Category: 7. Science

  • In a first, enamel proteins 18-20 million years old from tropical, High Arctic sites unravel palaeobiology of extinct taxa

    In a first, enamel proteins 18-20 million years old from tropical, High Arctic sites unravel palaeobiology of extinct taxa

    If obtaining sequences from ancient proteins found in fossils was previously limited to samples no older than four million years, two studies published in the journal Nature on Wednesday (July 9, 2025) have pushed back this timescale to more than 20 million years. The enamel proteins from extinct mammals are a staggering ten-fold older compared with the oldest known ancient DNA that has been obtained so far. The studies have used proteins or peptides trapped within dense enamel of the mammal teeth to study palaeoproteomics and to obtain phylogenetic information of extinct mammals.

    One study is of enamel proteins from extinct mammal fossils from the Turkana Basin in Kenya, and the other study is of enamel proteins from extinct mammals in the Haughton impact crater site located on Devon Island, Nunavut in far Northern Canada.

    “The two papers have redefined the boundaries of biomolecular preservation in the fossil record,” says Dr. Niraj Rai, Head of the Ancient DNA Lab at the Birbal Sahni Institute of Palaeosciences (BSIP) in Lucknow, who is not part of the two studies. “These findings confirm that enamel — a highly mineralised and durable tissue that serves as an extraordinary molecular archive — is capable of preserving endogenous peptides far beyond the temporal limits of ancient DNA, which typically degrades within a million years.”

    If recovering evolutionary-informative protein sequences from samples 18 to over 20 million years old is by itself remarkable, recovering well-preserved protein samples of extinct mammals 18 million years old from the Turkana Basin in Kenya, which is a hot tropical site, is even more astounding. Unlike in cold climatic conditions, the possibility of finding well-preserved DNA and proteins dating back millions of years in one of the hottest regions in the world is slim. As a rule, molecular breakdown happens over time, which is exacerbated in a hot climate.

    A view of the Turkwel River in Turkana, northern Kenya, where the fossils from which ancient peptides were recovered are found.
    | Photo Credit:
    Daniel Green

    The second study is on protein samples encased deep within the teeth enamel found in fossil samples collected from the Haughton impact crater site located on Devon Island, Nunavut in far Northern Canada. The researchers extracted and sequenced ancient enamel proteins from a fossilised rhino tooth that are 21-24 million years old. They recovered partial sequences of seven different enamel proteins and over 1,000 peptides.

    A recent study of an ancient Egyptian who lived 4,500-4,800 years ago as well the two current studies on extinct mammals have relied on teeth samples to obtain genetic and phylogenetic information, respectively; teeth samples have turned out to be invaluable in preserving almost intact DNA and proteins. DNA found at the root tip of teeth of the ancient Egyptian allowed researchers to sequence the whole genome of the ancient man. Now, two separate teams have successfully used proteins encased within dense enamel of teeth of different mammals to interpret the biology and evolution of mammals that lived 18-24 million years ago in completely different climatic settings — frigid cold and hot tropics.

    Proteins not inferior to DNA

    Explaining that not just DNA but proteins too can reveal vital information about ancient animals, Dr. Timothy P. Cleland in an email to The Hindu says: “Proteins are translated from DNA so it can provide similar information. We can learn a wide variety of information from studying proteins from ancient animals.” Dr. Cleland, a Physical Scientist at the Smithsonian Museum Conservation Institute, Suitland, Maryland, and one of the corresponding authors of the East African Rift paper, cites the example of an enamel protein called amelogenin which has X-linked and Y-linked forms that can be used to estimate biological sex of the mammal being studied. The enamel proteins have more evolutionary information than collagen (for example) and can be used to evaluate the evolutionary relationships of fossil species beyond morphology alone, he says.

    Dr. Ryan Sinclair Paterson in an email says that he would not say either palaeoproteomics or palaeogenomic data is more reliable than the other, when it comes to studying living organisms. Dr. Paterson is from Globe Institute, University of Copenhagen, Copenhagen, Denmark, and the first and a corresponding author of the paper on the discovery of teeth enamel of Rhinocerotinae in the Haughton impact crater site, Nunavut in far Northern Canada. “Genomic data can have a higher resolution, and be more useful for finer aspects, particularly of relatedness amongst closely-related lineages. Proteomic data can also be very useful for resolving very deep splits in the tree of life, as they are thought to be less prone to convergence and saturation,” he says.

    Dr. Paterson further adds: “With these ancient proteins, while they lack the resolution of DNA, they still represent robust genetic sequence data, carrying mutations that can allow for sequence-based timetrees. I think that is the major goal of this type of palaeoproteomic study – filling in the tree of life across vast geological timescales using genetic sequence data.”

    Both teams extracted key structural enamel proteins, enamelin, ameloblastin, and amelogenin using advanced mass spectrometry and rigorous criteria to rule out contamination. Remarkably, diagenetic alterations once considered damaging, such as advanced glycation end-products and carbamylation in the Kenyan samples, or widespread arginine oxidation and peptide bond hydrolysis in the Arctic specimen, are now leveraged as hallmarks of authenticity, says Dr. Rai.

    “The study of enamel proteins from fossils has been an exciting area of research for the last several years, and has benefited from new extraction methods, improvements in mass spectrometry methods, and data analysis tools. We took advantage of all of these developments to find preserved proteins from mammal enamel from the Turkana Basin of Kenya,” says Dr. Cleland.

    The Turkana Basin has produced the richest record of mammal evolution in eastern Africa in the current geological era — the Cenozoic Era — spanning the last 66 million years. The researchers had examined protein fragments ranging from 1.5-million-year-old elephant fossils to 29-million-year-old fossils from Arsinoitheriidae, a family of extinct, rhinoceros-like ungulates. The Turkana Basin has been found to document the evolutionary origins and/or diversifications of key taxonomic groups of African mammals, such as proboscideans, rhinocerotids, hippopotamids and hominoids (great apes).

    View of the Haughton Formation near Rabbit Run creek on Devon Island, Nunavut. The dry, cold “polar desert” conditions helped preserve the ancient rhinoceros fossil found here, including traces of original proteins.

    View of the Haughton Formation near Rabbit Run creek on Devon Island, Nunavut. The dry, cold “polar desert” conditions helped preserve the ancient rhinoceros fossil found here, including traces of original proteins.
    | Photo Credit:
    Martin Lipman

    Shielding the embedded proteins

    Explaining how the proteins had escaped complete destruction during the last 18 million years despite the hot climate and diagenesis — the physical and chemical changes that occur during the conversion of sediment to sedimentary rock — at the Turkana Basin, Dr. Cleland says: “Because the proteins are essentially self-fossilised within the enamel mineral, they are protected from other environmental impacts that could lead to their loss.” Going further to explain how the enamel proteins are protected even for millions of years, he says: “Enamel is the hardest substance that animals produce and shields the embedded proteins from access to water or microbial impact, so it begins as a good place to find the preserved proteins.” The researchers had sampled the internal part of the enamel that is fairly thick in these species, so it is unlikely that protein from elsewhere would be deposited on the enamel.

    Despite building the study to have a range of ages from 1.5 million years to 29 million years to explore the preservation of enamel proteins across a long-time range, the researchers of the Turkana Basin in the East African Rift System were “surprised and excited to find proteins that retained evolutionary information all the way to 18 million years”.

    Though the hot climate is not conducive for protein preservation for millions of years, the Turkana Basin also has fluviodeltaic sediments, which might have led to swift burial of ancient animals, thereby resulting in relatively well-preserved fossil samples. The findings from the Turkana Basin also suggest that this could have been the case. “Relatively more proteins are found in some sites that we study, compared to others. For instance, we find an especially high number of peptides from fossils at a very old site, Buluk. Sedimentary data suggest that Buluk fossils were buried rapidly, and this may be why protein preservation is better there,” Daniel R. Green from the Department of Human Evolutionary Biology, Harvard University, and the first and one of the corresponding authors of the East African Rift paper tells The Hindu in an email.

    Swift burial may have played a role in preserving the proteins even in the case of the Haughton impact crater site located on Devon Island, Nunavut, where it was a lake. “Swift burial can help with preservation of bones and teeth under the right conditions. Specifically, we expect exceptional preservation when there is both rapid burial and low oxygen or anoxic conditions. There may have been some low oxygen conditions in the Haughton Lake, as mummified wood has been discovered. So, it’s possible that this contributed to the exceptional preservation. However, it is most likely related to the cool temperatures, specifically preservation in permafrost. Interestingly, a lot of bones from the Haughton Crater end up broken due to the repeated freeze and thaw of the permafrost. Some are also brought to the surface by this freeze and thaw action, making them easier to find,” Dr. Danielle Fraser from Palaeobiology, Canadian Museum of Nature, Ottawa, Ontario, Canada and one of the corresponding authors of the paper says in an email to The Hindu.

    The team has collected a large amount of data from all of these sites across northern Kenya, which includes information about ancient climatic conditions as estimated through Earth System Climate Models. “We have reconstructed vegetation and rainfall through soil chemistry analyses. And we can make inferences about ancient diets, behaviours, and evolutionary processes through the fossils themselves, and their stable isotope compositions,” says Dr. Green.

    According to Dr. Frazer, finding intact teeth, which are identifiable, is not surprising, given that there are teeth from mammals dating back many more millions of years into the Mesozoic. “What is exceptional, is that the proteins we recovered were complete and abundant enough to infer evolutionary relationships; these are, by about 10 million years, the oldest from which evolutionary information has been gleaned,” he says. “Specifically, we were able to test a hypothesis about the evolution of rhinocerotids (rhinoceroses and their extinct relatives), a group whose past diversity was much greater than today. What recovering such evolutionarily informative proteins from this fossil tells us is that we will be able to test many more hypotheses using many more fossils from the Arctic and, perhaps, challenge some other long-held evolutionary hypotheses along the way.”

    The Haughton Crater has been studied for decades to understand the depositional environment, the plant community, the date of the formation of the crater (based on several types of exact dating), the mammal fauna etc. “What we know is that the environment was fundamentally different from the modern Arctic, being much more temperate, and that the mammal fauna was unique, being a combination of species with North American and Eurasian affinities,” says Dr. Frazer.

    He is very hopeful that we will see evolutionarily informative proteins extracted from older [more than 24 million years] materials and expects them to be found in Arctic or Antarctic conditions, where they have been preserved in a “freezer” for many millions of years.

    The authors of the Haughton impact crater site located on Devon Island, Nunavut in far Northern Canada used the protein sequences to shed light on the divergence between the two main subfamilies of rhinos, Elasmotheriinae and Rhinocerotinae. Based on protein sequences, they revised the rhinocerotid phylogeny, showing that Epiaceratherium diverged prior to the Elasmotheriinae-Rhinocerotinae split, contradicting fossil-based models that suggested a deeper basal divide.

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  • Creating a Lidar-based Elevation Map of the Moon

    Creating a Lidar-based Elevation Map of the Moon

    ESA’s Moonraker lunar mapping mission will use a custom-designed lidar mapping payload by NUVIEW GmbH for landing site selections and broader scientific purposes.

    Micro- and small-satellite builder SFL Missions recently announced it was chosen to form part of a team led by geospatial technology provider NUVIEW GmbH to conduct a study for the Moonraker lunar mapping mission, a three-year wide-area mapping project of the lunar polar regions to aid mission planners in landing site selections.

    SFL Missions was chosen to become a member of the team for this study as their spacecraft have a great track record of on-orbit reliability and provide a best-in-class precision pointing capability, which is critical for the Moonraker mission. Moreover, SFL is developing NUVIEW’s technology demonstration satellite, so both companies were already working together on a similar mission.

    SFL’s contribution to supporting the Moonraker mission concept

    As part of the Pre-Phase A contract led by NUVIEW, SFL Missions is supporting the mission concept by contributing to transit trajectory analysis, orbit design, and satellite platform conceptual design for Moonraker. For Moonraker in particular, SFL is leveraging its largest lunar platform, the DAUNTLESS-L platform.

    The mission analysis examines launch options and trajectories for efficient lunar orbit insertion and assesses how orbital parameters affect spacecraft design and data collection. The system design addresses payload integration, spacecraft configuration, and subsystem sizing, with particular focus on ensuring the propulsion system has sufficient fuel for transit and maintaining orbit against lunar gravity perturbations. Additionally, detailed mission and system requirements are established to inform future design phases.

    Moonraker’s lidar payload

     The Moonraker mission will consist of a single orbiter operating in a low-altitude polar orbit around the Moon. The orbiter will host a lidar payload to capture highly accurate elevation points of the terrain that will be used to generate 3D elevation models for assessing and selecting  future landing sites.

    The payload will be a mapping lidar custom-designed and developed by NUVIEW for the Moonraker mission. It will leverage the heritage of the lidar payload developed for NUVIEW’s technology demonstrator. The wide-area lidar mapper will cover both polar regions, or about 5 M square kms. The enhanced, high-fidelity zoom lidar will be tasked to cover individual landing sites approximate 425 x 425 m squared. Moonraker will fly in a circular polar orbit with a 50 km (mean) altitude.

    Moonraker’s lidar data will also serve a broader scientific purpose, including scanning permanently shadowed regions for water ice and providing valuable insights into the Moon’s geological and interior composition.

    Selecting a lunar landing site

    There are many factors that mission planners consider when selecting a lunar landing site. First and foremost is whether the mission’s payload requires certain locations or environmental conditions to execute its scientific objectives. 

    Next is landing safety, which is the aspect Moonraker’s data will impact. Craters, boulders, and slopes can easily tip a lander. Given the extreme lighting conditions of the lunar poles and the relatively low resolutions of current digital elevation models (DEMs), safe landing sites are not guaranteed for lunar landers. Most landers today either land blindly and hope for the best, or they execute a hover maneuver over their landing site and scan it with a short range hazard detection and avoidance (HDA) lidar.

    If no safe landing site can be found, the lander needs to carry sufficient propellant onboard to divert to a secondary landing site and repeat the process. This carries substantial risk that no safe landing site can be found, which is especially critical for manned landers. Moonraker’s data will enable mission planners to identify hazards down to small boulders and craters (considered the smallest obstacles which could tip a lander) before their missions ever launch.

    Finally, there are other considerations such as length of the lunar day at the landing site latitude, thermal effects of the surrounding environment, and visibility of Earth for direct line-of-sight communications. 

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  • Warming climate, volcanos raise risk of ice falls on Chile's glaciers – Reuters

    1. Warming climate, volcanos raise risk of ice falls on Chile’s glaciers  Reuters
    2. Melting glaciers and ice caps could unleash wave of volcanic eruptions, study says  The Guardian
    3. Scientists warn hundreds of dormant volcanoes could soon erupt thanks to climate change  MSN
    4. Glacier retreat could lead to volcanic eruptions worldwide, including in Antarctica: Study  Down To Earth
    5. More great news about climate change: It’s also causing more volcanic eruptions  Fast Company

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  • China’s Chang’e-6 sheds first light on evolution history of moon’s far side-Xinhua

    BEIJING, July 9 (Xinhua) — A series of research findings by Chinese scientists on the samples collected by the Chang’e-6 mission from the moon’s far side have unveiled the volcanic activity, ancient magnetic field, water content and geochemical characteristics of the moon mantle, shedding the first light on the evolutionary history of its dark side.

    Four studies by the research teams from the Institute of Geology and Geophysics (IGG), the National Astronomical Observatories, both under the Chinese Academy of Sciences (CAS), Nanjing University, and other institutions were published in the latest issue of Nature.

    As the moon’s revolution cycle is the same as its rotation cycle, the same side always faces Earth. The other face, most of which cannot be seen from Earth, is called the far, or dark, side of the moon. This term doesn’t refer to visible darkness, but rather the mystery shrouding the moon’s largely unexplored terrain.

    The moon’s near and far sides exhibit significant differences in morphology, composition, crustal thickness and magmatic activities. However, the mechanisms behind these disparities remain unresolved, representing a key issue in lunar science. Previously, scientific understanding of the far side relied primarily on remote sensing studies, scientists say.

    In 2024, Chang’e-6 made history by bringing 1,935.3 grams of lunar far-side samples back to Earth. These samples were collected from the South Pole-Aitken (SPA) Basin, the largest, deepest and oldest basin on the moon, which provided a rare opportunity to clarify the compositional differences between the near and far sides and to unravel the long-standing mystery of their asymmetry.

    “The SPA Basin is one of the moon’s three major tectonic units, measuring approximately 2,500 kilometers in diameter. The energy from the impact that formed this crater is estimated to be 1 trillion times greater than that of an atomic bomb explosion. Yet, the exact influence of such a massive collision on the moon’s evolution has remained an unsolved mystery,” Wu Fuyuan, an academician of CAS and a leading researcher with the IGG, said at a CAS press conference on Wednesday.

    The four papers published in Nature systematically reveal, for the first time, the effects of this colossal impact, which is the core highlight of these findings, said Wu.

    Over the past year, Chinese scientists have achieved multiple pioneering breakthroughs through the study of the Chang’e-6 samples.

    They found the evidence of volcanic activity on the moon’s far side approximately 4.2 billion and 2.8 billion years ago, indicating such activity had persisted for at least 1.4 billion years.

    For the first time, scientists obtained the ancient magnetic field information from the far side of the moon, revealing a possible rebound in the moon’s magnetic field intensity around 2.8 billion years ago. This discovery indicates the presence of fluctuations in the driven power of the lunar dynamo.

    Scientists have found that the water content in the lunar far-side mantle is significantly lower than that of the near side, indicating a significant difference in water distribution between the two hemispheres.

    “We found that the mantle source of basalt from the SPA basin is extremely depleted in incompatible elements, which are commonly used to reveal the geological processes that rocks have undergone,” said Yang Wei, a researcher with IGG.

    This depletion could mean either the original lunar mantle was very low in the incompatible elements, or the massive impact event melted the rocks and carried these elements away. This discovery underscores the profound influence of large impacts on the evolution of the moon’s deep interior, Yang said.

    “The new discovery marks humanity’s first direct access to key evidence of the deep interior material properties on the far side of the moon. It provides us with unique information to understand how the moon’s early interior became layered, cooled and evolved, representing a crucial step toward unraveling the mystery behind the dramatic differences between the lunar near and far sides,” said Li Chunlai, a researcher at the National Astronomical Observatories of CAS and deputy chief designer of the Chang’e-6 mission.

    Additionally, Chinese scientists have made other discoveries. They unveiled the physical, mineralogical and geochemical characteristics of the Chang’e-6 lunar samples.

    Meanwhile, Chinese scientists precisely determined for the first time that the SPA Basin formed 4.25 billion years ago, providing humanity with a more accurate anchor point for studying the history of large-scale impacts in the early solar system.

    Mahesh Anand, a professor at the Open University in the UK, said, “We have had samples from the moon for over 50 years, samples collected by the Apollo and Luna missions. And we have many lunar meteorites.”

    “But there are lots of new findings that are coming out based on the work that has been done on Chang’e-6 samples that are actually turning many of the well established hypotheses and theories in the field of lunar science upside down, necessitating reexamination of many of those theories,” Anand said.

    He Hongping, vice president of CAS, said that upon receiving the Chang’e-6 lunar samples, CAS has placed high priority on related research efforts, and has yielded a series of high-level research achievements.

    Guan Feng, director of the Lunar Exploration and Space Engineering Center of the China National Space Administration, expressed the hope that the comprehensive development of space science, space technology and space applications will be further promoted, urging more scientists to make use of the extraterrestrial samples and scientific data obtained from China’s lunar and deep space exploration missions to achieve more results and make more discoveries.

    Previously, Chinese scientists analyzed the samples collected by the Chang’e-5 mission from the moon’s near side, and found evidence of young volcanic activity dating back just 2 billion years, extending the moon’s volcanic timeline by 1 billion years. This discovery was hailed by international peers as changing humanity’s understanding of lunar evolution.

    The success of China’s lunar exploration program is a prime example of the deep integration between science and engineering, said Li of the National Astronomical Observatories.

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  • First images from the Vera C. Rubin…

    First images from the Vera C. Rubin…

    Sarah Al-Ahmed:
    We’re exploring the dazzling new images from the Vera C. Rubin Observatory this week on Planetary Radio. I’m Sarah Al-Ahmed of The Planetary Society, with more of the human adventure across our solar system and beyond. Today, we explore the first public release of images from the Vera Rubin Observatory, and learn more about the powerful telescope behind them. Stephanie Deppe, a planetary scientist and astronomy content strategist at Rubin Observatory, joins us to explain how this revolutionary facility works, what these first images reveal, and how Rubin will transform our understanding of the universe over the next decade. Later in the show, we celebrate the Observatory’s namesake, Vera Rubin.

    Jess Soto, who’s the STEM Strategies Coordinator at Mount Wilson Observatory and founder of Science Women Shirts, shares how Rubin’s scientific brilliance and advocacy for women in science continue to shape and inspire future generations. And, of course, we’ll wrap things up with what’s up with our Chief Scientist, Bruce Betts, with a discussion of the third interstellar object ever discovered, Comet 3I/ATLAS. If you love Planetary Radio and want to stay informed by the latest space discoveries, make sure you hit that subscribe button on your favorite podcasting platform. By subscribing, you’ll never miss an episode filled with new and awe-inspiring ways to know the cosmos and our place within it. On June 23rd, 2025, the Vera C. Rubin Observatory released its first public images, offering a dazzling glimpse of the universe captured at an unprecedented scale.

    In just over 10 hours of test observations, the telescope imaged millions of galaxies and stars, and discovered over 2,100 never-before-seen asteroids. These are the very first images shared with the public, but behind the scenes, Rubin’s team has been hard at work for months, gradually bringing this next generation observatory into focus, fine-tuning the systems, and preparing for its official science mission. Perched high in Chile’s Cerro Pachón, the Rubin Observatory is the product of more than two decades of vision and engineering, jointly funded by the U.S. National Science Foundation and the Department of Energy’s Office of Science. Its state-of-the-art 8.4-meter telescope, and record-breaking digital camera, which is the largest humanity has ever built, will capture a dynamic time-lapse record of the universe, over a 10-year mission called the Legacy Survey of Space and Time. That survey is expected to reveal everything from dark matter and dark energy to asteroids, interstellar objects, and cosmic events that we haven’t even imagined yet.

    The release of these first images was a global event for space fans. More than 300 institutions, schools, and science centers around the world hosted watch parties for the image release. And Rubin isn’t just for scientists. With new tools like their SkyViewer and a dedicated Public Engagement platform, the observatory is bringing astronomical data on an unbelievable scale into classrooms, homes, and citizen science projects, making real exploration of the cosmos accessible to anyone with an internet connection. The observatory is named for Vera Rubin, the legendary astronomer who found the first convincing evidence of dark matter. We’ll learn more about her story and her legacy later in the show.

    But first, to talk about this historic image release and what’s to come, I’m joined by Dr. Stephanie Deppe, astronomy content strategist for Rubin Observatory. Stephanie is a planetary scientist, astronomer, and science communicator, and she’s one of the voices that are helping connect this remarkable observatory with the world. Thanks for joining me, Stephanie.

    Stephanie Deppe:
    Thanks for having me. I’m super excited to talk with you.

    Sarah Al-Ahmed:
    Well, this is a moment that’s decades in the making. Building an observatory of this size takes so much love and so much effort, and so much international collaboration. What was it like for you after all of that to finally get to see these images for the first time?

    Stephanie Deppe:
    Oh, man, it is so hard to put into words. I have seen kind of the end of all of this planning, and the lead-up, and the excitement from everybody who has been involved for decades, just getting so excited about the eminent release of these images and the turning on of the observatory. Yeah, the first time I saw the images, it was a really surreal experience. There are a number of times I’ve seen kind of first images, I guess. The first one was when we turned the Commissioning Camera on for the first time, and this is a smaller engineering test camera.

    And that was the first time that photons had ever come from space, bounced through the telescope’s mirror, and hit a camera detector. And so that was a really special moment that happened back in October of 2024. But the next kind of moment that all of this kind of felt like it was leading up to, and it’s kind of like the moment that everyone who has been working on Rubin for 20 plus years has been waiting for was what we call first photon, and it is the moment when the LSST camera, the big car-sized camera was turned on, pointed at the sky for the first time. That moment was a party. We kind of were narrowing in on the day it was going to be, but up until probably the week before, we didn’t know exactly what day it was going to be, because it just takes time to get everything into place and check all the boxes and whatever.

    And you’re assembling this huge facility, this telescope, this camera, like you’re putting all of these components together for the first time. And so you don’t know how it’s going to work until you plug things in and try to turn them on. And so finally, kind of a few days beforehand, we were like, “Okay, we’re pretty sure it’s going to happen on April 15th.” There was kind of like this buzz around all of the meetings that I was in, because everyone knew that it’s happening tonight, like we are turning this giant camera on, and there will be stars and galaxies visible in this camera for the first time tonight. And so they kind of last minute scrambled to put together a kind of staff-wide zoom room.

    So there were a bunch of people who were on site, but most people who work for Rubin are not in Chile. They’re in the U.S. or they’re elsewhere. Yeah, there were probably 200 people on the zoom room, plus probably another 100 people who were, throughout the various control rooms in person gathered. And we got the announcement like, “Okay, the shutter’s open. We’re taking the image.”
    And then like, “Okay, shutter is closed,” and we were all just like, “Where’s the image?” And then on zoom, everyone in the control room, who was actually physically there, just started cheering, and we were like, “We can’t see anything.”

    Sarah Al-Ahmed:
    “What’s happening?”

    Stephanie Deppe:
    So everyone on zoom was like, “We can’t see anything, but we know they can see something.” And so it was probably another seven seconds. It was the longest seven seconds ever, between that first year we knew that first image was on the screen in the control room, and when the rest of us online were able to see it. And then, of course, that first image was not in focus. It’s not going to be in focus the first time you put everything together and turn it on.

    It’s just not. It was pretty close, though. It was amazingly close, because the observatory … The telescope has laser trackers that help align everything without having to take an image, but it’s not exactly perfect. And so they took this image, and it was out focus, and everyone was all excited, like cheering, and then they were like, “Okay, now we have to work.”
    “We have to get it in focus,” and so they started taking successive images. And this camera is amazing, because it is 3,200 megapixels, which is a lot of pixels, and it reads out those 3,200 megapixels in two seconds. It is incredibly fast. And so they started doing kind of these iterations to bring the telescope into focus and bring the images into focus, and you take a 32nd exposure, wait two seconds, and you’re like, “Okay,” and mix into it.” So it’s really fast to do this sort of iteration, and within three or four minutes, it was in focus, which is amazing.

    Sarah Al-Ahmed:
    Well, this release was full of these just absolutely mind-blowing images. I cannot imagine what it would be like to be on the team after so much time working, and then finally, see these, that they’re … I don’t have words to describe what these are like, so I’m going to post them on the episode page for this episode so people can look at them themselves. But all of that was accomplished in 10 hours of test observations. How does that compare to what we’re going to be seeing when this thing is in full operation?

    Stephanie Deppe:
    Yeah. So I will say that the way that these first look observations, these first images, the way these observations were taken were a little bit different just in the sense that the goal was to create these beautiful images. And so we were very much focused on these two patches of sky, the Messier 49 Virgo Cluster region and the Trifid, Lagoon Nebula region. And so the way that those observations were captured is not exactly the same as how the observatory will operate in normal kind of science operations, but it also kind of was. So we have something that’s called a Feature Based Scheduler, which is a software algorithm that determines where to point the telescope next in the sky.

    And this is to really optimize the shutter time that’s open, the time that we have, the camera actually on sky. The software will map out the most efficient pattern to map out the sky based on where we’ve already covered, where clouds are in the sky, where the moon is. All of these different factors, they’ll take all that in, and be like, “Okay, the next best place to point is here. Go here.” And so that software was what drove these observations, but it was restricted to these specific areas rather than the whole sky.

    So that kind of mechanism for taking the observations was very similar to how Rubin Observatory will operate, but it was just restricted to these two smaller portions of sky. So ultimately, what we got in these 10 hours, for these two patches of sky was particularly for the Messier 49 Virgo Cluster region. It’s comparable to about five years of the full 10-year survey, is the depth that you’re seeing there. So we’re going to get more. It’s going to get even better, but that is kind of what you can expect from year five out of 10 of the whole survey.

    Sarah Al-Ahmed:
    What exactly is this survey going to be trying to accomplish, the Survey of Space and Time?

    Stephanie Deppe:
    It’s going to try to do everything, which is always a very ambitious thing to try to do. But the whole point of Rubin is really to see everything. It’s going to take these all-purpose images of the sky. It’s just going to look for the sake of looking, it’s going to record what it sees, and send that to our supercomputing data centers, and then the scientists will come in and sort through that data, and filter it, and curate the set of data that they need just for their specific area of science. And so the way I’ve heard it described, and I’ve kind of started describing it, is Rubin is not giving data to scientists, they are bringing scientists to the data.

    It’s a very fundamentally different way of doing astronomy. Scientists are not going to be downloading this data to their laptops. I mean, they might, but we’re talking like 20 terabytes of data every single night. You just cannot download that to a laptop. So everything’s going to happen on supercomputers in the cloud.

    So Rubin will get really precise data on galaxies and galaxy clusters, very distant galaxies. This will help us understand more about dark matter and dark energy, how the universe is expanding, how it clumps due to gravitational effects of everything that’s in it, and how those two kind of play together to shape the overall large-scale structure of the universe. Because Rubin is going to see everything, it’s also going to see a whole bunch of stars in our Milky Way. So Rubin is going to create the most comprehensive and precise map of the Milky Way ever generated. We’re going to see more stars than any previous observatory has been able to map in the Milky Way, which will help us understand the evolution, and structure, and history of our own galaxy.

    The part that I’m personally most excited about, I’m a solar system astronomer by training. Rubin is going to create the most kind of comprehensive inventory of the solar system that’s ever been generated. Currently, we know of about 1.5-ish million asteroids in the solar system, and Rubin is expected to discover up to another about four million than what we currently know, and so that’s going to give us a lot of information about what’s in our solar system, how did it get there, how did we get here, and just generally the evolution in history of our solar system. And then finally, the fourth kind of primary science driver of Rubin Observatory is looking out into the universe and seeing what changes, the changing, dynamic, transient sky. So the way that the Legacy Survey of Space and Time operates is we get a new snapshot of the entire Southern Hemisphere sky every few nights, about twice a week.

    And with that, you can essentially play a game of spot the difference every three to four nights. You look at the sky, and the next time you visit, you see what changed, and the next time you visit, you see what changed again. Rubin is going to be doing this over and over and over every night and essentially alerting the entire world about all of the changes it detects every night.

    Sarah Al-Ahmed:
    Just to give people an understanding of the camera on this thing, in last week’s show, we talked a little bit about the physical size of this camera. It’s like the size of a car. It’s huge. But this is the biggest digital camera ever built in the history of humankind. What makes this camera so special?

    Stephanie Deppe:
    There are a few things that make it pretty special. We actually have a couple of Guinness World Records for different parts of the camera. We’re in the Guinness Book of World Records for the largest lens ever made, which is literally human-sized. It’s about, I think five feet tall, which is … I mean, maybe relatively short human, but-

    Sarah Al-Ahmed:
    It’s like knee size.

    Stephanie Deppe:
    Yeah. I know, it’s huge. It’s giant. And the other really special thing about it is its focal plane, or that kind of grid of CCD detectors. There are 189 of them that are used for science, and then there are a few that are used for helping to focus in these other kind of fine-tune adjustments to make the image quality as good as it possibly can be. That focal plane, I believe is also the largest focal plane ever constructed, and so it’s like 60 or 65 centimeters across, which is also huge.

    Sarah Al-Ahmed:
    Yeah.

    Stephanie Deppe:
    Think of your handheld digital camera in the sensor that’s in your handheld digital camera, and then compare that to more than half a meter. It is really difficult to describe how substantial this camera is, how big it is.

    Sarah Al-Ahmed:
    If you could actually view the images that this thing is taking at max resolution on some giant high-definition screens or something, how many of these would it take to actually show a full image?

    Stephanie Deppe:
    If you wanted to display every single pixel using high-definition screens, you would need 400 high-definition screens, which would really go a long way in starting to cover the side of a building.

    Sarah Al-Ahmed:
    I love it when I just get to scroll through these giant images and see all the cool details, and as you said, like 20 terabytes of data every single night. What is the plan for managing this data and access for it so that people can get into it?

    Stephanie Deppe:
    Yeah. So Rubin Observatory is not just a telescope, it is a whole data management system with a community of scientists, who have been working for years and years to get ready for this data that is coming. So Rubin Observatory is the telescope, it’s the summit facility, but it’s also all of the data infrastructure that also had to be put into place to be able to get this data off of the camera, off of the mountain in Chile, and to our supercomputing centers. So the first place it goes is down the high-speed fiber-optic cables under the Pacific Ocean to the SLAC National Accelerator Laboratory in California. And there, we have what’s called the U.S. Data Facility, which is a big supercomputing center, and is also our primary data processing center.

    They process a little more than a quarter of all of the data that comes off of Rubin Observatory. They are the first kind of stop in the data processing pipeline. And SLAC is also where this nightly processing takes place. So every time an image comes off the camera at Rubin, within seven seconds, it arrives at the U.S. Data Facility in California. Then, within the next couple of minutes, it gets processed.

    So we were talking about how you compare these images from previous nights to the current image to find changes in the night sky. That is what happens during those next couple minutes. It scans all of these 3,200 megapixels, and it’s like, “Oh, there’s a change, there’s a change.” And it packages these … Identify changes up and sends them out to the world, as what are called alerts.

    And so these alerts are just literally going to be streaming from Rubin Observatory over the next 10 years, but that is what happens during those first couple minutes at SLAC, is identifying all of those changes and sending them out to the world. Then, it gets stored, and another set of processing that happens over the next 24 to 80 hours, where now that you have identified these changes, now you can start trying to identify what those changes are. So one of the things that will happen is the solar system identification. So which of these changes are actually objects that are moving from place to place on the sky? But they’re the same object.

    They’re just moving between different spots on the sky. And so that processing starts to happen after that initial two minutes. And we also send a copy to the France Data Facility. They are going to keep the copy of the raw data in France, and then there is also a data facility in the United Kingdom, that will … And between those three, those are what are the data facilities that are going to do a lot of the kind of big processing of all the images.

    We’re going to have these annual data releases, and that is going to require a lot more computational power. That’s like when you really crunch the numbers and combine all the data that you took over the last year to squeeze the most amount of science out of it, that takes a lot of computation power. And so between those three data facilities, that’s where that work is going to happen. Data are proprietary for two years to allow Rubin scientists and scientists who have access to Rubin data to be able to do their work, but then after those two years, after that proprietary period, the data becomes public, and anyone can use it.

    Sarah Al-Ahmed:
    We’ve spoken with people on the past, who were developing some of the systems that were going to be helping track objects in our solar system, and even in just the first 10 hours, this thing found over 2,100 asteroids, which is huge when it comes to planetary defense. There are a lot of things out there lurking in the dark, and I don’t want to panic people because we’ve found the majority of ones that are big enough to cause a Chicxulub style, destroy all life on earth situation, but there are plenty of things out there that come in and destroy a city, or, for example, something like Tunguska or Chelyabinsk, right? How would you envision this thing changing the game for planetary defense?

    Stephanie Deppe:
    Oh, it’s completely going to change the game. Rubin is going to find probably the majority of those kind of potentially threatening asteroids, the potentially hazardous ones. It’s going to find most of the ones that would do any sort of damage. I really come back to the saying like, “Knowledge is power.” We can’t do anything if we don’t know what’s out there, but if we know what’s out there, then we can start to formulate some sort of plan, if we do find something that does pose a threat.

    And so, I mean, really, the name of the game is just making sure we know everything that’s out there that could maybe pose a threat at some point in the future, because then, we have as much time as possible to be able to do something about it. Rubin is really going to fill in that gap in the Southern Hemisphere sky, and help us know even more what’s out there.

    Sarah Al-Ahmed:
    And then, we combine that with all of the amateur astronomers. I call them amateur astronomers, as if they aren’t completely professional in their ability to hunt for these asteroids, and then things like NEO Surveyor that we’re hoping to launch into space. If we combine all of this together, that’s going to give us the knowledge that we need because it’s just a numbers game. It’s a matter of time before something comes in. And with all of our innovations and things like DART, and hopefully with our observations of the upcoming asteroid Apophis, between all these things together, hopefully we can literally save the world, but you got to start with having the information.

    But something that I’m really interested in, because we’ve only detected two of these things, are interstellar asteroids. We’ve only found ‘Oumuamua and Borisov, and that was really difficult, but with this kind of data, do you envision that we’ll be able to spot a lot more of these objects that are coming in from outside of our solar system?

    Stephanie Deppe:
    Yeah. I mean, if they are passing through our solar system and are there to be found, Rubin is our best chance at finding them. We’ve only found two so far, so it’s really hard to make conclusive predictions with only two objects, but people have tried because that is definitely something that we’re very interested in. Interstellar objects are a really interesting way to be able to study other planetary systems directly. We can study their composition as they pass by, and compare that to what we see in our own solar system, and gain more knowledge about how planetary systems form and what they form from.

    And so these are really interesting and valuable objects, so the only way we have to study other planetary systems directly. However, we are kind of at the whim of whenever they pass by. We can’t really choose when one might pass us by, but if they’re passing through our solar system and exists to be found, Rubin is our best chance to find them. And I think that the current estimates are we’ll find somewhere around 10 interstellar objects over the next 10 years, about one a year, but again, it’s really hard to make really conclusive predictions, because we’ve only found two so far.

    Sarah Al-Ahmed:
    We’ve also spoken recently with Brown and Batygin, the team behind the search for Planet 9, and that’s a really challenging thing, given that this object, if it does exist, is so far away from the sun, so we’re dealing with low-light conditions and an orbit on the scale of thousands, if not tens of thousands of years. Even if we’re seeing the night sky over the course of 10 years, it might not move that much on the sky. Is it possible that this could help us find where it is if it exists?

    Stephanie Deppe:
    Totally. Yeah. I know. You always have to caveat with if it exists, but again, if it exists, I think Rubin is our best chance at finding it. The Planet 9 hypothesis comes from this set of objects.

    There’s multiple aspects to it, but the initial proposal was really inspired by the set of objects that were clustered. Their orbits were clustered in a very peculiar way, that you couldn’t explain unless something was essentially shepherding them into that configuration. But there’s been a bit of a debate over the last nine or so years on whether that is a real effect or whether that is due to the way that we observe the solar system from here on earth. And so Rubin is really, I think, going to break the … I don’t know if I want to call it a tie, but it’s going to, I think, be decisive one way or the other.

    So either it’s going to find more of these objects that support the Planet 9 hypothesis, or it’s going to find objects that refute it so that we no longer need a Planet 9 to explain what we’re seeing, or the third option is we find Planet 9 directly. So those are kind of the three outcomes that I see, but I think regardless of those three outcomes, we will answer the question of whether Planet 9 exists.

    Sarah Al-Ahmed:
    Well, I’m hoping that we can answer some of these big questions, and we need a telescope of this scale in order to help us do this, which is why I’m so excited that there are so many of these larger scale telescopes coming online. But I tell you, I was sitting there, staring at some of these images, just absolutely slack-jawed at their scale and detail. And I know this is an audio conversation, but I want to give people some idea of what these images were like. So let’s start with that image of the Virgo Cluster. What were we seeing in that field, and what really stands out to you scientifically?

    Stephanie Deppe:
    Yeah. So Messier 49 is the largest elliptical galaxy in the Virgo Cluster. So one of Rubin’s first images is centered on the southern region of the Virgo Cluster, which is the nearest galaxy cluster to earth. And what really stood out to me is just how full the images are. You are hard-pressed to find empty black space in that image.

    There are so many galaxies and so many things to see. There are 10 million galaxies in this image. And so anywhere you zoom in and you look, it’s just peppered with distant galaxies and small, faint smudges of galaxies. It’s just full. And that is really the story of Rubin and what it’s going to do.

    It’s just going to fill out what we know about the entire Southern Hemisphere sky. The whole Southern Hemisphere sky is going to look like that after Rubin. So I think for me, I mean, again, I’m really biased toward solar system astronomy. That is my science area of expertise. It’s what I love, but just the sheer …

    I was not prepared for the sheer number of galaxies, like the faint, tiny, little smudges that you see when you zoom in, I was not prepared for how many of those there would be.

    Sarah Al-Ahmed:
    It was like a reflection of that moment of the first time I saw my first Deep Field as a kid, and the first time someone explained that to me, just even as a child, feeling this deep, upwelling of emotion, of this understanding of just like how tiny we are and the scale of the universe, and how special it is that we get to be here and look out at all of that, it just fills me with this absolute awe and this gratitude that we get to be here to see all of this, after all this time of humanity, trying to understand the universe. It is just unbelievable what we’re going to learn.

    Stephanie Deppe:
    Yeah. I mean, as Carl Sagan said, “We are the universe, trying to understand itself,” and I think there is something so beautifully poetic about that. And I’m reminded of that every time I pull up our images, any images from a space telescope, really, but our images to just the sheer number of galaxies. Every one of those galaxies has billions of stars, and so it’s really special to be here at a time when we can do this sort of thing.

    Sarah Al-Ahmed:
    And that other image of the Trifid and the Lagoon Nebula, I mean, it by itself is a stacking of like 678 separate images. How are these stacked and processed together? People do this on a lot of smaller scale telescopes, but this is like a lot of data.

    Stephanie Deppe:
    Yeah. Processing images of that scale really does push whatever system you’re trying to do that on, because these images are so huge. You can actually go download the full resolution version of these images from our website. We’re talking tens of gigabytes, though. So I don’t know if you’ll be able to open it with any program on your computer, but you can download it and have it if you’d like.

    But it was an enormous weeks-long effort to produce just these two images, and one of them, the M49 Virgo Cluster image was actually produced with our scientific processing pipelines that were tuned in such a way to make this really aesthetic, beautiful image of this region of sky. You don’t usually need to put that sort of effort into an image that you’re only using for science, but if you really want it to be really beautiful, there’s a lot of extra fine-tuning that needs to happen in order to accomplish that. And it was just an absolutely heroic effort by dozens of people to make these two images for the world. I am in awe of the people who made these happen.

    Sarah Al-Ahmed:
    We’ll be right back with the rest of my interview with Stephanie Deppe after the short break.

    Bill Nye:
    Greetings, planetary defenders, Bill Nye here. At The Planetary Society, we work to prevent the earth from getting hit with an asteroid or comet. Such an impact would have devastating effects, but we can keep it from happening.

    Bruce Betts:
    The Planetary Society supports near-Earth object research through our Shoemaker NEO grants. These grants provide funding for astronomers around the world to upgrade their observational facilities. Right now, there are astronomers out there finding, tracking, and characterizing potentially dangerous asteroids. Our grant winners really make a difference by providing lots of observations of the asteroid so we can figure out if it’s going to hit earth.

    Bill Nye:
    Asteroids big enough to destroy entire cities still go completely undetected, which is why the work that these astronomers are doing is so critical. Your support could directly prevent us from getting hit with an asteroid. Right now, your gift in supporting our grant program will be matched dollar for dollar, up to $25,000.

    Bruce Betts:
    Go to planetary.org/neo, N-E-O, to make your gift today.

    Bill Nye:
    With your support, working together, we can save the world. Thank you.

    Sarah Al-Ahmed:
    You don’t necessarily have to download the whole thing in order to interact with it, thankfully. One of the tools that came out with this release was a SkyViewer, that can help people actually comb through this. How can, people who just want to look through it, but also people who are trying to share space with people, use these tools to dive into these images?

    Stephanie Deppe:
    From the very start, we knew that Rubin images were going to be giant, and really unwieldy, and difficult to work with for a regular laptop. The whole way that the Rubin Observatory science community, the data processing, everything is designed around the fact that you won’t have to download these giant data sets. And that’s true for the images too. The images are giant and huge, both in terms of number pixels and in just this sheer data volume. So SkyViewer is our tool where you can interact with Rubin images without having to download anything.

    You can download your view if you would like. If there’s a particularly beautiful area of sky and you’re like, “I want this as my new desktop wallpaper or my phone background,” anything like that, we have a really easy built-in way to download your current view, but the point is to make these giant images available at full resolution without you having to download them. This is our way for you to be able to work, or explore, or experience these huge images without totally crashing your computer when you try to open it.

    Sarah Al-Ahmed:
    I’ve also spoken in the past to some of the people on the Chandra team, who decided they were going to sonify some of their images to help them be shared with the world. There are a lot of people who might not be able to see these images or want a new way to interact with them. How do you see these visual and audio tools helping people connect with these Rubin images?

    Stephanie Deppe:
    One of the things we really wanted to do for these first images was also have a way to interact with them, not with site. That was really important to us, and the way we went about designing the experience … So SkyViewer also has a sonification version of it. We call it SkySynth, and this is that Virgo Cluster image, but conveyed via sound. It’s also conveyed via images for those who are sighted, who want to interact with it, but we really wanted to recreate the experience of being faced with this huge image of the Virgo Cluster and just exploring, just almost losing yourself in it.

    There are so many places where you can zoom in, and pan, and find something new, and no two people are going to have the same experience, exploring these images, and we wanted to recreate that for the sonification as well. We really wanted to create an experience where no two listeners would have the same experience, because that is visually also in the visual version of these images, what you’re getting. So the sonification piece of SkyViewer is essentially a random walk, so it kind of sticks you. You start in one area of the image, and there are two layers of sound that happen. The first is we have a central focus area, where the average color and average brightness within that focus area sets the pitch and the volume of kind of an underlying hum almost.

    It’s like a continuous tone, and then the central focus area kind of goes on a random walk around the image. It just kind of drifts around the image, similar to like if you were a sighted person interacting, and you were just kind of free-form exploring. The sonification goes on this random walk. As stars and galaxies enter the central focus area, they play as distinct notes. So galaxies will sound like harps, and stars sound like chimes.

    And so as galaxies and stars enter this focus area, you’ll hear harps and chimes sounding. Those are also like redder notes, correspond to lower pitch for those as well. So you have this really multi-layered soundscape happening. My favorite thing to do is to leave it open in a tab in the background and just let it play as background music, because it’s really relaxing, I find. But yeah, you have these kind of two layers, this underlying ambient tone, and then the individual notes from the stars and galaxies as they come into view.

    Sarah Al-Ahmed:
    Are there going to be opportunities for community or citizen scientists to get involved with this data?

    Stephanie Deppe:
    Absolutely. That is a huge effort that specifically the Rubin Education & Public Outreach team has been preparing for. So one of the things that our team has been working on is setting up all of the infrastructure needed for our scientists to very easily set up citizen science projects. So again, one of the complications with Rubin data is it it’s so huge, that you can’t just download this data, and then upload it to whatever your citizen science project platform of choices. We’ve partnered with the Zooniverse to do citizen science.

    But again, the fundamental issue was Rubin produces so much data, that you can’t download it, and then upload it to, for example, the Zooniverse. So what our team has done is cut out that download step. So our scientists who want to create a citizen science projects just say, “I want this data to go to Zooniverse,” and then it just happens, and you can set up these Zooniverse projects. And so we actually have a couple that are coming out very soon. Actually, by the time the show airs, it might already be out and done, because we expect a lot of attention on this first project, for sure. So sorry if you missed the first one, but there’s going to be lots, lots more citizen science projects, including additional data for this one that maybe you missed.

    Sarah Al-Ahmed:
    I love Zooniverse projects.

    Stephanie Deppe:
    Yeah. Well, it is.

    Sarah Al-Ahmed:
    I’m definitely one of those people that spends my extra time just clicking through Zooniverse projects.

    Stephanie Deppe:
    Yes, we will have a lot of citizen science projects on Zooniverse, I think. There’s going to be a lot of data that you just need human eyes and that kind of volunteer effort to be able to sort through all that data and really get the science that you need. There’s just some things that computers can’t do, and you need humans for it. So citizen science is going to be a huge, huge part of science with Rubin.

    Sarah Al-Ahmed:
    So what comes next for this telescope after the commissioning phase is done? What last steps do we have to do before it goes into full science operations?

    Stephanie Deppe:
    Yeah. So right now, the observatory is in what’s called science verification. And so we are kind of closing out this … It’s a bit of a blurry line between commissioning and science verification, but we are now transitioning from the, “Okay, we’ve turned everything on, and now we’re making sure it works together” to, “Okay. Now, we’re making sure it works well.”
    And so that is the phase, I think, we’re in now, is that verification phase that like, “Okay, here are the data sets we have identified to verify that.” From a science perspective, the observatory is working as well as it should. And then, we’re looking at kind of end of 2025 is when this big ten-year survey is going to start. So it’s coming very, very soon.

    Sarah Al-Ahmed:
    And how are you going to be collaborating with other observatories, because I know already the people at the large Magellan Telescope are ready to kick into high gear?

    Stephanie Deppe:
    Oh, yeah. Yeah. Well, the power of Rubin is really, its ability to see everything in detail and repeatedly. And so Rubin is really a discovery machine. It’s going to make a whole lot of discoveries that people are going to want to follow up, and we will get some of that follow up from Rubin just because of the nature of the survey.

    It’s going to be back at that same place in the sky three nights later. But the real power of Rubin and the way that it’s going to really powerfully work with a lot of other observatories is by providing those initial discoveries, those alerts, those like, “Hey, we’ve never seen this before,” and then providing that information so that other telescopes around the world can go follow that up for more information, or more data, or different kinds of data. Rubin Observatory is an optical imaging observatory, so if you want more data about kind of the different wavelengths of light, like with spectroscopy, that’s going to have to come from a different telescope because Rubin is only imaging. It has an imaging camera, or if you want information in different wavelengths, that’ll be a different telescope too. But in order to study something in detail, you have to first know that it exists, and so that’s what Rubin is going to do, is tell the world, “Hey, here’s what exists. Now, go follow it up.”

    Sarah Al-Ahmed:
    Well, this observatory is named for Vera Rubin, who helped uncover dark matter. And we’re going to be talking more about her life and her legacy in our upcoming segment, but what do you think she would make of this moment in history and this beautiful observatory that is her namesake?

    Stephanie Deppe:
    I like to think that she’d be proud of us the way that we’ve designed the observatory, the way that we have very intentionally made choices to bring in more scientists who maybe have not had access to this type of astronomical data before. We have a lot of folks who are at smaller institutions, who this is going to be game-changing for a lot of them, because we are the ones who are hosting the data. We are taking the data. All you need is an internet connection, a browser, and curiosity, and you can tap in and use this data for your own science. And so the way that we have designed the whole observatory is really about opening access to the incredible science that is going to come out of this. And I like to think that she’d be proud of us for where we’ve gotten.

    Sarah Al-Ahmed:
    And hopefully we can learn more about the secrets of dark matter and dark energy just as much as all the awesome planetary science we’re about to do. My gosh.

    Stephanie Deppe:
    Yeah. I mean, the initial name of Rubin Observatory when it was very, very first proposed to just a sketch on a piece of paper was the Dark Matter Telescope, so it’s very fitting and very full circle that our namesake provided the first convincing evidence for dark matter. It’s all full circle.

    Sarah Al-Ahmed:
    Really? Well, thanks for joining me, Stephanie, and sharing all of this, and seriously, good luck to you and the entire team as you go forward. You’re going to be providing the space community just such a wealth of knowledge, just a beautiful asset that we can use to learn more about our universe for decades to come, and it will take us decades to go through all of this data. So seriously, thank you for everything you guys have all done.

    Stephanie Deppe:
    Yeah. I mean, there’s a whole generation of people who’s really going to grow up with Rubin Observatory. Rubin Observatory is going to be the data set for generations, and I cannot wait to see all of the discoveries that come out of it.

    Sarah Al-Ahmed:
    Thank you so much.

    Stephanie Deppe:
    Thanks.

    Sarah Al-Ahmed:
    While the Vera C. Rubin Observatory represents the future of astronomy, its name honors a scientist whose work fundamentally reshaped our understanding of the universe. Vera Rubin was born in 1928, and passed away in 2016. She found the first convincing evidence of dark matter after it was first suggested by astronomer, Fritz Zwicky, but her impact extended far beyond her research. She believed science was for everyone, and spent her life working to make that a reality. Rubin didn’t just break barriers, she worked to remove them.

    She challenged hiring committees, called out conference organizers who excluded women, and used her influence to elevate others. She insisted on inclusion, not just as a value, but as a prerequisite for good science. Known for her warmth and humility, she mentored countless students and colleagues, often going out of her way to ensure young scientists, especially women, felt seen, supported, and empowered. She also raised four children, all of whom earned PhDs in science and mathematics, which is a powerful reflection of the way that she nurtured both curiosity and resilience. Much of Rubin’s groundbreaking work was done at observatories across the American Southwest, including Kitt Peak, Lowell Observatory, and Palomar, where she became the first woman officially allowed to observe.

    She spent the bulk of her career with the Carnegie Institute for Science, whose support was instrumental to her research. One of Carnegie’s earliest sites was Mount Wilson Observatory, which is visible on the mountain over our headquarters in Southern California. Vera fought to get data access for women at the observatory in a time when we were still excluded from using the telescopes directly. Our next guest, Jess Soto, is the STEM strategies coordinator at Mount Wilson Observatory, a long-time educator at Griffith Observatory, and the founder of Science Women Shirts. She joined me at Planetary Society HQ to reflect on Vera Rubin’s life and the lasting impact of her work. Thanks for joining me in our studio, Jess.

    Jess Soto:
    Thanks for having me.

    Sarah Al-Ahmed:
    I know you’ve been on the show before, but you also run a small company. You want to honor the legacy of women in science, and now, we, for the first time, have a telescope, an observatory named for a woman in science.

    Jess Soto:
    Yes, it’s really exciting. Vera Rubin, right? So what an exciting person to celebrate because her accomplishment was so relevant to astrophysics and just some revolutionary changes and concepts on how we saw galaxies in the universe, and just certain things that were invisible that she brought to light, so to speak.

    Sarah Al-Ahmed:
    What were some of the things that Vera Rubin did that led to this discovery, this idea that dark matter was a thing, because now, that’s something we just kind of accept in astrophysics, is a huge pillar of what we try to research.

    Jess Soto:
    Right. So she was really interested to see how galaxies work, and contrary to the popular belief that in the middle, there must be the most mass, and so everything falling outwards should be rotating less fast. That’s the thing that she pretty much proved to be wrong, and especially with spiral galaxies. It turns out that everything is moving sort of at the same speed, even on the outskirts of galaxies, which proves that there must be mass, and come to find out it’s dark matter.

    Sarah Al-Ahmed:
    It was a time when there were limited opportunities for women to do this kind of research, and she was very discouraged even early on from going into this field. What were some of the things that she had to overcome?

    Jess Soto:
    Her physics teacher, I believe one of her first physics teachers even told her, “Good luck.” “Just as long as you stay away from science,” I believe was something along the lines of how he sent her off. When she was excited and told him that she got accepted to Vassar, that was what he reciprocated, and that was a little discouraging, and I think it kind of geared her away from her love for physics. She wanted to apply to Princeton, but Princeton wasn’t accepting women, so they also pretty hastily, as she put it, rejected. I’m pretty sure they regret that after.

    Sarah Al-Ahmed:
    I hope they do. Really though, the number of things that she had to face during that time, I’ve met some women in science who’ve had some really difficult times, and it made them really thick-skinned and kind of off-puttish, almost confrontational when they’re trying to deal with other people.

    Jess Soto:
    Absolutely.

    Sarah Al-Ahmed:
    But Vera instead, took that energy and tried to do what she could to welcome as many people as she could into science.

    Jess Soto:
    Yeah.

    Sarah Al-Ahmed:
    What did she do for women and underrepresented groups in science during that time?

    Jess Soto:
    So from my understanding, even from folks that I know that had the privilege of working with her, she seemed to be kind of wise beyond her years. She definitely fought for women to have an equal opportunity and to be seen as folks that men can collaborate with. I don’t know if you heard about the bathroom skirt incident in the-

    Sarah Al-Ahmed:
    Yeah.

    Jess Soto:
    Yeah, the skirt. I don’t know if I’m phrasing that right, but over at … Oh my gosh, what observatory was that? Was that at Palomar?

    Sarah Al-Ahmed:
    Oh, I think that’s right, actually.

    Jess Soto:
    Yeah, where there was no restroom for women, so she cut out a skirt, or not an actual skirt, but something like a piece of paper or something, and placed it on top of the little man sign on the bathroom and said, “There. Now you have a women’s bathroom.” It’s one of those things that she was in the thick of, during a time, when women were starting to really be a part of the science. And as you could see, it was decades of a journey for many women in science, from Katherine Johnson to all the way back to the Harvard computers, which were really astronomers. They mapped the entire celestial sky. So it’s really crazy to me to see that even in her time by the ’60s, ’70s, she was still fighting the good fight, so to speak.

    Sarah Al-Ahmed:
    And so many of the women that you just named are women that you’ve tried to honor through your T-shirt line.

    Jess Soto:
    Yeah.

    Sarah Al-Ahmed:
    Why is it so important for you to share the stories of these women, so much so that you are willing to take this, veer off into a side project and try to represent them on shirts that people can wear?

    Jess Soto:
    Yeah, because I think it’s exciting when you go into a store and you see certain legends, so to speak, represented like Einstein, and that’s a common one that you see in most gift shops at museums, or Nikola Tesla, but there are so many that we are recognizing now that just were forgotten, and they contributed in ways that were just as important to science, and as like Tesla and Einstein, Henrietta Leavitt that I mentioned, discovered the star that ultimately helped us have a cosmic yardstick and led to the discovery of the universe outside of our Milky Way galaxy. Katherine Johnson got us to the moon, and back successfully, safely. I mean, these are things that are just overlooked, in my opinion, and all too often forgotten. Cecilia Payne, Annie Jump Cannon, and Vera Rubin is up there with all of them as well, and it’s exciting because these are women that, I think, are just now getting that kind of recognition more than ever, and I’m proud to be a part of that time, so I figured, “Why not help? Why not let anybody who wants to wear a shirt that mentions their name, help them become a common household name like Einstein?”

    Sarah Al-Ahmed:
    But despite all of that progress, we are in a time where opportunities in science are really shrinking due to budget cuts. But also, and I think Vera Rubin is a very concerning example of this, we’re in a time where diversity, equity, and inclusion programs are trying to be removed by the government, and mentions of it on government websites are being removed. And we got reporting from both ProPublica and Space News earlier this year, that they were going through the NASA websites about Vera Rubin, and removing bits of her history about the way that she mentored women and tried to open up opportunities for them at institutions. In that context, what kind of wisdom do you think we can take from Vera’s story? What do you think she would say to us in this moment?

    Jess Soto:
    Oh, that is a really good question. I would think it doesn’t define us. It doesn’t truly define us as a people in science right now. I think that a lot of people do not agree with this situation. It’s something that we have to keep fighting, unfortunately.

    And so I think we just need to kind of stand our ground and just continue to really focus on the science and do what we can in order to stand up for women, because it is just one entity and a very powerful entity. We all love and are grateful for NASA, but I think that we live in a different time, and it really actually misrepresents us as who we are. We are inclusive, we have diversity, and that’s not something that is really going to change just because they’ve removed the past. What do you think she would say?

    Sarah Al-Ahmed:
    She’s given some really good speeches and was very passionate about the idea that every person can make a difference, and that you need to push past these barriers and just keep striving. I mean, what an inspiring woman. I can only think that if she could do it in those times, we can lift each other up now.

    Jess Soto:
    Exactly. I love that. Nothing ever geared her away from being who she genuinely is, and her legacy of being the mother of dark matter is not the only thing that she’s really known for in science today. She’s known for being all inclusive for being fair, for just really being kind to everyone, and that’s something that obviously, although it’s a personal character, has played into her professional career, so I think that’s wonderful.

    Sarah Al-Ahmed:
    And now, we have this beautiful observatory that’s going to be looking at the sky and helping us to unravel the mysteries of the questions, but also give data access to people all around the world who might not have had it otherwise.

    Jess Soto:
    Yeah.

    Sarah Al-Ahmed:
    It’s a perfect namesake.

    Jess Soto:
    It’s amazing. Yeah, it’s really great.

    Sarah Al-Ahmed:
    Well, thanks for joining me and for sharing some of her story, and for doing what you can to share the stories of these women that have uplifted so much of us in science. I don’t think either one of us would be here without them.

    Jess Soto:
    That’s right. Yeah. Thank you for that. Thank you for helping me get the word out there too, and to remember these incredible women.

    Sarah Al-Ahmed:
    Here’s to Vera Rubin and all of the people who open the doors for people like me, Jess, and Stephanie. May we honor their legacy with awesome science forever. Strangely, just after I finished speaking with Stephanie Deppe at Rubin Observatory, and its potential to detect things like interstellar objects, wouldn’t you know it? A new one was discovered. 3I/ATLAS is the third known object to enter our solar system from interstellar space.

    This discovery was reported on July 1st, 2025, by the NASA funded ATLAS survey telescope. That’s the Asteroid Terrestrial-impact Last Alert System, which is also located in Chile. There have been two previously detected interstellar objects you might remember, the mysterious asteroid called 1I/’Oumuamua, and the more comet-like 2I/Borisov. Like Borisov, 3I/ATLAS appears to have a tail, which is fueling excitement among astronomers that are eager to study its composition. Now, let’s check in with Dr. Bruce Betts, our chief scientist for What’s Up? Hey, Bruce.

    Bruce Betts:
    Hey, Sarah.

    Sarah Al-Ahmed:
    Ah. Now, I swear I did not do this on purpose, but as I was talking to our guest this week about the Vera Rubin Telescope, I asked her whether or not it was going to help us find these interstellar objects, and then literally, a few days later, here comes the third interstellar object we’ve ever discovered. Can you tell us a little bit about this object that we found?

    Bruce Betts:
    Yes, 3I/ATLAS, the three for the third interstellar object found. So it’s come off from elsewhere in the galaxy and comes zipping through it. Anyway, it’s big, it’s out there, it’s not going to hit us, and it’s interesting because it comes from elsewhere in the grand universe, elsewhere in the galaxy, and it’s flying through our solar system. And you can tell it’s coming through because it’s got this high-speed hyperbolic orbit speed that you plot it backwards, it leaves the solar system, you plot it forwards, it leaves the solar system, so don’t get attached.

    Sarah Al-Ahmed:
    Some of my favorite comments online are about the direction it’s coming at us from, because it’s coming from Sagittarius, which is kind of where the center of our Milky Way galaxy is from our perspective. So people are making all these stories like, “It’s coming at us from the galactic core.”

    Bruce Betts:
    Just because it’s coming from kind of that direction, we’re 27,000 light years from the galactic core, but maybe. And yes, it is, and it’s awesome.

    Sarah Al-Ahmed:
    If people want to see this object, is it something they can actually see through their telescopes?

    Bruce Betts:
    I think it’ll be a tough object to see if you don’t have a fairly nice, advanced amateur telescope. You’re certainly not going to see it with just your eyes. You’re going to be probably beyond the binoculars. If you’re in an astronomy organization, astronomy club, you probably can do it. If you aren’t, you probably can’t, but I’m not totally sure, and still, it falls now into the realm of predicting the brightness of comets, which is notoriously like predicting the action of, I don’t know, a drunk cat.

    A cat should never be drunk. That was just important safety tip.

    Sarah Al-Ahmed:
    Well, that’s pretty random. What’s our Random Space Fact this week?

    Bruce Betts:
    Random Space Fact …

    Sarah Al-Ahmed:
    That’s the drunken cat.

    Bruce Betts:
    Yeah. So flying discs, flying saucer, I’m going to talk about these today. But what I’m talking about is what’s now called a Frisbee or a flying disc. When it was first put forth and started to be a little bit mass-marketed, it was originally known not as the Frisbee, but as the Pluto Platter. Yes, that Pluto.

    And in fact, it had names of all the planets around the outer edge of the disk and kind of had a sci-fi flying saucer look to it. And then, when the rights were sold to Wham-O, Wham-O, they ended up naming it Frisbee because of pie tins and a company named Frisbee, and you can look all that up. But the point is they still marketed it with the Pluto Platter initially, and then somewhere in there, they removed the names to get better aerodynamics, and then they just switched the name over to Frisbee, but it had an origin in the land of the solar system naming. My dog loves them wherever they came from. All right, everybody, go out there, look in the night sky, and think about flying discs, Frisbees and Pluto Platters, and what you would serve on a Pluto Platter. Thank you, and good night.

    Sarah Al-Ahmed:
    We’ve reached the end of this week’s episode of Planetary Radio, but we’ll be back next week to share our show’s creator, Mat Kaplan’s first Zero-G flight. Thanks to Space for Humanity for making the dream finally come true. If you love the show, you can get Planetary Radio t-shirts at planetary.org/shop, along with lots of other cool spacey merchandise. Help others discover the passion, beauty, and joy of space science and exploration by leaving your review and a rating on platforms like Apple Podcasts and Spotify. Your feedback not only brightens our day, but helps other curious minds find their place in space through Planetary Radio.

    You can also send us your space thoughts, questions, and poetry at our email at [email protected], or if you’re a Planetary Society member, leave a comment in the Planetary Radio space in our member community app. Planetary Radio is produced by The Planetary Society in Pasadena, California, and is made possible by our members from all over the world who believe that space is for everyone. You can join us as we celebrate the advancement of space science and the people that make it happen at planetary.org/join. Mark Hilverda and Rae Paoletta are our associate producers. Casey Dreier hosts our monthly Space Policy Edition, and now announcing Mat Kaplan as the host of our new monthly book club edition of Planetary Radio.

    More on that next week. Andrew Lucas is our audio editor. Josh Doyle composed our theme, which is arranged and performed by Pieter Schlosser. And until next week, ad astra.


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  • Nature retracts paper on novel brain cell type

    Nature retracts paper on novel brain cell type

    Over the objections of the authors, the editors of Nature have retracted a 2022 paper on the cellular origins of medulloblastoma after an independent team’s reanalysis questioned the paper’s key findings. The reanalysis was published as a Matters Arising article today in Nature at the same time as the retraction notice.

    The 2022 paper, led by Q. Richard Lu, professor of pediatrics at Cincinnati Children’s Hospital Medical Center, identified a previously unknown transitional cerebellar progenitor (TCP) cell type via single-cell sequencing of human fetal cerebella. Single-cell profiling of medulloblastoma samples showed a “substantial increase in the proportion of transitional TCP-cells,” suggesting that these cells could be involved in cancer development, the authors wrote in the paper. The work has been cited 27 times, according to Clarivate’s Web of Science.

    This cell type may not exist at all, though, according to the reanalysis, which was led by Paul Northcott, a faculty member at St. Jude Children’s Research Hospital. The team could not find evidence of the cells in an independent cerebellar atlas, and they detected the proposed marker genes for TCP cells—HNRNPH1, SOX11 and CTNNB1—“in similar proportions of both TCP and non-TCP cells” in Lu’s original atlas, Northcott and his colleagues wrote in their paper.

    What’s more, the purported TCP cells in the 2022 study had “a low nuclear fraction of detected transcripts” and low unique molecular identifier counts, which are “consistent with ambient RNA contamination predominantly contributed by a single donor,” the reanalysis says. Northcott did not respond to multiple email requests for comment by the time of publication.

    The retraction notice states that “concerns that there was insufficient evidence for the transitional cerebellar progenitor (TCP) population were brought to the attention of the editors” after the publication of Lu’s paper in 2022. Post-publication peer review cast “doubt on a key novel conclusion of the paper,” leading to the retraction, the notice says.

    Lu says he and the other authors of the original paper do not agree with the findings of the Matters Arising article or the retraction by Nature. The dispute over his work falls “within the realm of scholarly norm” but does not rise to the level of needing a retraction, Lu says, adding that his comments on this matter represent his personal view and not that of his employer. “I really believe this is a debate, not an error we made,” he says.

    L

    u says Nature informed him of the Matters Arising article disputing his findings in April 2023. He and his colleagues then did further experiments and analyses and submitted a Reply to the Matters Arising paper for publication in Nature. In November 2024, though, he says, Nature informed him that it would not publish the Reply and planned to retract the 2022 paper. Lu posted the Reply as a preprint on bioRxiv last month.

    The preprint suggests that the independent cerebellar atlas does verify the existence of TCP cells. Lu and his co-authors analyzed the same atlas as Northcott’s team and identified cell types highly enriched in SOX11 and HNRNPH1, which “corroborates the presence of a TCP-like population,” according to the preprint.

    And when Lu’s team reanalyzed their original dataset using a more stringent data cutoff to exclude ambient RNA contamination, they still concluded that the TCP cells “possess a distinct transcriptional identity characterized by a set of significantly enriched marker genes,” the preprint says.

    Last month, Lu filed a complaint with the Committee on Publication Ethics (COPE) to ask the committee to conduct an independent review to determine if Nature “followed COPE guidelines and best editorial practices” during this process, he wrote in the letter. There is not “clear evidence” of an error that warrants retraction, Lu says, adding that he would retract the study if there was a mistake that changed the conclusions.

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  • Hidden Sources of Marine Pollution

    Hidden Sources of Marine Pollution

    Plastic waste pollutes oceans across all regions of the world. Marine animals may become entangled in larger plastic debris such as nets and bags or mistake smaller pieces for food. Ingested plastic can block or injure the gastrointestinal tract. The smallest plastic particles in the micro and nano range are mostly excreted, but a small proportion can pass through the intestinal wall and enter the bloodstream.

    So how much nanoplastic is actually present in the oceans? Most scientific attention has so far been focussed on macro- and microplastic because their larger size makes them easier to study. Quantitative data on the pollution of the oceans by nanoplastic particles smaller than 1 µm have been scarce until now because the particles are very small, prone to change, and often difficult to distinguish from other environmental particles using standard methods.

    During a 2020 expedition aboard the RV Pelagia, the largest Dutch research vessel and flagship of the NIOZ, researchers from the UFZ and Utrecht University recorded the occurrence of nanoplastic along a transect from the European continental shelf to the subtropical North Atlantic Gyre. Samples were taken at 12 measuring points: in the uppermost water layer at around 10 m, in the intermediate layer at around 1,000 m, and 30 m above the seabed. “With the data from these measuring points, we can make statements about the vertical and horizontal distribution of nanoplastic in the North Atlantic”, says Dr Dušan Materić, chemist at the UFZ and lead author of the study.

    Led by Materić, the scientists used a high-resolution proton transfer reaction mass spectrometer (PTR-MS) coupled with thermal desorption (TD) to measure the concentrations of organic trace gases. With this TD-PTR-MS, the tiny plastic particles in the samples can be combusted. By heating them, gases are released; these can then be quantified in the mass spectrometer. According to Materić, who developed the method in 2020 while working at Utrecht University, because each polymer produces a distinct chemical fingerprint, its identity and concentration can be reliably determined.

    The researchers detected nanoplastic at all depths analysed across the 12 measurement sites. “They are present everywhere in such large quantities that we can no longer neglect them ecologically”, says Materić. The research team most frequently found nanoparticles of polyethylene terephthalate (PET), polystyrene (PS), and polyvinyl chloride (PVC), which are commonly used in disposable and reusable plastic bottles, films, drinking cups, and cutlery. At nearly all measuring points, the researchers detected these types of plastic in the uppermost water layer. “This is because, on the one hand, the redistribution from the atmosphere occurs via the sea surface and, on the other hand, a lot of plastic is introduced via the estuaries of rivers”, says Materić. The intermediate layer (i.e. the layer between the oxygen-rich surface water and the oxygen-depleted deep water) is dominated by PET nanoparticles. According to Materić, a higher concentration of nanoplastic was found in the North Atlantic subtropical gyre, an area where surface microplastics are known to accumulate because of ocean currents.

    The researchers found the lowest concentrations of nanoplastic in the water layer near the sea floor. They detected PET nanoplastic at all measuring points there – even at depths of more than 4,500 m. This nanoplastic most likely originated from the fragmentation of synthetic clothing fibres but possibly also from previously unknown processes. “Nanoplastic and nanoparticles are so small that the physical laws governing larger particles often no longer apply”, says Materić.

    The research team were surprised to find no polyethylene (PE) or polypropylene (PP) at any of the measuring points. Both PE and PP are commonly used in bags and packaging, which often end up as marine plastic waste. “There is a lot of PE/PP microplastic on the sea surface, but we did not find any PE/PP nanoparticles that could have been formed as a result of solar radiation or abrasion by the waves”, says Materić. The PE and PP nanoplastic may be mineralised or molecularly altered to such an extent that they are no longer detected as plastic by the PTR-MS, or there might be some other dynamic sedimentation and removal processes we are not yet aware of.

    The scientists extrapolated the mass of nanoplastic in the North Atlantic from the concentration measurements. Based on these results, around 27 million tonnes of nanoplastic – 12.0 million tonnes of PET, 6.5 million tonnes of PS, and 8.5 million tonnes of PVC – are stored in the uppermost water layer of the North Atlantic, up to 200 m deep, from the temperate to the subtropical zone. “This is in the same order of magnitude as the estimated mass of macro- and microplastics for the entire Atlantic”, says Materić. This means that nanoplastic accounts for a large proportion of plastic pollution in the oceans and has not yet been factored into current assessments of the marine plastic balance. “Only a couple of years ago, there was still debate over whether nanoplastic even exists. Many scholars continue to believe that nanoplastics are thermodynamically unlikely to persist in nature, as their formation requires high energy. Our findings show that, by mass, the amount of nanoplastic is comparable to what was previously found for macro- and microplastic – at least in this ocean system”, says Materić.

    /Public Release. This material from the originating organization/author(s) might be of the point-in-time nature, and edited for clarity, style and length. Mirage.News does not take institutional positions or sides, and all views, positions, and conclusions expressed herein are solely those of the author(s).View in full here.

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  • ‘Chimpfluencers’ Are Sticking Grass in Their Ears And Butts in Latest Viral Trend : ScienceAlert

    ‘Chimpfluencers’ Are Sticking Grass in Their Ears And Butts in Latest Viral Trend : ScienceAlert

    If chimpanzees had access to TikTok, the platform might soon be flooded with videos of ‘chimpfluencers’ wearing grass in their ears and butts – the latest trend going around a chimp sanctuary in Africa.

    In August 2023, at the Chimfunshi Wildlife Orphanage Trust sanctuary in Zambia, a trendsetting chimp named Juma was seen sticking a piece of grass into his ear, deep enough to stay there on its own. Within a week the fad went viral, as four other chimps in the group started copying his unusual accessory.

    Not to be outdone, later that month Juma debuted a risqué variation: he inserted a blade of grass into his rectum, and left it dangling. This unorthodox trend also caught on, with five other chimps adopting the strange new fashion.

    Related: Bored Capuchin Monkeys Are Kidnapping Howler Babies in Weird New ‘Trend’

    The behavior fascinated researchers observing the captive chimpanzees (Pan troglodytes) . The grass didn’t seem to serve a biological purpose – they weren’t scratching itchy ears or butts, for example. Instead, the team hypothesizes that it might serve a social purpose.

    “By copying someone else’s behavior, you show that you notice and maybe even like that individual. So, it might help strengthen social bonds and create a sense of belonging within the group, just like it does in humans,” says Edwin van Leeuwen, biologist at Utrecht University in the Netherlands.

    A chimp showing off its trendy new ear grass. (Jake Brooker/Chimfunshi Wildlife Orphanage Trust)

    Intriguingly, the event wasn’t the first time Chimfunshi chimps had decorated their orifices with grass. An original trendsetter named Julie started the whole grass-in-ear thing way back in 2010, which caught on with seven other chimps. The behavior continues to this day among the group, even after Julie’s death.

    This seems to be a case of social learning and cultural transmission – after all, only one of the four groups observed back then exhibited the behavior, even though all lived in similar conditions. Weirdest of all is that more than a decade after Julie, Juma seems to have come up with the idea independently, since his group never had contact with hers.

    The researchers suggest that fads with no clear purpose could be a holdover from the important ability to learn new survival skills. It’s telling that wild chimps haven’t been observed following ‘useless’ trends – only captive ones seem to have enough time on their hands.

    YouTube Thumbnail frameborder=”0″ allow=”accelerometer; autoplay; clipboard-write; encrypted-media; gyroscope; picture-in-picture; web-share” referrerpolicy=”strict-origin-when-cross-origin” allowfullscreen>

    “Chimpanzees can socially learn novel skills and primarily use them in contexts of personal interest, like nut-cracking and termite fishing,” the researchers write in a paper about their observations.

    “Yet, when selection pressures relax (e.g., due to systematic provisioning in captive care), chimpanzees may extend their social learning occasionally to behaviors without direct instrumental utility.”

    Non-functional cultural trends aren’t unique to chimps either. In recent years, orcas have been seen wearing dead salmon on their heads like hats, and sinking boats in European waters – both of which seem to be fads.

    A group of wild Indo-Pacific bottlenose dolphins (Tursiops aduncus) in South Australia started ‘tail-walking’ along the surface of the water after one of them observed captive dolphins that had been trained to do the trick. Wild dolphins continued to perform the feat for decades afterwards, indicating the trend had been passed down culturally.

    Studying animal cultures could help teach us more about our own. After all, is sticking grass in your butt really that different from planking or eating laundry detergent pods?

    The research was published in the journal Behaviour.

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  • Research finds 18-million-year-old enamel proteins in mammal fossils — Harvard Gazette

    Research finds 18-million-year-old enamel proteins in mammal fossils — Harvard Gazette

    Proteins degrade over time, making their history hard to study. But new research has uncovered ancient proteins in the enamel of the teeth of 18-million-year-old fossilized mammals from Kenya’s Rift Valley, opening a window into how these animals lived and evolved.

    In their new paper in Nature, researchers from Harvard and the Smithsonian Museum Conservation Institute  discuss their findings.

    “Teeth are rocks in our mouths,” explained Daniel Green, field program director in the Department of Human Evolutionary Biology and the paper’s lead author. “They’re the hardest structures that any animals make, so you can find a tooth that is a hundred or a hundred million years old, and it will contain a geochemical record of the life of the animal.”

    That includes what the animal ate and drank, as well as its environment.

    “In the past, we thought that mature enamel, the hardest part of teeth, should really have very few proteins in it at all,” said Green. However, utilizing a newer proteomics technique called liquid chromatography tandem mass spectrometry, the team was able to detect “a great diversity of proteins … in different biological tissues.”

    “The technique involves several stages where peptides are separated based on their size or chemistry so that they can be sequentially analyzed at higher resolutions than was possible with previous methods,” explained Kevin T. Uno, associate professor in HEB and one of the paper’s corresponding authors.

    “We and other scholars recently found that there are dozens — if not even hundreds — of different kinds of proteins present inside tooth enamel,” said Green.

    With the realization that many proteins are found in contemporary teeth, the researchers turned to fossils, collaborating with the Smithsonian and the National Museum of Kenya for access to fossilized teeth, particularly those of early elephants and rhinos.

    Formed approximately 16 million years ago, the Buluk site in Kenya is found in one of the most remote and inhospitable places in the rift, but has yielded an extraordinary diversity of fossil fauna.

    Photo by Ellen Miller

    As herbivores, they had large teeth to grind the plants that made up their diets. These mammals, Green said, “can have enamel two to three millimeters thick. It was a lot of material to work with.”

    What they found — peptide fragments, chains of amino acids, that together form proteins as old as 18 million years — was “field-changing,” according to Green.

    “Nobody’s ever found peptide fragments that are this old before,” he said, calling the findings “kind of shocking.”

    Until now, the oldest prior findings were put at about 3.5 million years old, he said.

    “With the help of our colleague Tim Cleland, a superb paleoproteomicist at the Smithsonian, we’re pushing back the age of peptide fragments by five or six times what was known before.”

    The newly discovered peptides cover a range of proteins that perform different functions, altogether known as the proteome, Green said.

    “One of the reasons that we’re excited about these ancient teeth is that we don’t have the full proteome of all proteins that could have been found inside the bodies of these ancient elephants or rhinoceros, but we do have a group of them.”

    With such a collection, “There might be more information available from a group of them than just one protein by itself.”

    This research “opens new frontiers in paleobiology, allowing scientists to go beyond bones and morphology to reconstruct the molecular and physiological traits of extinct animals and hominins,” said Emmanuel K. Ndiema, senior research scientist at the National Museum of Kenya and paper co-author. “This provides direct evidence of evolutionary relationships. Combined with other characteristics of teeth, we can infer dietary adaptations, disease profiles, and even age at death — insights that were previously inaccessible.”

    In addition to shedding light on the lives of these creatures, it helps place them in history.

    “We can use these peptide fragments to explore the relationships between ancient animals, similar to how modern DNA in humans is used to identify how people are related to one another,” Uno said.

    “Even if an animal is completely extinct — and we have some animals that we analyze in our study who have no living descendants — you can still, in theory, extract proteins from their teeth and try to place them on a phylogenetic tree,” said Green.

    Such information “might be able to resolve longstanding debates between paleontologists about what other mammalian lineages these animals are related to using molecular evidence.”

    Although this research began as “a small side project” of a much larger project involving dozens of institutions and researchers from around the world, said Green, “We were surprised at just how much we found. There really are a lot of proteins preserved in these teeth.”


    This research was partially funded by the National Science Foundation and Smithsonian’s Museum Conservation Institute.


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  • Black holes could act as cosmic supercolliders – Physics World

    Black holes could act as cosmic supercolliders – Physics World






    Black holes could act as cosmic supercolliders – Physics World


















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