(singular: archaeon) a group of tiny organisms often living in extreme environments, such
as ocean vents and salt lakes.
Not exact matches
They can be several tens of metres tall, and grow
as minerals are deposited when the hot water meets the cold
ocean water at the outlet of the hydrothermal
vents.
These
vents are known
as black smokers for the plumes of dark hydrogen sulfide they belch into the
ocean.
Bienhold and her team are helping to clarify how life travels around the
ocean, and how amazingly well - adapted niche creatures can actually use organic - rich oases like whale carcasses
as convenient stepping stones between
vents which are few and far between.
A study described here today at the American Geophysical Union's biennial
Ocean Sciences Meeting shows that RNA's chemical building blocks fall apart within days to years at temperatures near boiling — a finding that poses problems for some origin of life theories, especially ones picturing that life arose in scalding settings such
as deep - sea hydrothermal
vents.
However, a microbe collected from a
vent in what's known
as the Faulty Towers neighbourhood, 2400 metres down in the Pacific
Ocean, has upped the ante.
Each contained jumbles of DNA sequences collected from environments such
as soil, the
ocean, hydrothermal
vents, industrial effluent, and cow and baboon faeces.
Now, new research offers a potential solution: Longer RNA chains could have hidden out in porous rocks near volcanic sites such
as hydrothermal
ocean vents, where unique temperature conditions might have helped complex organisms evolve.
Earthly life has proved remarkably hardy in similar extreme environments such
as hydrothermal
vents on the
ocean floor and polar ice.
The other, which has gained popularity in recent years, is that deep - sea
vents at the bottom of the
ocean acted
as a cradle for life, offering both heat and nutrition via fluids pumped up through Earth's crust.
Although the evidence was subsequently contested, some single - celled microbial life lacking a nucleus that segregates their internal DNA or RNA («prokaryotes») from the surrounding cytoplasm may have flourished in darkness within cracks in Earth's seafloor crust and around deep, warm or boiling hot
ocean springs (hydrothermal or volcanic
vents, such
as at Lost City or at black smokers) without a need for light or free oxygen in the
oceans or atmosphere.
As tides raised by Jupiter in Europa's
ocean rise and fall, they may cause cracking, additional heating, and even
venting of water vapor into the airless sky above Europa's icy surface.
Hydrothermal
vents on the
ocean floor known
as «black smokers» may support undersea habitats on Europa,
as on Earth (more).
Many of the deepest branches in Woese's tree, those that join nearest to the three - way junction of the kingdoms, turned out to belong to organisms that live at high temperatures,
as in the fuming springs in Yellowstone Park or the volcanic
vents that gash the
ocean floor.
Scientists have discovered unusual hot water
vents at the bottom of the Atlantic
Ocean, such
as this stone chimney rising three stories above the sea floor.
In Earth's
oceans, that sort of heating shows up at sites known
as hydrothermal
vents.
Microorganisms dominate all other life everywhere scientists have looked, including the human body, the Earth's soils and sediments, the
oceans and fresh waterways, the atmosphere and even extreme environments such
as hydrothermal
vents and subglacial lakes.
It is also thought that hydrothermal
vents may regulate the chemistry of the global
oceans and could be responsible for the elemental composition of seawater
as a whole.
Trained
as an astrobiologist at Stanford and Caltech, Loretta has been to the Canadian Arctic to study plant life in extreme environments and to the hydrothermal
vents at the bottom of the
ocean with «Titanic» director James Cameron to film a 3D IMAX documentary, «Aliens of the Deep.»
You will recall that hydrothermal
vents are plumes of hot water that spew from rocks and cracks along the
ocean floor, especially in regions of sea - floor spreading, such
as oceanic ridges and rift valleys.
As if to seal the case, in early 2017, Cassini discovered silica grains and hydrogen gas in the ice plumes above Enceladus, indicating there must be hydrothermal
vents on the floor of the subsurface
ocean.
Water, salts, organics, and methane make their way from the hydrothermal
vents on the
ocean bottom to the surface through cracks in the icy crust, erupting
as geysers.
Methane bubbles are coming up from
ocean vents off the Washington and Oregon coast, and a new study identified warming
ocean temperatures one - third of a mile below the surface
as likely responsible.
For a long time people thought that
ocean pH was regulated ultimately by reactions between deep seawater and sediments, but
as Walt Allensworth February 5, 2015 at 3:08 pm, says there are so many black, and clear,
vents along the midocean ridges spewing acidic water, that these probably maintain
ocean pH instead.
Exploration of deep - sea hydrothermal
vents in other sectors of the Southern
Ocean, such
as the Pacific - Antarctic Ridge [16], are likely to reveal further chemosynthetic communities.
Further exploration of high - latitude ridges is critical for a full understanding of the global biogeography of
vent ecosystems, given the potential role of the Southern
Ocean as a gateway or a barrier between the major ocean ridges and back - arc ba
Ocean as a gateway or a barrier between the major
ocean ridges and back - arc ba
ocean ridges and back - arc basins.
-- Volcanoes and
vents emit less than 1 % of human emissions (even the Pinatubo eruption caused a dip in the CO2 increase,
as the cooling by the volcanic dust increased the absorption of the
oceans beyond the extra emissions.
However, the conditions predicted for the open
ocean may not reflect the future conditions in the coastal zone, where many of these organisms live (Hendriks et al. 2010a, b; Hofmann et al. 2011; Kelly and Hofmann 2012), and results derived from changes in pH in coastal ecosystems often include processes other than OA, such
as emissions from volcanic
vents, eutrophication, upwelling and long - term changes in the geological cycle of CO2, which commonly involve simultaneous changes in other key factors affecting the performance of calcifiers, thereby confounding the response expected from OA by anthropogenic CO2 alone.