ALSO MORE EVIDENCE FOR ABIOGENIC OIL
The abiotic hypothesis is that the full suite of hydrocarbons found in petroleum can either be generated in the mantle by abiogenic processes, or by biological processing of those abiogenic hydrocarbons, and that the source-hydrocarbons of abiogenic origin can migrate out of the mantle into the crust until they escape ...
by Queen Mary, University of London
Photograph taken from ALVIN, a manned deep-ocean research submersible, taking sediment cores at the ocean floor of the Dorado Outcrop in 2014. Credit: Geoff Wheat, NSF OCE 1130146, and the National Deep Submergence Facility.
An international team of researchers led by Queen Mary University of London have discovered that microorganisms buried in sediment beneath the seafloor can survive on less energy than was previously known to support life. The study has implications for understanding the limit of life on Earth and the potential for life elsewhere.
An international team of researchers led by Queen Mary University of London have discovered that microorganisms buried in sediment beneath the seafloor can survive on less energy than was previously known to support life. The study has implications for understanding the limit of life on Earth and the potential for life elsewhere.
The study, published in the journal Science Advances, uses data from the sub-seafloor to construct innovative models that divide the oceans into hundreds of thousands of individual grid cells. A global picture of the sub-seafloor biosphere was then assembled, including key lifeforms and biogeochemical processes.
By combining data on the distribution and amounts of carbon and microbial life contained in Earth's deep biosphere with the rate of biological and chemical reactions, the researchers were able to determine the 'power' consumption of individual microbial cells—in other words—the rate at which they utilize energy. All life on Earth constantly uses energy in order to remain active, sustain metabolism, and carry out essential functions such as growth, and the repair and replacement of biomolecules.
The results show that sub-seafloor microbes survive using far less energy than has ever previously been shown to support any form of life on Earth. By stretching the habitable boundaries of life to encompass lower energy environments, the findings could inform future studies of where, when and how life arose on a hostile early Earth, and where life might be located elsewhere in the solar system.
By combining data on the distribution and amounts of carbon and microbial life contained in Earth's deep biosphere with the rate of biological and chemical reactions, the researchers were able to determine the 'power' consumption of individual microbial cells—in other words—the rate at which they utilize energy. All life on Earth constantly uses energy in order to remain active, sustain metabolism, and carry out essential functions such as growth, and the repair and replacement of biomolecules.
The results show that sub-seafloor microbes survive using far less energy than has ever previously been shown to support any form of life on Earth. By stretching the habitable boundaries of life to encompass lower energy environments, the findings could inform future studies of where, when and how life arose on a hostile early Earth, and where life might be located elsewhere in the solar system.
John Beck (Imaging Specialist, IODP-USIO/TAMU), Chad Broyles (Curator, IODP-USIO/TAMU), Zenon Mateo (Core Laboratory, IODP-USIO/TAMU) and Lisa Crowder (Assistant Laboratory Officer, IODP-USIO/TAMU) carry a sediment core on the catwalk. On site at the South Pacific Gyre, International Ocean Discovery Program Expedition 329. October 2010. Credit: Carlos Alvarez Zarikian (Expedition Project Manager/Staff Scientist, IODP-USIO/TAMU).
Dr. James Bradley, Lecturer in Environmental Science at Queen Mary said: "When we think about the nature of life on Earth, we tend to think about the plants, animals, microscopic algae, and bacteria that thrive on Earth's surface and within its oceans—constantly active, growing and reproducing. Yet here we show that an entire biosphere of microorganisms—as many cells as are contained in all of Earth's soils or oceans, have barely enough energy to survive. Many of them are simply existing in a mostly inactive state—not growing, not dividing, and not evolving. These microbes use less energy than we previously thought was possible to support life on Earth.
"The average human uses around 100 watts of power—meaning they burn approximately 100 joules of energy every second. This is roughly equivalent to the power of a ceiling fan, a sewing machine, or two standard lightbulbs . We calculate that the average microbe trapped in deep ocean sediments survives on fifty-billion-billion times less energy than a human."
Jan Amend, Director of the Center for Dark Energy Biosphere Investigations (C-DEBI) at the University of Southern California, and co-author of the study, said "Previous studies of life in the subseafloor—and there have been many good ones—focused predominantly on who's there, and how much of it is there. Now we're digging deeper into ecological questions: what is it doing, and how fast is it doing it? Understanding the power limits of life establishes an essential baseline for microbial life on Earth and elsewhere."
The findings raise fundamental questions about our definitions of what constitutes life, as well as the limits of life on Earth, and elsewhere. With such little energy available, it is unlikely that organisms are able to reproduce or divide, but instead use this miniscule amount of energy for 'maintenance' - replacing or repairing their damaged parts. It is likely, therefore, that many of the microbes found at great depths beneath the seafloor are remnants from populations that inhabited shallow coastal settings thousands to millions of years ago. Unlike organisms on the surface of Earth, which operate on short (daily and seasonal) timescales according to the Sun, it is likely that these deeply buried microbes exist on much longer timescales, such as the movement of tectonic plates, and changes in ocean oxygen levels and circulation.
Dr. James Bradley, Lecturer in Environmental Science at Queen Mary said: "When we think about the nature of life on Earth, we tend to think about the plants, animals, microscopic algae, and bacteria that thrive on Earth's surface and within its oceans—constantly active, growing and reproducing. Yet here we show that an entire biosphere of microorganisms—as many cells as are contained in all of Earth's soils or oceans, have barely enough energy to survive. Many of them are simply existing in a mostly inactive state—not growing, not dividing, and not evolving. These microbes use less energy than we previously thought was possible to support life on Earth.
"The average human uses around 100 watts of power—meaning they burn approximately 100 joules of energy every second. This is roughly equivalent to the power of a ceiling fan, a sewing machine, or two standard lightbulbs . We calculate that the average microbe trapped in deep ocean sediments survives on fifty-billion-billion times less energy than a human."
Jan Amend, Director of the Center for Dark Energy Biosphere Investigations (C-DEBI) at the University of Southern California, and co-author of the study, said "Previous studies of life in the subseafloor—and there have been many good ones—focused predominantly on who's there, and how much of it is there. Now we're digging deeper into ecological questions: what is it doing, and how fast is it doing it? Understanding the power limits of life establishes an essential baseline for microbial life on Earth and elsewhere."
The findings raise fundamental questions about our definitions of what constitutes life, as well as the limits of life on Earth, and elsewhere. With such little energy available, it is unlikely that organisms are able to reproduce or divide, but instead use this miniscule amount of energy for 'maintenance' - replacing or repairing their damaged parts. It is likely, therefore, that many of the microbes found at great depths beneath the seafloor are remnants from populations that inhabited shallow coastal settings thousands to millions of years ago. Unlike organisms on the surface of Earth, which operate on short (daily and seasonal) timescales according to the Sun, it is likely that these deeply buried microbes exist on much longer timescales, such as the movement of tectonic plates, and changes in ocean oxygen levels and circulation.
Photograph taken from ALVIN, a manned deep-ocean research submersible, taking sediment cores at the ocean floor of the Dorado Outcrop in 2014. Credit: Geoff Wheat
The research also sheds light on how the microbes interact with chemical processes occurring deep below the seafloor. Whilst oxygen provides the highest amount of energy to microbes, it is in overwhelmingly short supply—present in less than 3 per cent of sediments.
Anoxic sediments, however, are far more widespread, often containing microorganisms that obtain energy by generating methane—a potent greenhouse gas. Despite being practically inactive, the microbial cells contained in Earth's marine sediments are so numerous, and survive over such extraordinarily long timescales, that they act as an important driver of earth's carbon and nutrient cycles—even affecting the concentration of CO2 in earth's atmosphere over thousands to millions of years.
"The findings of the research call into question not just the nature and limits of life on Earth, but elsewhere in the Universe," added Dr. Bradley. "If life does exist on Mars or Europa for example, it would most likely take refuge in the subsurface of these energy-limited planetary bodies. If microbes only need a few zeptowatts of power to survive, there could be remnants of extant life, long dormant but still technically 'alive', beneath their icy surface."
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The research also sheds light on how the microbes interact with chemical processes occurring deep below the seafloor. Whilst oxygen provides the highest amount of energy to microbes, it is in overwhelmingly short supply—present in less than 3 per cent of sediments.
Anoxic sediments, however, are far more widespread, often containing microorganisms that obtain energy by generating methane—a potent greenhouse gas. Despite being practically inactive, the microbial cells contained in Earth's marine sediments are so numerous, and survive over such extraordinarily long timescales, that they act as an important driver of earth's carbon and nutrient cycles—even affecting the concentration of CO2 in earth's atmosphere over thousands to millions of years.
"The findings of the research call into question not just the nature and limits of life on Earth, but elsewhere in the Universe," added Dr. Bradley. "If life does exist on Mars or Europa for example, it would most likely take refuge in the subsurface of these energy-limited planetary bodies. If microbes only need a few zeptowatts of power to survive, there could be remnants of extant life, long dormant but still technically 'alive', beneath their icy surface."
Explore further
More information: "Widespread energy limitation to life in global subseafloor sediments" Science Advances (2020). advances.sciencemag.org/lookup … .1126/sciadv.aba0697
Journal information: Science Advances
Provided by Queen Mary, University of London
Journal information: Science Advances
Provided by Queen Mary, University of London
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