Their primary goal was to produce life from non life.
Did Friedrich Wöhler's experiment prove that life could be produced from non-life?
Of course not, it is old and actually more contemporary research updated his work. still no proof here.
You perpetually abuse the English language and science by using phony terminology such as accusations of the need and use of "proof" in science
No, his synthesis of urea demonstrated that the boundary between inorganic and organic matter wasn’t fixed as Scientist thought.
Enjoy,
No enjoyment here concerning your selective abuse of science, I doubt seriously that you have any qualification to make the statements and conclusion you make The research and discoveries concerning abiogenesis is work in progress. There has far more discoveries and research since that have demonstrated the processes of abiogenesis, such as the following example . . .
Researchers led by Ryuhei Nakamura at the RIKEN Center for Sustainable Resource Science (CSRS) in Japan and The Earth-Life Science Institute (ELSI) of Tokyo Institute of Technology have discovered inorganic nanostructures surrounding deep-ocean hydrothermal vents that are strikingly similar to...
phys.org
https://phys.org/news/2024-09-nanostructures-deep-ocean-floor-hint.html#
September 25, 2024
Editors' notes
Nanostructures in the deep ocean floor hint at life's origin
by
RIKEN
a) Photograph of HV precipitates collected from the Shinkai Seep Field. b) Cross-polarized optical microscope images of precipitates in cross section. c,d) Scanning electron images showing layers within the precipitates. f) Magnification showing sublayers in the boxed area of d. Credit: RIKEN
Researchers led by Ryuhei Nakamura at the RIKEN Center for Sustainable Resource Science (CSRS) in Japan and The Earth-Life Science Institute (ELSI) of Tokyo Institute of Technology have discovered inorganic nanostructures surrounding deep-ocean hydrothermal vents that are strikingly similar to molecules that make life as we know it possible. These nanostructures are self-organized and act as selective ion channels, which create energy that can be harnessed in the form of electricity.
Published Sept. 25 in
Nature Communications, the
findings impact not only our understanding of how life began, but can also be applied to industrial blue-
energy harvesting.
When seawater seeps way down into the Earth through cracks in the ocean floor, it gets heated by magma, rises back up to the surface, and is released back into the ocean through fissures called hydrothermal vents. The rising hot water contains dissolved minerals gained from its time deep in the Earth, and when it meets the cool ocean water,
chemical reactions force the mineral ions out of the water where they form solid structures around the vent called precipitates.
Hydrothermal vents are thought to be the birthplace of life on Earth because they provide the necessary conditions: they are stable, rich in minerals, and contain sources of energy. Much of life on Earth relies on osmotic energy, which is created by ion gradients—the difference in salt and proton concentration—between the inside and outside of living cells.
The RIKEN CSRS researchers were studying serpentinite-hosted hydrothermal vents because this kind of vent has mineral precipitates with a very complex layered structure formed from metal oxides, hydroxides, and carbonates.
"Unexpectedly, we discovered that osmotic energy conversion, a vital function in modern plant, animal, and microbial life, can occur abiotically in a geological environment," says Nakamura.
The researchers were studying samples collected from the Shinkai Seep Field, located in the Pacific Ocean's Mariana Trench at a depth of 5,743 m. The key sample was an 84-cm piece composed mostly of brucite. Optical microscopes and scans with micrometer-sized X-ray beams revealed that brucite crystals were arranged in continuous columns that acted as nano-channels for the vent fluid.
The researchers noticed that the surface of the precipitate was electrically charged, and that the size and direction of the charge—positive or negative—varied across the surface. Knowing that structured nanopores with variable charge are the hallmarks of osmotic energy conversion, they next tested whether osmotic energy conversion was indeed occurring naturally in the inorganic deep-sea rock.