Can Cells Form in Venus’s Clouds? – Cyworthy

Venus, the second planet from the Sun, is often called Earth’s sister planet. If extraterrestrial observers on a remote exoplanet were to analyze our solar system with the same methods used by observers on Earth today, the two planets would appear strikingly similar. Both are rocky, with nearly identical diameters and masses, and both exist within or near the solar system’s habitable zone. However, only one of them is known to support life.

A significant difference between the two planets—and a likely reason for the first—is their atmospheric compositions. Earth’s atmosphere comprises approximately 78% nitrogen and 21% oxygen, whereas Venus’ atmosphere consists of more than 96% carbon dioxide. In the distant past, volcanic activity released this carbon dioxide, triggering an uncontrollable greenhouse effect. This process, coupled with Venus’ proximity to the Sun, has driven its surface temperature to a searing 500°C (900°F).

Harold Morowitz and Carl Sagan first observed in 1967 that although Venus’ barren surfaces may be inhospitable to life as we know it, its clouds present “an entirely different story,” according to Morowitz. The upper atmosphere of Venus contains low levels of water vapor and cloud regions characterized by extreme temperatures and pressures. These conditions could potentially support some types of terrestrial microorganisms and have led scientists to investigate the clouds of Venus. In the 1970s, these clouds were found to be primarily composed of sulfuric acid, which is considered incompatible with life. Nevertheless, a controversial detection of phosphine—gases found in Venus’ clouds that could be produced by microbes on Earth—has prompted some astrobiologists to reevaluate this notion of habitability. This has opened discussions on potential habitability.

Previously, researchers established that biomolecules such as the nucleic acids forming DNA can remain stable for up to one year in sulfuric acid concentrations ranging from 81% to 98%. To advance this research, scientists at the University of Chicago have recently tested whether more complex organic structures can also form in concentrated sulfuric acid.

They began with a set of carbon-based molecules known as lipids. Lipids serve as the foundation of cell membranes, acting as a barrier to the external environment and regulating what enters and exits the cell. The research team contended that cell membranes are essential for life, especially under extreme conditions like those present in Venus’ clouds. Thus, they evaluated whether simple lipids could create membranous structures called vesicles in concentrated sulfuric acid.

Membrane lipids feature one side that is attracted to water, known as the hydrophilic side, and another that repels water, termed the hydrophobic side (Figure below, left). The hydrophilic side consists of long carbon chains, referred to as tails, while the hydrophobic side comprises charged compounds known as polar heads. In cell membranes, lipids are arranged in bilayers, with hydrophilic tails oriented inwards and hydrophobic heads facing outwards (Figure below, right). The research team selected simple, commercially available lipids with tails of 10 or 18 carbon atoms and polar heads of trimethylamine, sulfate, and phosphonate. These tailed lipids were chosen for their solubility and ability to form membrane structures due to their hydrophobic nature.

Illustration of a single simple lipid (left) and stacked lipids forming a cell membrane structure (right). Created by the author.

To assess the lipids’ resilience against sulfuric acid, various concentrations of each 10-carbon lipid were incubated in 1%, 30%, and 70% sulfuric acid for a minimum of 1 hour at room temperature. Utilizing a method that evaluates molecular structures based on their magnetic properties, they examined how increasing acid concentrations affected the lipids. Results indicated that trimethylamine and phosphonate lipids remained stable in up to 70% sulfuric acid, although around 20% of the sulfate head degraded.

The researchers then explored whether the lipids could form vesicles in these sulfuric acid solutions. They prepared lipid mixtures across varying concentrations in 70% to 90% sulfuric acid, measuring the particle size of the lipid-acid mixture using light scattering techniques. They discovered that a 50/50 blend of 10-carbon or 18-carbon lipids produced particles comparable in size to typical vesicles in 70% and 80% sulfuric acid solutions, with these particles maintaining stability even after a week.

Upon examination under a high-powered microscope, the lipid particles formed foam-like vesicles. Lastly, numerical models illustrated that the charged ends of lipid and acid molecules interact at the molecular level to help stabilize the vesicles and prevent the entry of acid.

The researchers concluded that simple lipids can create stable membrane-like structures in sulfuric acid concentrations similar to those found in Venusian clouds. They recommended that future studies conduct laboratory experiments to validate the molecular model and ascertain whether lipid membranes can effectively block sulfuric acid. These scientists are beginning to formulate a clearer picture of the potential types of life that could exist within the cloud layers of Venus, although that picture remains largely incomplete.


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Source: sciworthy.com

Oxygen and carbon ions detected in Venus’s magnetosphere by BepiColombo

In August 2021, ESA/JAXA BepiColombo spacecraft bound for Mercury Performed a second flyby of Venus, providing short-term observations of its guided magnetosphere. The spacecraft detected cold oxygen and carbon ions at a distance of about six planet radii, in an area of ​​the magnetosphere that has never been explored before.



Schematic illustration of planetary material escaping through the sides of Venus's magnetic sheath. The red line and arrow indicate the observation region and direction of BepiColombo as the ions escape (C+,oh+,H+) was observed. Image credit: Thibaut Roger / Europlanet 2024 RI / Hadid other.

Venus was similar to Earth in many ways during its formation, including the presence of large amounts of liquid water.

However, Venus eventually underwent a divergent evolution, leading to major differences between the two planets.

Unlike Earth, Venus is currently a very dry planet with no inherent magnetic field.

The continuous influence of the solar wind on the atmospheres of both planets results in significant atmospheric losses.

Venus' atmosphere is primarily composed of carbon dioxide and small amounts of nitrogen and other trace species, and is affected by interactions with the solar wind, leading to significant ion fluxes.

“This is the first time that positively charged carbon ions have been observed to be ejected from Venus's atmosphere,” said Dr. Lina Hadid, a researcher at the Plasma Physics Institute and CNRS.

“These are heavy ions that typically move slowly, so we're still trying to understand the mechanism.”

“An electrostatic 'wind' may be moving them away from Earth, or they may be accelerated by centrifugal action.”

“Unlike Earth, Venus does not generate an intrinsic magnetic field at its core.”

“Nevertheless, interactions between charged particles emitted by the sun (solar wind) and charged particles in Venus' upper atmosphere create a weak, comet-shaped 'induced magnetosphere' around the planet. ”

“Around the magnetosphere there is a region called the 'magnetic sheath' where the solar wind is slowed down and heated.”

On August 10, 2021, BepiColombo passed Venus to slow down and adjust its course towards its final destination, Mercury.

The probe soared up the long tail of the planet's magnetic sheath, emerging from the nose of the magnetic region closest to the sun.

Over a 90-minute observation period, BepiColombo's mass spectrometer (MSA) and mercury ion analyzer (MIA) will measure the number and mass of charged particles encountered, and detect chemical and Captured information about physical processes. magneto sheath.

“Characterizing the loss of heavy ions on Venus and understanding the escape mechanisms will help us understand how Venus's atmosphere evolved,” said Dr. Dominique Delcourt, principal investigator at MSA and researcher at the Plasma Physics Institute. “This is critical to understanding how water is lost.” .

“This result shows a unique result from measurements made during a flyby of a planet, in which the spacecraft may pass through areas that are generally inaccessible to orbiting spacecraft. '' said Dr. Nicolas Andre, a researcher at the Astrophysical and Planetary Institute.

of study It was published in the magazine natural astronomy.

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LZ Hadid other. BepiColombo's observations of cold oxygen and carbon ions on the side of Venus' induced magnetosphere. Nat Astron, published online on April 12, 2024. doi: 10.1038/s41550-024-02247-2

Source: www.sci.news