Wednesday, March 19, 2025

SPACE/COSMOS

 

New high-definition pictures of the baby universe




The ACT collaboration has rigorously tested the standard model of cosmology and shown it to be remarkably robust. The new, polarized images of the early universe reveal the formation of ancient clouds that consolidated into the first galaxies and stars




Princeton University

New high-definition polarized pictures of the baby universe from ACT 

image: 

Research by the Atacama Cosmology Telescope collaboration has led to the clearest and most precise images yet of the universe’s infancy, the cosmic microwave background radiation that was visible only 380,000 years after the Big Bang.

This new sky map has put the standard model of cosmology through a rigorous new set of tests and show it to be remarkably robust. The new images of the early universe, which show both the intensity and polarization of the earliest light with unprecedented clarity, reveal the formation of ancient, consolidating clouds of hydrogen and helium that later developed into the first galaxies and stars. 

This piece of the new sky map that shows the vibration directions (or polarization) of the radiation. The zoom-in on the right is 10 degrees high. Polarized light vibrates in a particular direction; blue shows where the surrounding light’s vibration directions are angled towards it, like spokes on a bicycle; orange shows places where the vibration directions circle around it. This new information reveals the motion of the ancient gases in the universe when it was less than half a million years old, pulled by the force of gravity in the first step towards forming galaxies. The red band comes from our closer-by Milky Way.

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Credit: ACT Collaboration; ESA/Planck Collaboration




New research by the Atacama Cosmology Telescope (ACT) collaboration has produced the clearest images yet of the universe’s infancy – the earliest cosmic time yet accessible to humans. Measuring light that traveled for more than 13 billion years to reach a telescope high in the Chilean Andes, the new images reveal the universe when it was about 380,000 years old – the equivalent of hours-old baby pictures of a now middle-aged cosmos. 

“We are seeing the first steps towards making the earliest stars and galaxies,” says Suzanne Staggs, director of ACT and Henry deWolf Smyth Professor of Physics at Princeton University. “And we’re not just seeing light and dark, we’re seeing the polarization of light in high resolution. That is a defining factor distinguishing ACT from Planck and other, earlier telescopes.” 

The new pictures of this background radiation, known as the cosmic microwave background (CMB), add higher definition to those observed more than a decade ago by the Planck space-based telescope. “ACT has five times the resolution of Planck, and greater sensitivity,” says Sigurd Naess, a researcher at the University of Oslo and a lead author of one of several papers related to the project. “This means the faint polarization signal is now directly visible.” 

The polarization image reveals the detailed movement of the hydrogen and helium gas in the cosmic infancy. “Before, we got to see where things were, and now we also see how they're moving,” says Staggs. “Like using tides to infer the presence of the moon, the movement tracked by the light’s polarization tells us how strong the pull of gravity was in different parts of space.” 

The new results confirm a simple model of the universe and have ruled out a majority of competing alternatives, says the research team. The work has not yet gone through peer review, but the researchers will present their results at the American Physical Society annual conference on March 19. 

Measuring the universe’s infancy 

In the first several hundred thousand years after the Big Bang, the primordial plasma that filled the universe was so hot that light couldn’t propagate freely, making the universe effectively opaque. The CMB represents the first stage in the universe's history that we can see – effectively, the universe’s baby picture. 

The new images give a remarkably clear view of very, very subtle variations in the density and velocity of the gases that filled the young universe. “There are other contemporary telescopes measuring the polarization with low noise, but none of them cover as much of the sky as ACT does,” says Naess. What look like hazy clouds in the light’s intensity are more and less dense regions in a sea of hydrogen and helium – hills and valleys that extend millions of light years across. Over the following millions to billions of years, gravity pulled the denser regions of gas inwards to build stars and galaxies. 

These detailed images of the newborn universe are helping scientists to answer longstanding questions about the universe’s origins. “By looking back to that time when things were much simpler, we can piece together the story of how our universe evolved to the rich and complex place we find ourselves in today, ” says Jo Dunkley, the Joseph Henry Professor of Physics and Astrophysical Sciences at Princeton University and the ACT analysis leader. 

“We’ve measured more precisely that the observable universe extends almost 50 billion light years in all directions from us, and contains as much mass as 1,900 ‘zetta-suns’, or almost 2 trillion trillion Suns,” says Erminia Calabrese, professor of astrophysics at the University of Cardiff and a lead author on one of the new papers. Of those 1,900 zetta-suns, the mass of normal matter – the kind we can see and measure – makes up only 100. Another 500 zetta-Suns of mass are mysterious dark matter, and the equivalent of 1,300 are the dominating vacuum energy (also called dark energy) of empty space. 

Tiny neutrino particles make up at most four zetta-suns of mass. Of the normal matter, three-quarters of the mass is hydrogen, and a quarter helium. “Almost all of the helium in the universe was produced in the first three minutes of cosmic time,” says Thibaut Louis, CNRS researcher at IJCLab, University Paris-Saclay and one of the lead authors of the new papers. “Our new measurements of its abundance agree very well with theoretical models and with observations in galaxies.” The elements that we humans are made of – mostly carbon, with oxygen and nitrogen and iron and even traces of gold – were formed later in stars and are just a sprinkling on top of this cosmic stew. 

ACT’s new measurements have also refined estimates for the age of the universe and how fast it is growing today. The infall of matter in the early universe sent out sound waves through space, like ripples spreading out in circles on a pond.

“A younger universe would have had to expand more quickly to reach its current size, and the images we measure would appear to be reaching us from closer by”, explains Mark Devlin, the Reese W. Flower Professor of Astronomy at the University of Pennsylvania, and ACT’s deputy director. “The apparent extent of ripples in the images would be larger in that case, in the same way that a ruler held closer to your face appears larger than one held at arm’s length.” The new data confirm that the age of the universe is 13.8 billion years, with an uncertainty of only 0.1%. 

The Hubble tension 

In recent years, cosmologists have disagreed about the Hubble constant, the rate at which space is expanding today. Measurements derived from the CMB have consistently shown an expansion rate of 67 to 68 kilometers per second per Megaparsec, while measurements derived from the movement of nearby galaxies indicate a Hubble constant as high as 73 to 74 km/s/Mpc. Using their newly released data, the ACT team has measured the Hubble constant with increased precision. Their measurement matches previous CMB-derived estimates. “We took this entirely new measurement of the sky, giving us an independent check of the cosmological model, and our results show that it holds up,” says Adriaan Duivenvoorden, a research fellow at the Max Planck Institute for Astrophysics and lead author of one of the new papers. 

A major goal of the work was to investigate alternative models for the universe that would explain the disagreement. “We wanted to see if we could find a cosmological model that matched our data and also predicted a faster expansion rate,” says Colin Hill, an assistant professor at Columbia University and one of the lead authors of the new papers. Alternates include changing the way neutrinos and the invisible dark matter behave, adding a period of accelerated expansion in the early universe or changing fundamental constants of nature. 

“We have used the CMB as a detector for new particles or fields in the early universe, exploring previously uncharted terrain,” says Hill. ‘The ACT data show no evidence of such new signals. With our new results, the standard model of cosmology has passed an extraordinarily precise test.” 

“It was slightly surprising to us that we didn't find even partial evidence to support the higher value,” says Staggs. “There were a few areas where we thought we might see evidence for explanations of the tension, and they just weren’t there in the data.” 

A 5-year exposure

The background radiation measured by ACT is extremely faint. “To make this new measurement, we needed a 5-year exposure with a sensitive telescope tuned to see millimeter-wavelength light,” says Devlin. “Our colleagues at the National Institute of Standards and Technology provided detectors with cutting-edge sensitivity, and the National Science Foundation supported ACT’s mission for more than two decades to get us here.”

In surveying the sky, ACT has also seen light emitted from other objects in space. “We can see right back through cosmic history,” says Dunkley, “from our own Milky Way, out past distant galaxies hosting vast black holes, and huge galaxy clusters, all the way to that time of infancy.” 

ACT completed its observations in 2022, and attention is now turning to the new, more capable, Simons Observatory at the same location in Chile. The new ACT data are shared publicly on NASA’s LAMBDA archive. 

Research by the Atacama Cosmology Telescope collaboration has led to the clearest and most precise images yet of the universe’s infancy, the cosmic microwave background radiation that was visible only 380,000 years after the Big Bang.

This new sky map has put the standard model of cosmology through a rigorous new set of tests and show it to be remarkably robust. The new images of the early universe, which show both the intensity and polarization of the earliest light with unprecedented clarity, reveal the formation of ancient, consolidating clouds of hydrogen and helium that later developed into the first galaxies and stars. 

A new image of the cosmic microwave background radiation, adding high definition from the Atacama Cosmology Telescope to an earlier image from the Planck satellite. The zoom-in is 10 degrees across, or twenty times the Moon’s width seen from Earth, and shows a tiny portion of the new half-sky image. Orange and blue show more or less intense radiation, revealing features in the density of the universe when it was less than half a million years old - a time before any galaxies had formed. The image includes closer-by objects: the red band on the right is the Milky Way, and the red dots are galaxies containing vast black holes, the blue dots are huge galaxy clusters, and the spiral Sculptor Galaxy is visible towards the bottom.

Credit

ACT Collaboration; ESA/Planck Collaboration


Research by the Atacama Cosmology Telescope collaboration has led to the clearest and most precise images yet of the universe’s infancy, the cosmic microwave background radiation that was visible only 380,000 years after the Big Bang.

This new sky map has put the standard model of cosmology through a rigorous new set of tests and show it to be remarkably robust. The new images of the early universe, which show both the intensity and polarization of the earliest light with unprecedented clarity, reveal the formation of ancient, consolidating clouds of hydrogen and helium that later developed into the first galaxies and stars. 

Credit

Debra Kellner


The pre-peer review articles highlighted in this release are available on https://act.princeton.edu/ and will appear on the open-access arXiv.org. They have been submitted to the Journal of Cosmology and Astroparticle Physics. In addition to the authors mentioned, lead authors include Zachary Atkins (Princeton University), Yilun Guan (University of Toronto), Hidde Jense (CardiffUniversity), Adrien La Posta (University of Oxford), Matthew Hasselfield (Flatiron Institute) & Yuhan Wang (Cornell University). 

This research was supported by the U.S. National Science Foundation (AST-0408698, AST-0965625 and AST-1440226 for the ACT project, as well as awards PHY-0355328, PHY-0855887 and PHY-1214379), Princeton University, the University of Pennsylvania, and a Canada Foundation for Innovation award. The project is led by Princeton University and the University of Pennsylvania, with 160 collaborators at 65 institutions. ACT operated in Chile from 2007-2022 under an agreement with the University of Chile, in the Atacama Astronomical Park. 





Meteorites: A geologic map of the asteroid belt



Knowing from what debris field in the asteroid belt our meteorites originate is important for planetary defense efforts against Near Earth Asteroids.




SETI Institute

image001_1024x724 

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Geologic map of the asteroid belt. Circles identify the asteroid families from which our meteorites originate and letters mark the corresponding meteorite type. The horizontal axis ranges from short orbits moving just inside the asteroid belt (left) to longer orbits just outside (right). The vertical axis shows how much the asteroid orbits are tilted relative to the plane of the planets. Blue lines are the delivery resonances. 

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Credit: From: Jenniskens & Devillepoix (2025) Meteoritics & Planetary Science.




March 18, 2025, Mountain View, CA -- Where do meteorites of different type come from? In a review paper in the journal Meteoritics & Planetary Science, published online this week, astronomers trace the impact orbit of observed meteorite falls to several previously unidentified source regions in the asteroid belt. 

“This has been a decade-long detective story, with each recorded meteorite fall providing a new clue,” said meteor astronomer and lead author Peter Jenniskens of the SETI Institute and NASA Ames Research Center. “We now have the first outlines of a geologic map of the asteroid belt.” 

Ten years ago, Jenniskens teamed up with astronomer Hadrien Devillepoix of Curtin University and colleagues in Australia to build a network of all-sky cameras in California and Nevada that can capture and track the bright light of meteorites as they hit the Earth’s atmosphere. Many institutes and citizen scientists participated in this effort over the years. 

“Others built similar networks spread around the globe, which together form the Global Fireball Observatory,” said Devillepoix. “Over the years, we have tracked the path of 17 recovered meteorite falls.” 

Many more fireballs were tracked by doorbell and dashcam video cameras from citizen scientists around the globe and by other dedicated networks. 

“Altogether, this quest has yielded 75 laboratory-classified meteorites with an impact orbit tracked by video and photographic cameras,” said Jenniskens. “That proves to be enough to start seeing some patterns in the direction from which the meteorites approach Earth.” 

Most meteorites originate from the asteroid belt, a region between Mars and Jupiter where over a million asteroids larger than 1 kilometer circle the Sun. Those rocks originate from a small number of larger asteroids that broke in collisions, the debris fields of which litter the region. Even today, asteroids collide to create debris fields within these asteroid families, called clusters. 

“We now see that 12 of the iron-rich ordinary chondrite meteorites (H chondrites) originated from a debris field called “Koronis,” which is located low in the pristine main belt,” said Jenniskens. “These meteorites arrived from low-inclined orbits with orbital periods consistent with this debris field.” 

Astronomers can measure how long ago these rocks were dug up from below the asteroid’s surface by measuring the level of radioactive elements created by exposure to cosmic rays. This cosmic-ray exposure age of the meteorites proves to match the dynamical age of some of the asteroid debris fields. Scientists determine the dynamical age of debris fields by measuring how much asteroids of different size have spread over time. 

“By measuring the cosmic ray exposure age of meteorites, we can determine that three of these twelve meteorites originated from the Karin cluster in Koronis, which has a dynamical age of 5.8 million years, and two came from the Koronis2 cluster, with a dynamical age of 10-15 million years,” said Jenniskens. “One other meteorite may well measure the age of the Koronis3 cluster: about 83 million years.” 

Jenniskens and Devillepoix also found a group of H-chondrites on steep orbits that appear to originate from the Nele asteroid family in the central main belt, which has a dynamical age of about 6 million years. The nearby 3:1 mean-motion resonance with Jupiter can pump up the inclinations to those observed. A third group of H chondrites that have an exposure age of about 35 million years originated from the inner main belt. 

“In our opinion, these H chondrites originated from the Massalia asteroid family low in the inner main belt because that family has a cluster of about that same dynamical age,” said Jenniskens. “The asteroid that created that cluster, asteroid (20) Massalia, is an H chondrite type parent body.” 

Jenniskens and Devillepoix find that low iron (L chondrite) and very low iron (LL chondrite) meteorites come to us primarily from the inner main belt. Scientists have long linked the LL chondrites to the Flora asteroid family on the inner side of the asteroid belt, and they have confirmed that connection. 

“We propose that the L chondrites originated from the Hertha asteroid family, located just above the Massalia family,” said Jenniskens. “Asteroid Hertha doesn’t look anything like its debris. Hertha is covered by dark rocks that were shock-blackened, indicative of an unusually violent collision. The L chondrites experienced a very violent origin 468 million years ago when these meteorites showered Earth in such numbers that they can be found in the geologic record.” 

Knowing from what debris field in the asteroid belt our meteorites originate is important for planetary defense efforts against Near Earth Asteroids. An approaching asteroid’s orbit can provide clues to its origin in the asteroid belt in the same way as meteorite orbits. 

“Near Earth Asteroids do not arrive on the same orbits as meteorites, because it takes longer for these to evolve to Earth.” said Jenniskens. “But they do come from some of the same asteroid families.”

Jenniskens and Devillepoix discuss the links of several other meteorite types to their source regions. Not all assignments are certain. 

“We are proud about how far we have come, but there is a long way to go,” said Jenniskens, “Like the first cartographers who traced the outline of Australia, our map reveals a continent of discoveries still ahead when more meteorite falls are recorded.” 

What’s coming next? Asteroids directly meet meteorites when observed in space before impacting Earth and then recovered. Jenniskens guided the recovery of the first such small asteroid in 2008, called asteroid 2008 TC3, and we are about to see a lot more thanks to new astronomical facilities coming online. 

Link to the paper: 

https://onlinelibrary.wiley.com/doi/full/10.1111/maps.14321 

About the SETI Institute 

Founded in 1984, the SETI Institute is a non-profit, multi-disciplinary research and education organization whose mission is to lead humanity’s quest to understand the origins and prevalence of life and intelligence in the universe and share that knowledge with the world. Our research encompasses the physical and biological sciences and leverages data analytics, machine learning, and advanced signal detection technologies. The SETI Institute is a distinguished research partner for industry, academia, and government agencies, including NASA and the National Science Foundation.

Nanomaterials used to measure first nuclear reaction on radioactive nuclei produced in neutron star collisions




University of Surrey





Physicists have measured a nuclear reaction that can occur in neutron star collisions, providing direct experimental data for a process that had previously only been theorised. The study, led by the University of Surrey, provides new insight into how the universe’s heaviest elements are forged – and could even drive advancements in nuclear reactor physics. 

Working in collaboration with the University of York, the University of Seville, and TRIUMF, Canada’s national particle accelerator centre, the breakthrough marks the first-ever measurement of a weak r-process reaction cross-section using a radioactive ion beam, in this case studying the 94Sr(α,n)97Zr reaction. This is where a radioactive form of strontium (strontium-94) absorbs an alpha particle (a helium nucleus), then emits a neutron and transforms into zirconium-97.  

The study has been published as an Editors Suggestion in Physical Review Letters. 

Dr Matthew Williams, lead author of the study from the University of Surrey, said: 

“The weak r-process plays a crucial role in the formation of heavy elements, which astronomers have observed in ancient stars – celestial fossils that carry the chemical fingerprints of perhaps only one prior cataclysmic event, like a supernovae or neutron star merger. Until now, our understanding of how these elements form has relied on theoretical predictions, but this experiment provides the first real-world data to test those models that involve radioactive nuclei.” 

The experiment was enabled by the use of novel helium targets. Since helium is a noble gas, meaning it is neither reactive nor solid, researchers at the University of Seville developed an innovative nano-material target, embedding helium inside ultra-thin silicon films to form billions of microscopic helium bubbles, each only a few 10s of nanometres across. 

Using TRIUMF’s advanced radioactive ion beam technology, the team accelerated short-lived strontium-94 isotopes into these targets, allowing them to measure the nuclear reaction under conditions similar to those found in extreme cosmic environments.  

Dr Williams said: 

"This is a major achievement for astrophysics and nuclear physics, and the first-time nanomaterials have been used in this way, opening exciting new possibilities for nuclear research.  

“Beyond astrophysics, understanding how radioactive nuclei behave is crucial for improving nuclear reactor design. These types of nuclei are constantly produced in nuclear reactors, but until recently, studying their reactions has been extremely difficult. Reactor physics depends on this kind of data to predict how often components need replacing, how long they’ll last and how to design more efficient, modern systems.” 

The next phase of research will apply the findings to astrophysical models, helping scientists to better understand the origins of the heaviest known elements. As researchers continue to explore these processes, their work could deepen our understanding of both the extreme physics of neutron star collisions and practical applications in nuclear technology. 

[ENDS] 

Notes to editors 

 

Pacific oyster may colonize the Baltic Sea





University of Gothenburg
Pacific oyster 

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The Pacific oyster has established itself in Bohuslän at record speed, and now it has been sighted as far down as the Sound. The question is whether the oysters will continue their journey into the Baltic Sea.

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Credit: Youk Greeve




The invasive Pacific oyster have adapted to life in less salty seas and are reproducing off the coast of Skåne, although having been there for less than ten years. This discovery by researchers from the University of Gothenburg suggests that the oysters could colonise the western Baltic Sea in the future.

Pacific oysters were imported to oyster farms in Europe in the 1970s to replace native oysters whose stocks had collapsed. But they quickly began to spread from the farms, reaching northern Bohuslän in Sweden in 2006. Since then, they have spread southwards along the Swedish west coast and are now found as far south as the Sound.

Scientists have assumed that a low salinity would act as a barrier to a further spread into the Baltic Sea, but a new study shows that the oysters can adapt quickly and possibly spread into brackish water.

“We know today that the oysters in the Sound are able to reproduce and that their larvae can be transported into the Baltic Sea by ocean currents, but we don't know if they also can adapt to the brackish living conditions there,” says Pierre De Wit, researcher in marine biology at the University of Gothenburg.

Spreading helped by warmer seas

As early as the 1970s, attempts were made to cultivate Pacific oysters in Sweden, but they failed to reproduce, probably due to the water being too cold. Pacific oysters need water temperatures above 20 degrees Celsius during a period of time to reach maturity, and it is only in the 2000s that this has become regular in Swedish waters.

Now, oysters reproduce every summer in Sweden. A single female can release hundreds of millions of eggs, and the larvae drift with ocean currents for 2-3 weeks, allowing them to spread very quickly.

A combination of environment and genetics

The authors of the study crossbred female and male oysters in waters with different salinities, from Baltic Sea salinity (8 parts per thousand) to full marine salinity (33 parts per thousand).

Oysters collected from the waters of Hallands Väderö in Skåne were able to reproduce well down to 13 parts per thousand, while oysters from Bohuslän could not cope with salinities lower than 18 parts per thousand. The study showed that the oysters’ ability to reproduce depends on a combination of the oysters’ breeding habitat and their genetics. In the lowest salinities, genetics was the most important factor.

“We don't know how low salinity a Pacific oyster will need to reproduce in the future. But much suggests that they have genes that allow them to tolerate even more brackish water than today,” says Alexandra Kinnby, researcher in marine biology at the University of Gothenburg and first author of the study.

Sperms are important

Pacific oysters have external fertilisation – eggs and sperm are released in open water by the adults, and the sperm must then find the eggs and fertilise them. But the sperms are sensitive to factors such as temperature and salinity. In the new study, the researchers show that the genetic diversity of sperm in certain key genes determine whether oysters can reproduce in low salinity.

“It’s still unclear whether the oysters will be able to establish in the Baltic Sea, or what will happen to the larvae when they drift in that direction. Will they drift back towards land again with the currents or will they remain far at sea? We don't have those answers yet,” says Pierre De Wit.

 

Plant patch can detect stress signals in real time







American Chemical Society

Plant patch can detect stress signals in real time 

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This sensor measures hydrogen peroxide, a marker of stress in soybean and tobacco plant leaves.

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Credit: Adapted from ACS Sensors 2025, DOI: 10.1021/acssensors.4c02645




Environmental conditions can cause damaging stress to plants, posing challenges for home gardeners and farmers. Therefore, early detection — before leaves visibly discolor, wilt or wither — is crucial. Now, researchers reporting in ACS Sensors have created a wearable patch for plants that quickly senses stress and relays the information to a grower. The electrochemical sensor attaches directly to live plant leaves and monitors hydrogen peroxide, a key distress signal.

Pests, drought, extreme temperatures and infections all cause stress in plants. In response, plants’ normal biochemistry gets out of whack, and they produce hydrogen peroxide, which also acts as a signal between cells to activate their defense mechanisms. Early detection of this chemical clue could help people expertly tailor plant care and prevent further damage, thereby maximizing crop yields, even in difficult conditions. But most current methods for detecting hydrogen peroxide require removal of plant parts and multiple processing steps or external detectors that observe fluorescence changes, which can get muddled by chlorophyll. And researchers have previously investigated plant-wearable devices to monitor leaf water content as an indicator of plant health. So, Liang Dong and colleagues set out to design a stand-alone patch that quickly and accurately detects the hydrogen peroxide distress signals from living plants.

To build a patch that sticks to the underside of leaves, the researchers created an array of microscopic plastic needles across a flexible base. Onto this patterned surface they coated a chitosan-based hydrogel mixture that converted small changes in hydrogen peroxide into measurable differences in electrical current. The mixture contained an enzyme that reacted with hydrogen peroxide to produce electrons and reduced graphene oxide to conduct those electrons through the sensor. 

The researchers tested their patches on live, healthy soybean and tobacco plants and compared them to stressed bacteria-infected plants. They found:

  • For both crops infected with the bacterial pathogen Pseudomonas syringae pv. tomato DC3000, the sensor produced more electrical current on stressed leaves than on healthy ones, and the current levels were directly related to the amount of hydrogen peroxide present.
  • The sensor’s measurement of hydrogen peroxide was accurate and confirmed by conventional lab analyses.
  • After about 1 minute, the patches measured hydrogen peroxide in the leaves at significantly lower levels than those previously reported from needle-like sensors for live plants.
  • Patches could be reused nine times before the microscopic needles lost their form.

The new strategy provides information that could help growers efficiently make decisions about their crops. “We can achieve direct measurements in under a minute for less than a dollar per test,” says Dong. “This breakthrough will significantly streamline analysis, making it practical for farmers to use our patch sensor for real-time disease crop monitoring.”

And the researchers are excited to continue moving the research forward. “Our next step is to refine the technology and enhance its reusability,” concludes Dong.

The authors acknowledge funding from Iowa State University, the U.S. Department of Agriculture’s National Institute of Food and Agriculture, and the National Science Foundation.

The paper’s abstract will be available  here: http://pubs.acs.org/doi/abs/10.1021/acssensors.4c02645


This reusable patch (shown on the underside of a tobacco leaf) could help growers make decisions earlier to maintain the health of their crops through earlier detection of plant stress.

Credit

Adapted from ACS Sensors 2025, DOI: 10.1021/acssensors.4c02645

 

Unknown microorganisms used marble and limestone as a habitat



Unusual structures of unknown origin found in rocks of desert areas / Publication in the Geomicrobiology Journal




Johannes Gutenberg Universitaet Mainz

microorganisms_01 

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Marble from Namibia in which micro-burrows have grown in parallel arrangement downwards from a fracture filled with white calcium carbonate

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Credit: photo/©: Cees Passchier




In the desert areas of Namibia, Oman, and Saudi Arabia, research work has revealed unusual structures that are probably due to the activity of an unknown microbiological life form. Unusually small burrows, i.e., tiny tubes that run through the rock in a parallel arrangement from top to bottom, were discovered in marble and limestone of these desert regions. "We were surprised because these tubes are clearly not the result of a geological process," said Professor Cees Passchier from Johannes Gutenberg University Mainz (JGU), who first came across the phenomenon during geological field work in Namibia. During subsequent sample investigations, evidence of biological material was found. Evidently, microorganisms had perforated the rock. "We don't currently know whether this is a life form that has become extinct or is still alive somewhere," added Passchier.

Puzzling discovery in Namibia

Geologist Cees Passchier has been working in Namibia for 25 years, among other places. His research focuses on the geological reconstruction of Precambrian terranes. "We look at the structure of the rocks to find out how continents came together to form the supercontinent Gondwana 500 to 600 million years ago," explained Passchier. At that time, carbonate deposits formed in the ancient oceans and turned into marble due to pressure and heat. "We noticed strange structures in this marble that were not the result of geological events." Instead of smooth erosion surfaces, tubes could be seen that were about half a millimeter wide and up to three centimeters long, lined up parallel to one another and forming bands up to ten meters long. Some calcrete crusts had formed on the edges.

The first observations of this kind in the Namibian desert were made 15 years ago. In the meantime, Professor Cees Passchier, together with colleagues from the Institute of Geosciences at Mainz University, and Dr. Trudy Wassenaar, head of the consulting company Molecular Microbiology and Genomics Consultants, have continued to investigate the phenomenon. "We think that it must have been a microorganism that formed these tubes." The tubes were not empty but filled with a fine powder of clean calcium carbonate. It is assumed that microorganisms may have bored the tunnels to use nutrients present in the calcium carbonate, the main component of marble. The fine powder remained behind. Passchier also found very similar structures during field work in Oman and in Saudi Arabia – in Oman in limestone, while in the Saudi Arabian desert they were in marble.

"In any case, these are old structures, perhaps one or two million years old," said Passchier. "We assume that they were formed in a slightly more humid climate, not in the dry desert climate that prevails today." However, the organism that caused these structures remains a mystery.

Endolithic microorganisms use rock as a basis for life

Microorganisms such as bacteria, fungi, or lichen are found even in inhospitable or remote corners of the Earth. So-called endolithic microorganisms are not uncommon in desert areas as they can obtain their energy and nutrients from the rocks they live in. "What is so exciting about our discovery is that we do not know which endolithic microorganism this is. Is it a known form of life or a completely unknown organism?" According to Cees Passchier, it must be an organism that can survive without light because the tubes have formed deep inside the rock. The researchers found biological material, but no DNA or proteins that could provide further insights.

Passchier hopes that specialists on endolithic organisms will look into this phenomenon in the future. "This form of life, of which we do not know whether it still exists, could be important for the global carbon cycle. It is therefore essential that the scientific community becomes aware of it." The release of carbon through the biological activity of microorganisms could also play a major role in the Earth's CO2 balance.

Publication in the Geomicrobiology Journal

Cees Passchier was Professor of Tectonophysics and Structural Geology at the Institute of Geosciences of Johannes Gutenberg University Mainz from 1993 to 2019. He has been Senior Research Professor in Geoarchaeology at JGU since 2019. The current research paper "Subfossil Fracture-Related Euendolithic Micro-burrows in Marble and Limestone" was published in the Geomicrobiology Journal.

Band of heavily eroded micro-burrows that had been exposed to the surface

Top view of an outcrop in Namibia showing the marble penetrated by a group of micro-burrows

Marble from Namibia in which micro-burrows have grown in parallel arrangement downwards from two fractures filled with calcrete


Landscape in Namibia with marble outcrops where the bands of micro-burrow were found

Credit

photo/©: Cees Passchier

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Scientists unite to save the planet’s glaciers




University of Cambridge




Glacial ice stores 70% of Earth’s freshwater, underpinning the food and water security of billions of people. But ice is at the frontline of the climate crisis. Even with the most ambitious goal of limiting global warming to 1.5°C, analysis suggests that up to half of the world’s 200,000 glaciers will disappear by the end of this century.

In response to the UN declaration of 2025 as the International Year of Glaciers’ Preservation and UN Decade of Action for Cryospheric Research (2025–2034), an international team of glacier scientists has formed the Glacier Stewardship Program.

“The demise of glaciers and the impacts of the associated rise in sea level are not restricted to one country,” said team member Professor Jerome Neufeld, from the University of Cambridge. “A truly international effort is needed to figure out how we can safeguard these resources.”

Every molecule of greenhouse gas makes more melting ice, so reducing carbon emissions is critical to help save glaciers. However, the scientists say reducing emissions alone is not enough.

“It is likely that even under the most ambitious emissions reduction scenario we will see the loss of many crucial glaciers,” said Dr Shaun Fitzgerald, Director of the Centre for Climate Repair at Cambridge.

“We need to explore potential options which could help protect them while we get greenhouse gases down to sustainable levels.”

This alliance of scientists will address three priorities to help address the challenges and consequences of glacier loss.

First, in cooperation with communities and stakeholders, the Program will systematically evaluate, test, and develop new technical approaches which may be appropriate to help slow ice loss at the local scale.

Second, it will seek to mitigate the impacts of glacier loss on the hundreds of millions who live in the shadow of mountain lands. The Program will transform the state of the art in early-warning systems to protect communities from glacier-linked hazards in some of Earth’s most perilous mountain ranges.

Finally, the Program will establish a unique biobank – a microbial zoo - to save glacier biodiversity for future generations and harness its genetic potential for mitigating consequences of climate change. As Earth’s largest freshwater ecosystems, glaciers harbour unique biodiversity, and are home to tens of thousands of microbial species.

The Glacier Stewardship Program is supported by scientists from Austria, Czech Republic, China, Denmark, Finland, France, Germany, India, Italy, Norway, United Kingdom, Slovenia, and Switzerland.