
In a galaxy far, far away ... did we find life?
In the last few years, astronomers have discovered that our galaxy is teeming with planets unlike anything in our solar system.
One such exotic world, K2-18b, made the news recently over what some scientists claim is tentative evidence of what could be signs of life. Others say it's far too soon to tell.
K2-18b weighs in at more than eight times the mass of Earth, orbits a red dwarf star every 33 days and just might be covered with a massive ocean and blanketed by an atmosphere complete with water vapor and rain clouds, according to work done by two teams of researchers.
Researchers now say they've detected hints of two compounds that would make K2-18b smell like the sea. Dimethyl sulfide (DMS) and dimethyl disulfide (DMDS) are produced on Earth by phytoplankton and other marine microorganisms. The evidence isn't strong enough to declare alien life — yet — but with more observations, it might be.
Scientists do agree on the astonishing fact that it's possible to use tiny changes in light reaching us to measure what's in the atmospheres of planets orbiting stars trillions of miles away. Previous observations of K2-18b with the Hubble Space Telescope detected carbon dioxide, methane and water vapor in its atmosphere. The newer findings, published in the Astrophysical Journal Letters, were done using the James Webb Space Telescope and strengthened the case for the sea-scented sulfur compounds.
With a mass and size in between that of Earth and Neptune, it's called a sub-Neptune and fits into a size range that's not found in our solar system. The red dwarf it orbits is much dimmer than our sun but is closer, so it's warm enough for water to remain liquid. Models show it might be covered in an ocean 600 miles deep, more than 100 times the depth of our oceans. However, scientists say they can't rule out that K2-18b is a molten hellscape or a gaseous planet with no surface.
The possible detection of DMS and DMDS is exciting because they constitute a biosignature — a chemical unlikely to have formed without life. Abundant oxygen here on Earth would be a similar giveaway to life-seeking alien astronomers since we acquired our oxygen-rich atmosphere only after the evolution of photosynthesis.
Back in 1999, Sarah Seager, an astrophysicist at MIT, proposed a way to search for life by looking for such biosignature compounds in the atmospheres of planets around other stars — even though most such planets are invisible even to the most powerful telescopes and have to be detected indirectly by changes in stellar brightness or motion.
Seager's idea would only work in cases where a planet's orbit takes it between us and its parent star, causing a slight periodic dip in starlight, like a mini eclipse. In such cases, the planet's atmosphere would alter the starlight that passes through, like a flashlight passing through fog, Seager told me. She proposed back then that scientists could observe changes in the spectrum of starlight to infer which atmospheric gases were present.
Since then, Seager said, astronomers have been surprised to find hundreds of these mid-sized sub-Neptunes. "We have no solar system counterparts,' she said, "yet it appears to be the most common planet in our galaxy.'
And while studying distant planets isn't the primary purpose of the James Webb telescope, it's given astronomers a new window into their compositions and potential habitability. "It's just absolutely gratifying to see the telescope being used to study untold numbers of exoplanet atmospheres ... atmospheres of all kinds that we never anticipated existing,' she said.
One of her graduate students, now at Cambridge University, led this new work on K2-18b. She said they still need stronger evidence that they really detected the dimethyl sulfide and dimethyl disulfide, and then they need to show that these gases couldn't be produced by some nonbiological process.
Meanwhile, other lines of evidence suggest life is abundant in the universe. Microfossils show that Earth was inhabited soon after it cooled enough to form a solid crust and the building blocks of life have been detected far from Earth. A recent NASA mission to sample an asteroid named Bennu showed it held amino acids, which make up proteins and nucleotides — the same building blocks humans use to make RNA and DNA.
Detecting ET probably won't come as a single discovery credited to one group, said astrophysicist Adam Frank of the University of Rochester. Frank compares life detection to the understanding that the universe is expanding. That wasn't a scientific consensus until it was confirmed with multiple independent lines of evidence over the course of the 20th century.
He said it's possible to detect not only biosignatures on distant worlds but also "techno-signatures,' including gases unlikely to be produced except through alien technology. That might include chlorofluorocarbons, which started to build up in our atmosphere after we created them to use as refrigerants, propellants for aerosol sprays and other applications.
It may take a space telescope more powerful than the James Webb to determine which planets host life. That's why NASA is planning to launch a dedicated instrument called the Habitable Worlds Observatory. Given NASA's budget cuts, the future of this project is unknown, but it would be a shame to give up the search now when we're so close and the universe has produced so many weird and wonderful planets.
F.D. Flam is a Bloomberg Opinion columnist covering science. She is host of the "Follow the Science' podcast.
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Japan Times
2 days ago
- Japan Times
How did life survive 'Snowball Earth'? In ponds, study suggests.
Earth hasn't always been a hospitable place to live. During several ice ages, the planet's surface was almost completely frozen over, creating what has been dubbed "Snowball Earth." Liquid water appears to be the most important ingredient for life on any planet, raising the question: how did anything survive such frosty, brutal times? A group of scientists said Thursday that they had found an astonishing diversity of microorganisms in tiny pools of melted ice in Antarctica, suggesting that life could have ridden out Snowball Earth in similar ponds. During the Cryogenian Period between 635 and 720 million years ago, the average global temperature did not rise above minus 50 degrees Celsius. The climate near the equator at the time resembled modern-day Antarctica. Yet even in such extreme conditions, life found a way to keep evolving. Fatima Husain, the lead author of a new study published in Nature Communications, said there was evidence of complex life forms "before and after the Cryogenian in the fossil record." "There are multiple hypotheses regarding possible places life may have persisted," said Husain, a graduate student at the Massachusetts Institute of Technology. Perhaps it found shelter in patches of open ocean, or in deep-sea hydrothermal vents, or under vast sheets of ice. The tiny melted ice pools that dotted the equator were another proposed refuge. These ponds could have been oases for eukaryotes, complex organisms that eventually evolved into multicellular life forms that would rise to dominate Earth, including humans. Melted ice ponds still exist today in Antarctica, at the edges of ice sheets. In 2018, members of a New Zealand research team visited the McMurdo ice shelf in east Antarctica, home to several such pools, which are only a few meters wide and less a meter deep. The bottom of the ponds are lined with a mat of microbes that have accumulated over the years to form slimy layers. "These mats can be a few centimeters thick, colorful, and they can be very clearly layered," Husain said. They are made up of single-celled organisms called cyanobacteria that are known to be able to survive extreme conditions. But the researchers also found signs indicating there were eukaryotes such as algae or microscopic animals. This suggests there was surprising diversity in the ponds, which appears to have been influenced by the amount of salt each contained. "No two ponds were alike," Husain said. "We found diverse assemblages of eukaryotes from all the major groups in all the ponds studied." "They demonstrate that these unique environments are capable of sheltering diverse assemblages of life, even in close proximity," she added. This could have implications in the search for extraterrestrial life. "Studies of life within these special environments on Earth can help inform our understanding of potential habitable environments on icy worlds, including icy moons in our Solar System," Husain said. Saturn's moon Enceladus and Jupiter's Europa are covered in ice, but scientists increasingly suspect they could be home to simple forms of life, and several space missions have been launched to find out more about them.


Yomiuri Shimbun
03-05-2025
- Yomiuri Shimbun
Comet-like Planet Observed Disintegrating near Its Star
Jose-Luis Olivares, MIT / Handout via Reuters The disintegrating exoplanet BD+05 4868 Ab orbits a sun-like star 140 light years away from Earth in this illustration released on April 22. WASHINGTON (Reuters) — Astronomers have spotted a small rocky planet that orbits perilously close to its host star disintegrating as its surface is vaporized by stellar heat, trailed by a comet-like tail of mineral dust up to about 9 million kilometers long. About 5,800 planets beyond our solar system, called exoplanets, have been discovered since the 1990s. Of those, only four have been observed disintegrating in orbit, as this one is. This planet is the closest to our solar system of the four, giving scientists a unique opportunity to learn about what happens to these doomed worlds. The researchers have observed the planet, named BD+05 4868 Ab, as it gradually crumbles into dust, shedding material roughly equal to the mass of Mount Everest with each orbit of its star. The tail of dust trailing the planet wraps halfway around the star. The planet is estimated as between the size of our solar system's smallest and innermost planet Mercury and Earth's moon. It is located about 140 light years away from Earth in the constellation Pegasus. Its host star, a type called an orange dwarf, is smaller, cooler and dimmer than the sun, with about 70% of the sun's mass and diameter and about 20% of its luminosity. The planet orbits this star every 30.5 hours at a distance about 20 times closer than Mercury is to the sun. The planet's surface temperature is estimated at close to about 1,600 C thanks to its close proximity to its star. As a result, the planet's surface has probably been turned to magma — molten rock. 'We expect the planet to disintegrate into dust within the next million years or so,' said Marc Hon, a postdoctoral researcher at the Massachusetts Institute of Technology's Kavli Institute for Astrophysics and Space Research and lead author of the study published on April 22 in the Astrophysical Journal Letters. 'This is catastrophically quick in cosmic timescales. The disintegration is a runaway process. As more material from the planet turns into dust, the disintegration process gets faster,' Hon said. Once in space, the vaporized material cools down to form mineral dust that streams away from the planet. 'We know the dust grains in the tail can have sizes between large soot particles and fine grains of sand,' Hon said. 'We don't know the mineral composition of the tail yet.' The researchers detected BD+05 4868 Ab using the 'transit method,' observing a dip in the host star's brightness when the planet passes in front of it, from the perspective of a viewer on Earth. It was found using NASA's Transiting Exoplanet Survey Satellite, or TESS, space telescope. How the planet came to have its current close-in orbit is unclear. 'The planet's orbit is not seen to be visibly decaying from the data. It is possible that the planet initially formed farther away, and had its original orbit altered under the influence of an external body, such that the planet was sent much closer to the star,' Hon said. This could have resulted from the gravitational influence of another planet or some other celestial object. The researchers plan further observations in the coming months using NASA's James Webb Space Telescope to study the composition of the material in the tail, which could give clues about the makeup of rocky exoplanets. The search for life in other solar systems focuses on rocky exoplanets orbiting stars in the 'habitable zone,' a distance where liquid water, a key ingredient for life, can exist on a planetary surface. 'The tail is expected to contain minerals evaporated from the surface or interior of the disintegrating planet. So, this could be the crust, mantle or even the planet's core. Learning about the interiors of planets is extremely challenging. Doing this even for planets within our solar system is difficult. But BD+05 4868 Ab will allow us to directly measure the mineral composition of a terrestrial planet outside our solar system,' Hon said. 'This is definitely an exceptional opportunity for exoplanet geology and to understand the diversity and potential habitability of rocky worlds beyond our solar system,' Hon said.


Japan Times
28-04-2025
- Japan Times
In a galaxy far, far away ... did we find life?
In the last few years, astronomers have discovered that our galaxy is teeming with planets unlike anything in our solar system. One such exotic world, K2-18b, made the news recently over what some scientists claim is tentative evidence of what could be signs of life. Others say it's far too soon to tell. K2-18b weighs in at more than eight times the mass of Earth, orbits a red dwarf star every 33 days and just might be covered with a massive ocean and blanketed by an atmosphere complete with water vapor and rain clouds, according to work done by two teams of researchers. Researchers now say they've detected hints of two compounds that would make K2-18b smell like the sea. Dimethyl sulfide (DMS) and dimethyl disulfide (DMDS) are produced on Earth by phytoplankton and other marine microorganisms. The evidence isn't strong enough to declare alien life — yet — but with more observations, it might be. Scientists do agree on the astonishing fact that it's possible to use tiny changes in light reaching us to measure what's in the atmospheres of planets orbiting stars trillions of miles away. Previous observations of K2-18b with the Hubble Space Telescope detected carbon dioxide, methane and water vapor in its atmosphere. The newer findings, published in the Astrophysical Journal Letters, were done using the James Webb Space Telescope and strengthened the case for the sea-scented sulfur compounds. With a mass and size in between that of Earth and Neptune, it's called a sub-Neptune and fits into a size range that's not found in our solar system. The red dwarf it orbits is much dimmer than our sun but is closer, so it's warm enough for water to remain liquid. Models show it might be covered in an ocean 600 miles deep, more than 100 times the depth of our oceans. However, scientists say they can't rule out that K2-18b is a molten hellscape or a gaseous planet with no surface. The possible detection of DMS and DMDS is exciting because they constitute a biosignature — a chemical unlikely to have formed without life. Abundant oxygen here on Earth would be a similar giveaway to life-seeking alien astronomers since we acquired our oxygen-rich atmosphere only after the evolution of photosynthesis. Back in 1999, Sarah Seager, an astrophysicist at MIT, proposed a way to search for life by looking for such biosignature compounds in the atmospheres of planets around other stars — even though most such planets are invisible even to the most powerful telescopes and have to be detected indirectly by changes in stellar brightness or motion. Seager's idea would only work in cases where a planet's orbit takes it between us and its parent star, causing a slight periodic dip in starlight, like a mini eclipse. In such cases, the planet's atmosphere would alter the starlight that passes through, like a flashlight passing through fog, Seager told me. She proposed back then that scientists could observe changes in the spectrum of starlight to infer which atmospheric gases were present. Since then, Seager said, astronomers have been surprised to find hundreds of these mid-sized sub-Neptunes. "We have no solar system counterparts,' she said, "yet it appears to be the most common planet in our galaxy.' And while studying distant planets isn't the primary purpose of the James Webb telescope, it's given astronomers a new window into their compositions and potential habitability. "It's just absolutely gratifying to see the telescope being used to study untold numbers of exoplanet atmospheres ... atmospheres of all kinds that we never anticipated existing,' she said. One of her graduate students, now at Cambridge University, led this new work on K2-18b. She said they still need stronger evidence that they really detected the dimethyl sulfide and dimethyl disulfide, and then they need to show that these gases couldn't be produced by some nonbiological process. Meanwhile, other lines of evidence suggest life is abundant in the universe. Microfossils show that Earth was inhabited soon after it cooled enough to form a solid crust and the building blocks of life have been detected far from Earth. A recent NASA mission to sample an asteroid named Bennu showed it held amino acids, which make up proteins and nucleotides — the same building blocks humans use to make RNA and DNA. Detecting ET probably won't come as a single discovery credited to one group, said astrophysicist Adam Frank of the University of Rochester. Frank compares life detection to the understanding that the universe is expanding. That wasn't a scientific consensus until it was confirmed with multiple independent lines of evidence over the course of the 20th century. He said it's possible to detect not only biosignatures on distant worlds but also "techno-signatures,' including gases unlikely to be produced except through alien technology. That might include chlorofluorocarbons, which started to build up in our atmosphere after we created them to use as refrigerants, propellants for aerosol sprays and other applications. It may take a space telescope more powerful than the James Webb to determine which planets host life. That's why NASA is planning to launch a dedicated instrument called the Habitable Worlds Observatory. Given NASA's budget cuts, the future of this project is unknown, but it would be a shame to give up the search now when we're so close and the universe has produced so many weird and wonderful planets. F.D. Flam is a Bloomberg Opinion columnist covering science. She is host of the "Follow the Science' podcast.