussels and crabs, depend directly or indirectly on microorganisms that can oxidize the petroleum compounds.
Credit: Center for Marine Environmental Sciences (MARUM), University of Bremen
“One of the strengths of this study is the large number of samples analyzed, allowing robust statistical inferences of the microbes present in the petroleum seeps,” Ruff says. Because the seafloor is so difficult to access, explorations of deep-sea ecosystems are often limited by the number and quality of samples.
The team used metagenomic approaches to determine what microbes were present in the sediment samples, and genome sequencing of particularly interesting organisms to indicate what their activity in the subsurface might be.
Contacts and sources: Diana Kenney, The Marine Biological Laboratory (MBL)
Publication: Hydrocarbon seepage in the deep seabed links subsurface and seafloor biospheres Anirban Chakraborty et al. PNAS first published April 30, 2020
http://dx.doi.org/10.1073/pnas.2002289117
Source: http://www.ineffableisland.com/2020/05/life-is-bubbling-up-to-seafloor-with.html
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Barry from Victoria
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Thomas Gold wrote an excellent book on the subject- The Deep Hot Biosphere. It’s one of those rare books worth reading more than once.
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Andy Rowlands
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Thomas Gold had some good ideas, and some not so good ideas. In the mid-80s he convinced the Swedish energy company Vattenfall to drill for gas in the Siljan Ring impact crater, but by the early 90s, the drilling had proven ‘inconclusive’ and was abandoned. There was a BBC Horizon programme in 1987 about him and the Siljan Ring project called ‘Energy From Outer Space’. I still have it on tape 🙂
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Ian Howarth
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By coincidence I have just received a copy of this book from amazon.
I have grave doubts on the current scientific consensus on the formation of
hydrocarbons in the earth.
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Andy Rowlands
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These seeps remind me of the very hot hydrothermal vents discovered in 1979 in the Pacific by the famous submersible Alvin, which were nicknamed ‘black smokers’. Samples of the discharges were taken and later found to be previously unknown ecosystems that exist without sunlight, and are based on chemosynthesis, which is the process whereby biological conversion of carbon-containing molecules (usually carbon dioxide or methane) and nutrients into organic matter by oxidation of inorganic compounds.
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