In their work examining intergranular attack of alloys under
hydrothermal conditions, scientists from PNNL's ACMD Division Computational Mathematics group, Physical Sciences Division, and Energy and Environment Directorate developed a mathematical model that is directly comparable to experimental data in predicting how fast oxygen penetrates binary alloys and the resulting depletion of select elements in the materials that leads to failures.
' Undersea
hydrothermal conditions on Mars may have existed about 3.7 billion years ago; undersea
hydrothermal conditions on Earth at about that same time are a strong candidate for where and when life on Earth began.
The hydrothermal conditions of the experiments, which also mimic early Earth settings (a proximity to volcanic activity and impact craters), released a complex mixture of oxygen - rich compounds, the probable result of oxidative processes that occurred in the parent body.
Some impact simulations suggest that
these hydrothermal conditions could persist for perhaps thousands of years, making for potentially habitable conditions.
Not exact matches
Bacteria thrive virtually everywhere on Earth — from sub-zero temperatures to over 750 degrees F (in
hydrothermal vents at the bottom of the ocean), and in widely varying oxygen, pressure and nutrient
conditions.
Yet we know that life on Earth can thrive in extreme
conditions: from the Antarctic (where temperatures can drop to almost -90 °C) to
hydrothermal vents on the ocean floor (where temperatures can exceed 460 °C).
The technology,
hydrothermal liquefaction, mimics the geological
conditions Earth uses to create crude oil, using high pressure and temperature to achieve in minutes something that takes Mother Nature millions of years.
Europa has a global ocean locked away beneath a crust of ice; deep below, the moon's internal heat might create hospitable
conditions, akin to
hydrothermal vents at the bottom of the mid-Atlantic ridge and East Pacific Rise on Earth.
Knowing the lifespan of the larval tube worm and the current
conditions at other
hydrothermal vent sites should thus enable researchers to predict tube worm dispersal, team member Lauren Mullineaux of the Woods Hole Oceanographic Institute says.
The unique temperature
conditions of
hydrothermal vents like this one could have favored the evolution of complex life.
Water locked away in rocks for 1.5 billion years reveals
conditions were right for complex organic molecules to form in deep sea
hydrothermal vents
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.
It's «nice chemistry,» says marine chemist Jeffrey Bada of the University of California (UC), San Diego, but he is not convinced that
hydrothermal vents, or any other likely habitat on early Earth, could have provided the
conditions created in the lab: «The processes outlined are not likely to take place on a significant scale on the Earth or elsewhere.»
Such statements do not begin to address the
conditions and processes that led to the assembly of the nucleotides — adenine, guanine, cytosine, thymine and uracil — nor do the statements indicate that the materials necessary to form the nucleotides might be present in
hydrothermal vents.
Mars is thought to have contained oceans with similar
conditions to those near
hydrothermal vents at around the same time the fossils were thriving, living creatures.
On Earth,
hydrothermal habitats always contain extremophiles, or organisms capable to adapt to the extreme
conditions.
Gabriel Tobie of the University of Nantes in France, who was not involved in the research, compared the
conditions that created these silica particles to a
hydrothermal field in the Atlantic Ocean known as Lost City.
The revolutionary discovery in the 1970s of a thriving complex marine ecosystem around the
hydrothermal vents of the Galapagos Rift on the ocean floor of the eastern Pacific forever changed our understanding of habitability showing that life could also arise and flourish in the complete absence of sunlight in
conditions that were utterly toxic to any other life forms on Earth.
On Earth, the most common way to form silica grains of this size is
hydrothermal activity under a specific range of
conditions; namely, when slightly alkaline and salty water that is super-saturated with silica undergoes a big drop in temperature.
«The
conditions of
hydrothermal alteration inferred by analogy with experiments, especially temperature, are at odds with the
We were able to show that under [presumed] Enceladus - like
conditions and the given environmental parameters, biological methane production did occur in the lab,» and that a «microoorganism from a
hydrothermal vent system on Earth could be grown in the presence of [presumed] inhibitors in combination with high pressure.»
u «The
conditions of
hydrothermal alteration inferred by analogy with experiments, especially temperature, are at odds with the [observed] mineralogy and preservation of volatile organic compounds.»
Under natural
conditions, vapor pressure may rise high enough to cause fracturing in a process known as
hydrothermal brecciation.
Weather
conditions have constrained the discovery of
hydrothermal vents at high latitudes, although there is evidence from water column plumes that vents occur in the Arctic along the Gakkel Ridge [10], the Mohn Ridge, [11] and the Arctic Mid-Ocean Ridge [12], and in the Southern Ocean, in Antarctica, along the East Scotia Ridge (ESR), in the Scotia Sea [13], in the Bransfield Strait, west of the northern Antarctic Peninsula [14], [15], and along the Pacific - Antarctic Ridge [16].