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«Researchers establish long - sought source
of ocean methane: An abundant enzyme in marine microbes may be responsible for production of the greenhouse gas.»
Several years ago, van der Donk and University of Illinois colleague William Metcalf found a possible clue to the mystery
of ocean methane: They discovered a microbial enzyme that produces a compound called methylphosphonate, which can become methane when a phosphate molecule is cleaved from it.
Not exact matches
«Greenhouse gas emissions are going to go through the roof with a project
of this kind,» said Wilderness Committee National Campaign Director Joe Foy «From escaped
methane at the drill sites to the massive carbon emissions required to cool the gas, to more escaped
methane on the long trip across the
ocean to Asia and then the emissions from burning the gas.
I vaguely collect reading that there was a lot
of methane on the
ocean floor (as
methane clathrate), plus occasional pockets
of oil (through accumulation
of perished marine life).
There's enough vinyl cyanide (C2H3CN) in the moon's liquid
methane seas to make about 10 million cell - like balls per cubic centimeter
of ocean, researchers calculate.
Thus,
methane and carbon dioxide together, unaccompanied by carbon monoxide, on a rocky,
ocean - bearing world would best be interpreted as an airtight sign
of anoxic life.
The race is on to tap the world's biggest and most unusual fossil fuel supply —
methane trapped in frozen hydrates in permafrost and at the bottom
of the
ocean
In the process, they might identify a planet's surface features — such as
oceans, continents, ice caps and even cloudbanks — and detect the presence
of biomarkers like oxygen,
methane and water.
«Researchers build alien
ocean to test NASA outer space submarine: Working in a -300 F
ocean of methane and ethane has its challenges.»
The engineering is even trickier because, unlike the nearly homogeneous water in earth - based
oceans, the concentration
of ethane and
methane can vary dramatically in the Titan
oceans and change the liquid's density properties.
«Although most
of the macrophyte carbon is released back to the atmosphere in the same form that it is assimilated, carbon dioxide, some
of it is actually exported to the
ocean as dissolved carbon or released to the atmosphere as
methane, a gas that has a warming potential 20 times larger than carbon dioxide,» said John Melack, a professor at the University
of California, Santa Barbara.
Ryskin proposes that huge deposits
of methane and other gases, which are naturally produced in deep - sea waters, became trapped under the pressure
of a then - stagnant global
ocean.
Gas hydrates, icelike deposits
of methane locked away in permafrost and buried at the
ocean bottom, may pose a threat to our climate (see Discover, March 2004).
Through them we have learned
of lava plains on Venus, a buried
ocean on Jupiter's moon Europa, lakes
of methane on Saturn's moon Titan, and salty geysers on another Saturnian moon, Enceladus.
This is actually one
of the most active
methane seep sites that we have mapped in the Arctic
Ocean.
500m wide and 10m high, the
methane domes on the Arctic
Ocean floor are containing huge amounts
of methane.
Warmer
oceans are thawing
methane deposits, adding more
of the greenhouse gas to the atmosphere
A possible explanation is that the build - up
of methane below the
ocean floor creates bubbles.
The resulting outburst
of methane produced effects similar to those predicted by current models
of global climate change: a sudden, extreme rise in temperatures, combined with acidification
of the
oceans.
The Arctic
ocean floor hosts vast amounts
of methane trapped as hydrates, which are ice - like, solid mixtures
of gas and water.These hydrates are stable under high pressure and cold temperatures.
A crew
of a dozen sailors, a geophysics professor, and two graduate students, we were combing the
ocean floor for buried
methane hydrate, an ice - like form
of natural gas estimated to be more abundant than fossil fuels.
Gargantuan stores
of gas hydrates under the
oceans and permafrost regions
of the globe have many scientists wondering whether they can find an economically feasible way to unlock the
methane, creating a natural gas supply that could last for centuries.
The extensive
methane seep mounds across the remote arctic island
of Ellef Ringnes may be a caution from the past regarding potential impacts
of modern warming
of the Arctic
Ocean.
Because they form by leakage
of methane into seawater it implies that something at that time caused a large release
of methane into the
ocean.
Bowen says the two relatively rapid carbon releases (about 1,500 years each) are more consistent with warming
oceans or an undersea landslide triggering the melting
of frozen
methane on the seafloor and large emissions to the atmosphere, where it became carbon dioxide within decades.
Release
of methane hydrates has previously been suggested as a mechanism to drive runaway greenhouse events, as warming
oceans releases trapped
methane that causes further warming and releases more
methane.
Similar frozen
methane hydrates occur throughout the same arctic region as they did in the past, and warming
of the
ocean and release
of this
methane is
of key concern as
methane is 20x the impact
of CO2 as a greenhouse gas.
Even short - lived atmospheric greenhouse gases, like
methane, leave an imprint in the
oceans that can last centuries, according to a paper published in the Proceedings
of the National Academy
of Sciences in January.
Methane hydrates were later found in permafrost in the 1960s, and in the
oceans, commonly on the edges
of the continental shelves, but only at certain
ocean pressures and temperatures.
That may in turn have caused the planet to heat up enough to melt deposits
of methane frozen in sediments on the
ocean floor (something, incidentally, that could happen again), discharging even more potent greenhouse gases into the atmosphere and further heating the planet in an escalating feedback loop.
He wonders whether megaplumes carry the gases
of an eruption, such as carbon dioxide and
methane and helium 3, as well as minerals such as sulfur and iron, to upper layers
of the
ocean where most plant and animal life resides.
But in the case
of a big release
of undersea
methane, how much would escape the
ocean to exert its greenhouse effects?
Methane, the carbon - hydrogen compound that is the main component
of natural gas and cow flatulence, gets trapped inside crystalline cages
of frozen water in the muddy
ocean bottom.
For example, it says a sudden
methane release from the
ocean, or a slowdown
of the Gulf Stream, are «very unlikely» and that a collapse
of the West Antarctic or Greenland ice sheets during this century is «exceptionally unlikely.»
Finds like that, along with sediment cores and ice cores that show how the amount
of methane in the atmosphere and
ocean has fluctuated dramatically in the past, have led to a slew
of «
methane burp» theories.
Some geologists speculate that massive volcanic eruptions covering areas as large as modern continents triggered the release
of methane buried in the
ocean floor, causing a greenhouse effect.
Scientists excavating the
ocean floor have found huge chunks
of frozen
methane along Hydrate Ridge, about 60 miles off the coast
of Oregon.
Living organisms could use these oxidizing chemicals to burn fuels such as iron or
methane seeping up from the rocky bottom
of Europa's
ocean.
Already billions
of years ago, Methanosarcinales archaea might have abundantly thrived under the
methane - rich atmosphere in the ferruginous (iron holding) Archaean
oceans, 4 to 2.5 billion years ago.
A new study led by researcher Natalia Shakhova
of the University
of Alaska, Fairbanks, and the Russian Academy
of Sciences» Far Eastern Branch reports that
methane releases from one part
of the Arctic
Ocean are more than twice what scientists previously thought.
Until 2003, when Shakhova's team started studying this part
of the Arctic
Ocean, no one had measured how much
methane was being released from it.
In deeper parts
of the
ocean, the
methane released from the
ocean floor would likely never make it up to the atmosphere, since it would get used up by microbes before it reached the surface.
The microbial communities in these sediments include aggregates
of methane - oxidizing archaea called ANME (for ANaerobic MEthanotrophs) and sulfate - reducing bacteria (SRB) that live together symbiotically and help to remove some 80 percent
of the
methane released from
ocean sediments.
We suggest that a vigorous deepwater bacterial bloom respired nearly all the released
methane within this time, and that by analogy, large - scale releases
of methane from hydrate in the deep
ocean are likely to be met by a similarly rapid methanotrophic response.
The acetate is a product
of methane and hydrogen from the alkaline hydrothermal vents and carbon dioxide dissolved in the surrounding
ocean.
Our goal was to fingerprint the source
of methane in the Arctic
Ocean to determine if ancient
methane was being liberated from the seafloor and if it survives to be emitted to the atmosphere,» says Sparrow, who conducted the study, published in Science Advances, as part
of her doctoral research at the University
of Rochester.
With that in mind, environmental scientist Katy Sparrow»17 (PhD) set out to study the origin
of methane in the Arctic
Ocean.
In some parts
of the Arctic
Ocean, the shallow regions near continents may be one
of the settings where
methane hydrates are breaking down now due to warming processes over the past 15,000 years.
Trapped in
ocean sediments near continents lie ancient reservoirs
of methane called
methane hydrates.