Category: 7. Science

  • Deep-sea fish confirmed as a significant source of ocean carbonate

    Deep-sea fish confirmed as a significant source of ocean carbonate

    image: 

    Martin Grosell, Ph.D., observes the blackbelly rosefish, the subject of the study. 


    view more 

    Credit: Diana Udel, University of Miami

    Deep-sea fish confirmed as a significant source of ocean carbonate

    New research sheds light on the overlooked contribution of the ocean’s most abundant fish to marine carbon cycling. The findings open new avenues for studying deep-sea carbon dynamics and may improve Earth system models.

    MIAMI, FL — July 25, 2025 – A new study offers the first direct evidence that deep-dwelling mesopelagic fish, which account for up to 94 percent of global fish biomass, excrete carbonate minerals at rates comparable to shallow-water species. The findings validate previous global models suggesting that marine fish are major contributors to biogenic carbonate production in the ocean.

    Scientists at the University of Miami Rosenstiel School of Marine, Atmospheric, and Earth Science studied the blackbelly rosefish (Helicolenus dactylopterus), a deep-sea species living at depths of 350-430 meters (1,148-1,410 feet), to determine whether it forms and excretes intestinal carbonate—known as ichthyocarbonate. This physiological process, common among marine fish, helps maintain internal salt and water balance in saline environments and plays a critical role in marine carbon cycling.

    “Mesopelagic fish live in deep, cold, high-pressure environments, and until now, it was unclear if they produced carbonate like shallow water fish do— or at what rate,” Martin Grosell, the lead author of the study and chair of the Department of Marine Biology and Ecology at the Rosenstiel School, said. “This study is the first to confirm that they do and that the mechanisms and characteristics of ichthyocarbonate formation are remarkably consistent across depths.”

    The blackbelly rosefish was an ideal model. Unlike many mesopelagic species, it lacks a swim bladder and can survive both capture and lab acclimation. Researchers maintained specimens at 6 degrees Celsius, replicating their natural habitat, and found they excreted approximately 5 milligrams of ichthyocarbonate per kilogram per hour, aligning with predictions from thermal and metabolic scaling models.

    “This research fills a major gap in our understanding of ocean chemistry and carbon cycling,” Amanda Oehlert, co-author and assistant professor in the Department of Marine Geosciences, said. “With mesopelagic fish playing such a significant role, their contribution to carbonate flux—and how it might change with warming oceans—deserves greater attention.”

    Key findings include:

    • Deep-sea blackbelly rosefish produce carbonate at rates and compositions comparable to shallower fish, confirming that depth and pressure do not inhibit ichthyocarbonate formation.
    • These results strengthen global estimates of fish-derived carbonate production, confirming that mesopelagic fish are substantial contributors to the ocean’s carbonate budget.
    • Ichthyocarbonate composition is similar regardless of the depth at which it forms, which influences how and where it is stored or dissolved in the ocean.

    “These results offer strong support for global models of fish-derived carbonate production, which had assumed—but not verified—that mesopelagic species contribute at similar rates,” Grosell said. “Mesopelagic fish aren’t just prey; they’re chemical engineers of the ocean.”

    The study underscores the importance of ichthyocarbonate in the ocean carbon cycle, especially given the vast, underexplored biomass of the mesopelagic zone.

    The authors say the findings open new avenues for studying deep-sea carbon dynamics and may improve Earth system models, which are sophisticated computer models that incorporate interactions between physical, chemical, and biological processes, such as biological carbon production and export.

    The study, titled “Osmoregulation by the gastro-intestinal tract of marine fish at depth—implications for the global carbon cycle,” was published on July 15, 2025 in the Journal of Experimental Biology. The authors are Martin Grosell, Bret Marek, Sarah Wells, Carolyn Pope, Cameron Sam, Rachael M. Heuer, and Amanda M. Oehlert, all from the University of Miami Rosenstiel School of Marine, Atmospheric, and Earth Science.

    Funding for the study was provided by the National Science Foundation Chemical Oceanography Program and Earth Sciences Instrumentation and Facilities, and the University of Miami Rosenstiel School’s Departments of Marine Biology and Ecology and Marine Geosciences.


    Disclaimer: AAAS and EurekAlert! are not responsible for the accuracy of news releases posted to EurekAlert! by contributing institutions or for the use of any information through the EurekAlert system.

    Continue Reading

  • Multi-Wavelength Dust Characterization of the HL Tau Disk and Implications for Planet Formation

    Multi-Wavelength Dust Characterization of the HL Tau Disk and Implications for Planet Formation

    Images of dust continuum emission of the HL Tau disk. An arcsinh stretch is applied to the color scale. — astro-ph.EP

    We present a comprehensive analysis of the HL Tau dust disk by modeling its intensity profiles across six wavelengths (0.45 to 7.9 mm) with a resolution of 0.05 arcsec (∼7 au).

    Using a Markov Chain Monte Carlo (MCMC) approach, we constrain key dust properties including temperature, surface density, maximum grain size, composition, filling factor, and size distribution. The full fitting, with all parameters free, shows a preference for organics-rich dust with a low filling factor in the outer region (r≳40 au), where the spectral index is ∼3.7, but amorphous-carbon-rich dust also reasonably reproduces the observed intensity profiles.

    Considering the scattering polarization observed at 0.87 mm, compact, amorphous-carbon-rich dust is unlikely, and moderately porous dust is favored. Beyond 40 au, the maximum dust size is likely ∼100 μm if dust is compact or amorphous-carbon rich.

    However, if the dust is moderately porous and organics-rich, both the predicted dust surface density and dust size can be sufficiently large for the pebble accretion rate to reach ∼10M Myr−1 in most regions, suggesting that pebble accretion could be a key mechanism for forming planets in the disk.

    In contrast, if the dust is amorphous-carbon-rich, forming a giant planet core via pebble accretion is unlikely due to the combined effects of low dust surface density and small dust size required to match the observed emission, suggesting other mechanisms, such as disk fragmentation due to gravitational instability, may be responsible for planet formation in the HL Tau disk.

    Takahiro Ueda, Sean M. Andrews, Carlos Carrasco-González, Osmar M. Guerra-Alvarado, Satoshi Okuzumi, Ryo Tazaki, Akimasa Kataoka

    Comments: 20 pages, 11 figures, accepted for publication in ApJ
    Subjects: Earth and Planetary Astrophysics (astro-ph.EP)
    Cite as: arXiv:2507.14443 [astro-ph.EP] (or arXiv:2507.14443v1 [astro-ph.EP] for this version)
    https://doi.org/10.48550/arXiv.2507.14443
    Focus to learn more
    Submission history
    From: Takahiro Ueda
    [v1] Sat, 19 Jul 2025 02:39:16 UTC (10,856 KB)
    https://arxiv.org/abs/2507.14443
    Astrobiology, Astrochemistry,

    Continue Reading

  • Mars Glaciers Are Purer And More Uniform Than Previously Thought

    Mars Glaciers Are Purer And More Uniform Than Previously Thought

    This is an example of a debris-covered glacier on Mars. New research into these features suggests that they are purer than once thought, with implications for understanding Mars’ overall water budget and resource utilization on future crewed missions. Credit: NASA/JPL-Caltech/University of Arizona

    On the slopes of Martian mountains and craters clings what appears to be flowing honey, coated in dust and frozen in time. In reality, these features are incredibly slow-moving glaciers, and their contents were once thought to be mostly rock enveloped in some ice.

    Work over the last 20 years has demonstrated that at least some of these glaciers are mostly pure ice with only a thin cover of rock and dust, but according to a new paper published in Icarus, glaciers all over the planet actually contain more than 80% water ice, a significant finding. Ultimately, this means that Mars’s glacial ice deposits are nearly pure across the globe, providing a clearer understanding of Mars’ climate history and a possible resource for future utilization.

    The paper was led by Yuval Steinberg, a recent graduate of the Weizmann Institute of Science, based in Israel. The two coauthors, Oded Aharonson and Isaac Smith, are senior scientists at the Planetary Science Institute, based in Tucson, with faculty appointments at the Weizmann Institute of Science and York University, respectively.

    “This study highlights how NASA programs are advancing science not just within the United States, but also reaching students around the world,” Aharonson said.

    The five sites that the team investigated for glacier purity. The fact that these disparate sites contained a similarly high ice-to-rock ratio implies that Mars experienced either one widespread glaciation or multiple glaciations that had similar properties, according to the team. Credit: Steinberg et. al.

    Peering under the dust-covered veil

    While reading up on past research, the team quickly realized that when it comes to analyzing debris-covered glaciers, it’s the Wild West.

    “Different techniques had been applied by researchers to various sites, and the results could not be easily compared,” said Smith. “One of the sites in our study had never been studied, and at two of the five sites we used, only partial analysis had been completed previously.”

    So, the team decided to standardize how these debris-covered glaciers are analyzed. They specifically measured their dielectric property (a measure of how quickly radar waves move through a material) and their loss tangent (a measure of how quickly energy dissipates from the radar wave into a material). From these, researchers can infer the ratio of rock to ice within a glacier. This cannot be done from visual observation of the glaciers that have dust and rock-covered surfaces.

    They also identified another area on Mars where SHARAD, short for the SHAllow RADar instrument onboard the Mars Reconnaissance Orbiter, could also do these analyses. This gave them a total of five sites spread across the red planet, enabling global comparison.

    They were surprised to find that all glaciers, even in opposite hemispheres, have nearly the same properties.

    “This is important because it tells us that the formation and preservation mechanisms are probably the same everywhere,” Smith said. “From that, we can conclude that Mars experienced either one widespread glaciation or multiple glaciations that had similar properties. And, by bringing together these sites and techniques for the first time, we were able to unify our understanding of these types of glaciers.”

    Knowing the minimum purity of these glaciers benefits scientific understanding of the processes that form and preserve them. Additionally, it helps when planning for future human exploration of Mars, when using local resources, such as water, becomes mission-critical.

    Next, the team will seek out additional glaciers to add their global comparison and solidify their understanding of these dust-covered mysteries.

    THE PLANETARY SCIENCE INSTITUTE

    The Planetary Science Institute is a private, nonprofit 501(c)(3) corporation dedicated to Solar System exploration. It is headquartered in Tucson, Arizona, where it was founded in 1972.

    PSI scientists are involved in numerous NASA and international missions, the study of Mars and other planets, the Moon, asteroids, comets, interplanetary dust, impact physics, the origin of the Solar System, extra-solar planet formation, dynamics, the rise of life, and other areas of research. They conduct fieldwork on all continents around the world. They are also actively involved in science education and public outreach through school programs, children’s books, popular science books and art.

    PSI scientists are based in over 30 states, the District of Columbia and several international locations.

    Physical properties of subsurface water ice deposits in Mars’s Mid-Latitudes from the shallow radar, Icarus (open access)

    Astrobiology,

    Continue Reading

  • Can You See The ISS From Earth?

    Can You See The ISS From Earth?

    Summer nights are great for watching the sky. The best meteor shower of the year has started, most of the world will get to see a lunar eclipse soon, and even if you live in a city with light pollution, you can still catch the International Space Station (ISS) as it passes overhead.

    Humans have lived in the ISS for almost a quarter of a century, and it is still going strong. It goes around the planet every 93 minutes, in a peculiar orbit; it has an inclination of 51.6 degrees to Earth’s equator, which means it is not passing over the same place over and over again. Well, not immediately.

    The ISS does 15.5 orbits every 24 hours, covering a lot of Earth, but it is not bright enough to be seen during the day. At night it is easier to spot after dusk or before dawn, when it is still dark here on Earth, but 400 kilometers (250 miles) up, the station’s solar panels are still catching sunlight and reflecting it back to us. Sometimes there are periods where you can watch the ISS just once a month, and others where you can try multiple times a week.

    When to see the ISS in the US

    Right now, if you are in Los Angeles, you are in the latter category. It will be visible twice tonight, at 8:43 pm PT, and then at 10:17, and then tomorrow, at 9:29 pm. On July 27 and 28, it will repeat a similar pattern, just shifted by a few minutes. This won’t be a California exclusive, however. Wherever you are in the US, you will get the chance to see it multiple times this week. In New York, you have tonight and tomorrow at 10:11 pm and tomorrow at 9:22 pm to catch it, then again on July 28 and 30.

    How to find the ISS from wherever you are on Earth

    There are multiple official trackers to let you know where and when to look. The one linked here gives a prediction of direction and brightness. There is also a NASA official tracking app that comes with notifications for when the ISS is above your head.

    How to see the ISS 

    You do not need binoculars or telescopes; the ISS is bright enough to be seen with the naked eye. It might be the length of an American football field (including the end zones), hundreds of kilometers up in the sky, but it is pretty reflective, making it an easy spot. Also, it moves! And not like an airplane does, or a satellite. It will be larger than you are probably expecting, will look quite clearly white, and will be moving fast across the sky in a smooth line at a steady pace. If it’s above you, you can’t miss it. 

    And if the weather is not good right now for clear skies, don’t worry. The good thing about the ISS is that it comes around again and again.

    Continue Reading

  • 850,000-Year-Old Homo Antecessor Remains Suggest Ancient Child Was Decapitated And Eaten By Its Own Kind

    850,000-Year-Old Homo Antecessor Remains Suggest Ancient Child Was Decapitated And Eaten By Its Own Kind

    Warning: This is a grisly one. Around 850,000 years ago, a small child belonging to a now extinct human species was decapitated and processed for food, according to new archaeological finds in northern Spain.

    The specimen, a tiny vertebra, belonged to a two- to four-year-old member of the archaic human species known as Homo antecessor, which was recently excavated from the Gran Dolina site in Sierra de Atapuerca, Spain. This species of human lived in Western Europe during the Lower Palaeolithic era, around 1.2 million to 800,000 years ago. Some have argued that this species may have represented the common ancestor of Neanderthals and Homo sapiens.

    The vertebra showed evidence of precision cutting, while other bones found at the site exhibited marks characteristic of defleshing and intentional fracturing. These are typical indicators of meat being removed for food and are common on animal bones eaten by these early humans.

    The team also discovered a tooth belonging to Homo antecessor at the site.

    Image credit: Maria D. Guillen/IPHES-CERCA

    “This case is particularly striking, not only because of the child’s age, but also due to the precision of the cut marks,” Dr Palmira Saladié, IPHES-CERCA researcher and co-director of the Gran Dolina excavation alongside Dr Andreu Ollé, explained in a statement. “The vertebra presents clear incisions at key anatomical points for disarticulating the head. It is direct evidence that the child was processed like any other prey.” 

    Although this is a pretty unpalatable find, it is not the first time such behavior has been identified at this site. Nearly thirty years ago, the same archaeological level revealed the first known case of human cannibalism in the world.

    “What we are documenting now is the continuity of that behaviour: the treatment of the dead was not exceptional, but repeated,” said Saladié.

    The new evidence, which was excavated in July this year, adds to our belief that these humans exploited one another as a food source and possibly as a form of territorial control. In addition to the child’s vertebrae, archaeologists also recovered a hyena latrine with over 1,300 coprolites (fossilized poop) that were plopped on the level just above where the human remains were found. Such overlaying evidence helps archaeologists reconstruct who or what occupied the cave at different times, and as a result, get a better understanding of the history of interspecies competition in this environment.

    The archaeologists believe there is likely more to be discovered at the site, especially in relation to human bones.

    “Every year we uncover new evidence that forces us to rethink how they lived, how they died, and how the dead were treated nearly a million years ago,” Saladié concluded. 

    Continue Reading

  • DNA Packaging Regulates Genomes Guardian’

    DNA Packaging Regulates Genomes Guardian’

    Each cell in our bodies carries about two meters of DNA in its nucleus, packed into a tiny volume of just a few hundred cubic micrometers—about a millionth of a milliliter. The cell manages this by winding the strings of DNA around protein spools. The protein-DNA complexes are called nucleosomes, and they ensure that DNA is safely stored.

    But this packaging into nucleosomes also poses a challenge: important cellular machinery must still access the genetic code to keep cells healthy and prevent diseases like cancer.

    One of the most important proteins in our cells is p53, the “genome’s guardian.” It helps control cell growth, triggers repair of damaged DNA, and can even order faulty cells to self-destruct.

    In many cancers, p53 is disabled or hijacked, so understanding how p53 works is vital for developing cancer therapies. But there’s a problem: most of the DNA sequences that p53 targets are buried inside nucleosomes, making them difficult to reach. Scientists have long wondered how p53 can reach those “hidden” sequences to do its job, as well as how other proteins that interact with p53 manage to find it in this maze of chromatin.

    A new layer of control revealed

    Now, researchers led by Nicolas Thomä, who holds the Paternot Chair in Cancer Research at EPFL, have found that nucleosomes act as a gatekeeper for p53’s molecular partners. By studying how p53 interacts with different cofactors while attached to nucleosomal DNA, the team has revealed a new layer of control over this critical protein’s activity.

    The researchers used a combination of cutting-edge techniques, including cryo-electron microscopy (cryo-EM), biochemical assays, and genome-wide mapping. Using these tools, they reconstructed how p53 binds to its DNA targets when those targets are wrapped up in nucleosomes.

    They then tested whether two important “cofactor” proteins could still reach p53 when it is bound to nucleosomal DNA: USP7, which helps stabilize p53, and the viral E6-E6AP complex, which helps degrade p53.

    They found that p53 can still bind to DNA even when it is wrapped in nucleosomes, especially at the edges where DNA enters or exits the spool. But more surprisingly, the researchers discovered that USP7 could interact with p53 even while bound to the nucleosome, forming a stable complex that they could observe in detail using cryo-EM.

    In contrast, E6-E6AP couldn’t access p53 when it was attached to nucleosomal DNA. This means that the structure of chromatin itself selectively allows or blocks certain proteins from reaching p53, adding an extra level of regulation beyond simple genetic sequences or protein-protein interactions.

    The work shows that the physical structure of DNA and its packaging in the nucleus actively influences molecular interactions. By revealing how nucleosomes can “gatekeep” access to p53, the research opens new possibilities in cancer research that could inform future therapies that aim to restore or control p53 function in disease.

    Other contributors

    • Friedrich Miescher Institute for Biomedical Research
    • University of Basel

    Reference

    Deyasini Chakraborty, Colby R. Sandate, Luke Isbel, Georg Kempf, Joscha Weiss, Simone Cavadini, Lukas Kater, Jan Seebacher, Zuzanna Kozicka, Lisa Stoos, Ralph S. Grand, Dirk Schübeler, Alicia K. Michael, Nicolas H. Thomä. Nucleosomes specify cofactor access to p53. Molecular Cell, 25 July 2025.

    /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.

    Continue Reading

  • Fetal Brain Genes May Drive Later Brain Disorders

    Fetal Brain Genes May Drive Later Brain Disorders


    Register for free to listen to this article

    Thank you. Listen to this article using the player above.


    Want to listen to this article for FREE?


    Complete the form below to unlock access to ALL audio articles.

    A new study by researchers at the Hospital del Mar Research Institute and Yale University suggests that the origins of several brain-related disorders may be found in the earliest stages of fetal brain development. The findings, published in Nature Communications, show that many genes associated with neuropsychiatric and neurodegenerative diseases are active in neural stem cells, well before birth.

    The research focused on nearly 3,000 genes linked to conditions such as autism, bipolar disorder, depression, schizophrenia and neurodegenerative diseases including Alzheimer’s and Parkinson’s. Using a combination of human and mouse data, alongside in vitro cellular models, the team simulated how genetic disruptions might affect the development of the fetal brain.

    Simulating genetic disruptions in neural stem cells

    Neural stem cells give rise to all the cell types of the brain, including neurons and their support cells. The study explored how gene alterations influence these progenitor cells during different stages of development. Researchers modelled regulatory networks for each relevant cell type and assessed how activating or silencing disease-linked genes affected their behaviour.

    Neural stem cells

    These are self-renewing cells in the developing brain that generate neurons and glial cells. They play a crucial role in forming brain structures during fetal development.

    Regulatory networks

    In biology, these are systems of interacting genes, proteins, and other molecules that control gene expression and cellular behaviour. They are key to understanding how genes function in specific contexts.

    This approach allowed the team to identify when and where specific genes are most active, providing a clearer picture of how early genetic alterations may lead to brain structure and function changes later in life. Disorders ranging from cortical malformations, such as microcephaly and hydrocephaly, to anorexia, depression and schizophrenia were included in the analysis.

    “Scientists usually study the genes of mental illnesses in adults, but in this work we discovered that many of these genes already act during the early stages of fetal brain formation, and that their alterations can affect brain development and promote mental disorders later on”.

    Dr. Nicola Micali.

    Cortical malformations

    These refer to structural abnormalities in the cerebral cortex, the brain’s outer layer, which can lead to neurological and developmental disorders.

    Broader implications for understanding disease mechanisms

    The study suggests that disruptions to gene function in neural stem cells could contribute to a wide range of conditions affecting the cerebral cortex. It also highlights specific developmental windows when these genes are especially influential, which could be critical for identifying periods of heightened vulnerability or therapeutic opportunity.

    The findings may contribute to future efforts in understanding how early brain development impacts mental and neurological health. They also lay the groundwork for more targeted studies into gene function during neurodevelopment, potentially informing future gene-based treatment approaches.

    Reference: Mato-Blanco X, Kim SK, Jourdon A, et al. Early developmental origins of cortical disorders modeled in human neural stem cells. Nat Commun. 2025;16(1). doi: 10.1038/s41467-025-61316-w

    This article has been republished from the following materials. Note: material may have been edited for length and content. For further information, please contact the cited source. Our press release publishing policy can be accessed here.

    This content includes text that has been generated with the assistance of AI. Technology Networks’ AI policy can be found here.

    Continue Reading

  • Jaw-Dropping Video Shows NASA’s Plan to Deliver a Helicopter Swarm to Mars Without Landing

    Jaw-Dropping Video Shows NASA’s Plan to Deliver a Helicopter Swarm to Mars Without Landing

    It’s been more than a year since the Ingenuity helicopter broke one of its blades, ending its experimental stint on Mars. On the heels of this wildly successful NASA mission, a defense contractor has introduced a new design concept to succeed the iconic Mars chopper—one that would release multiple vehicles to spread across the Martian landscape at the same time, like a coordinated swim team diving into the water.

    Virginia-based AeroVironment (AV), in partnership with NASA’s Jet Propulsion Laboratory (JPL), recently revealed its Skyfall mission concept, a next-generation Mars helicopter designed to pave the way for a future human landing on the neighboring world. Skyfall would deploy six small choppers, similar to NASA’s Ingenuity, to the Red Planet using a single entry capsule, with each helicopter landing independently on the Martian surface. The mission is aiming for a launch date in 2028, according to AV.

    The landing carrier would drop the six helicopters midway through its descent through the planet’s atmosphere, eliminating the need for a landing platform. Following their release from the carrier, each helicopter would land on the Martian surface under its own power. Each helicopter would quickly get to work, exploring different parts of the planet and investigating potential landing sites for a future human mission.

    Operating independently, each chopper will collect high-resolution images of the surface and radar data from beneath the surface to search for potential resources on Mars. “With six helicopters, Skyfall offers a low-cost solution that multiplies the range we would cover, the data we would collect, and the scientific research we would conduct–making humanity’s first footprints on Mars meaningfully closer,” William Pomerantz, head of Space Ventures at AV, said in a statement.

    Ingenuity was the first helicopter to fly on another planet, paving the way for a fleet of successors that can explore the Martian surface from above. The o.g. Mars helicopter arrived on the planet in February 2021, tucked inside the belly of NASA’s Perseverance rover. Shortly afterwards, the 19-inch-tall (48-centimeter), 4-pound (1.8-kilogram) helicopter became the first powered aircraft to lift off from the surface of another planet. Although it was originally intended to perform just five test flights, Ingenuity kept on going, performing 72 flights and flying 14 times farther than planned for a total flight time of two hours.

    Things came crashing down for Ingenuity last year after the helicopter broke its blades while landing for the 72nd time, officially ending its mission in January 2024. Its mission more than exceeded expectations, delivering precious data on a new method of exploring the surface of another planet and opening up a new gateway for missions to Mars and elsewhere. Whatever chopper comes next will have some pretty big shoes to fill, so maybe sending six helicopters to Mars is the appropriate follow-up.

    Continue Reading

  • New Python Toolkit Automates Single-Cell Lineage Tracing, Accelerates Tumor Drug Resistance Analysis

    New Python Toolkit Automates Single-Cell Lineage Tracing, Accelerates Tumor Drug Resistance Analysis

    Researchers at Tsinghua University have released a novel Python toolkit, scLT-kit, which automates the processing and analysis of single-cell lineage tracing data, delivering clear insights into how individual cells develop, differentiate, and respond to treatments. Think of scLT-kit as a “GPS for cell genealogies”—it takes messy, high-dimensional data and plots each cell’s journey, making complex lineage relationships easy to follow. This tool addresses the growing need for flexible, user-friendly software to handle complex single-cell datasets.

    Novel Model to Decode Cell Dynamics Energises Regenerative Medicine and Cancer Research

    Understanding how cells change over time is crucial for fields ranging from regenerative medicine to cancer therapy. By making lineage tracing analyses more accessible, scLT-kit can accelerate research into tissue development, drug resistance, and disease progression. Its streamlined workflows could help biologists, pharmaceutical developers, and policymakers better evaluate how cells respond to treatments, ultimately informing new strategies for diagnosis and therapy.

    “With scLT-kit, we’ve improved a previously labor-intensive, bespoke analysis into a seamless, reproducible workflow,” says Prof. Jin Gu. “Our goal was to empower every lab—whether focused on development, drug resistance, or disease progression—to extract lineage insights from single-cell data in minutes, not months.”

    Automated Barcode Analysis Uncovers Predictable Developmental Clones—and Unruly Drug-Resistant Tumor Cells

    Through a series of analyses, the researchers uncovered the following insights:

    • scLT-kit reliably processes time-series single-cell RNA-seq data tagged with heritable barcodes, providing rapid quality checks and summary statistics of barcoding efficiency and clone sizes.
    • In developmental datasets (e.g., blood progenitors and C. elegans embryos), cells sharing the same barcode showed higher similarity in gene expression than unrelated cells.
    • In tumor cell lines treated with EGFR inhibitors (osimertinib or erlotinib), this within-clone similarity was less pronounced, reflecting the high heterogeneity of cancer persisters.
    • The toolkit computes measures of cell fate diversity, showing that normal development features more predictable outcomes, whereas drug-treated cancer cells exhibit greater randomness in fate decisions.
    • scLT-kit identifies subpopulations with distinct fate trajectories and uncovers genes linked to these fates through differential expression analysis.

    All-in-One Python Package Delivers Barcode QC, Lineage Networks and Interactive Sankey Plots

    scLT-kit combines standard single-cell RNA-seq processing with two specialized modules for lineage data. The scLT-statistics module calculates barcoding fractions and clone sizes at each time point. The scLT-analysis module builds lineage-based networks to infer how clusters of cells transition over time, visualizing dynamics with Sankey plots. Four quantitative indicators assess cell fate randomness and neighbor similarity. Finally, the package uses established statistical tests to link gene expression changes to specific fate outcomes, all within an easy-to-install Python package available on PyPI and GitHub.

    Streamlined Workflows Lower the Barrier to Single-Cell Lineage Tracing in Development and Disease

    scLT-kit brings robust, automated workflows to single-cell lineage tracing studies, lowering the barrier for labs to explore cell dynamics in development and disease. By integrating data quality checks, dynamic analysis, and gene-level insights, this toolkit promises to advance our understanding of how cells make fate decisions under both normal and perturbed conditions. The full study was published in Frontiers of Computer Science in April 2025 (https://doi.org/10.1007/s11704-025-41249-9).

    Frontiers of Computer Science (FCS) is a leading peer-reviewed international journal co-published by HEP and Springer Nature. FCS publishes papers in all major branches of computer science including (not limited to): Architecture, Software, Artificial intelligence, Theoretical computer science, Networks and communication, Information systems, Image and graphics, Information security, Interdisciplinary. Papers published in FCS include research articles, review articles, letters. FCS is indexed by SCI(E), EI, Scopus, et al. The Latest IF will be 4.8, Q1. It is also class B journal in the CCF recommended journals directory.

     


    Continue Reading

  • Simple Rules Govern Soil Microbiome Responses to Environmental Change

    Simple Rules Govern Soil Microbiome Responses to Environmental Change

    Newswise — Just like any living organism, the soil has its own metabolism. Plants, worms, insects, and most importantly, microorganisms in the soil, break down organic matter, consume and generate nutrients, and process other materials to give the soil a life of its own. Soil microbiomes, which drive much of the metabolism in these ecosystems, are immensely complex – comprised of thousands of species with untold interactions and dynamics.

    Given the complexity of the soil, however, it can be nearly impossible to understand how the communities of microbes living there respond to changes in the environment, such as temperature, moisture, acidity, and nutrient availability. Solving this problem is critical if we want to understand how soil microbiomes adapt to ever-changing environmental conditions and climate change.

    New research from the University of Chicago shows that a deceptively simple mathematical model can describe how the soil responds to environmental change. Using just two variables, the model shows that changes in pH levels consistently result in three distinct metabolic states of the community.

    The study, published this week in Nature, highlights how describing the collective behavior of complex systems mathematically can cut through the complexity, enabling predictions of how the soil and its metabolism will respond to change.  Ultimately, this will help scientists design interventions for improving agriculture or restoring ecosystems.

    “When people think about these ecosystems, they assume you have to write down a mathematical description of the entire system, which involves thousands of variables, interacting species, and the resources they’re consuming,” said Seppe Kuehn, PhD, Associate Professor of Ecology and Evolution at the University of Chicago, and the senior author of the paper. “So, the fact that we were able to describe this in a simple way was extremely intellectually satisfying.”

    A herculean effort to analyze the soil

    The study is the result of a herculean effort by Kiseok Lee, PhD, a recently graduated student from Kuehn’s lab. He sampled 20 natural soils across the pH gradient from Cook Agronomy Farm in Pullman, Washington, that have large natural variations in pH but few differences in other environmental factors. Then, he manipulated each native soil’s pH by small increments in the lab, resulting in 1,500 microcosm experiments.

    The pH level is a measure of the concentration of hydrogen ions in a solution. Lower pH means more acidic (more hydrogen ions), and higher pH means more basic or alkaline (fewer hydrogen ions).

    Levels of pH in the soil are important because they affect the types of microorganisms living there, their metabolic activity, and the soil’s chemistry. The researchers wanted to test the effects of changing pH on anaerobic nitrate respiration, which is the process by which anaerobic microbes (i.e. ones that don’t require oxygen) use nitrate to generate energy. Nitrate respiration is a key metabolic process in agriculture and soil health.

    Lee painstakingly placed samples onto plates, each with 48 wells for holding the soil, along with some water, nitrates, and acid or base solution to change the pH. Preparing and incubating the samples took months. After that, Lee took time-series measurements of nitrate in each microcosm—a total of 15,000 measurements, all by hand. “I was the machine,” Lee said, when asked if he was able to automate any of the sampling and testing.

    Deceptively simple modeling

    Lee and Kuehn worked with Siqi Liu, PhD, co-first author and a former graduate student in the lab of study co-corresponding author Madhav Mani, PhD, Associate Professor of Engineering Sciences and Applied Mathematics at Northwestern University, along with co-corresponding author Mikhail Tikhonov, PhD, Associate Professor of Physics at Washington University in St. Louis.

    The team created a model to describe the dynamics in each of the 1,500 samples as they metabolized the nitrate. They found that a simple model predicted the activity with just two parameters: indigenous biomass activity and the amount of growth-limiting nutrient available. Depending on how the pH was changed, they saw three consistent results:

    • Regime I, or the “acidic death regime”:  Large changes toward acidity caused the death of functional biomass
    • Regime II, “nutrient-limiting regime”: During moderate changes, acidic or basic, the nitrate metabolism was limited by the availability of a limiting nutrient (carbon), resulting in linear nitrate dynamics
    • Regime III, “resurgent growth regime”: Large changes toward basic conditions caused dominant groups of microbes to become less active, while rare groups rapidly grew and metabolized nitrate exponentially

    “No matter how you perturb the pH, there’s just these three dynamic classes of behavior that the whole ecosystem can exhibit. Outside of that, it doesn’t look like anything else is allowed,” Kuehn said. “That’s really quite striking, because you have all this complexity at the lower level giving rise to this relative simplicity at the higher level.”

    “This connects to an important theoretical question: when is it OK to summarize dozens of diverse species with a single coarse model?” Tikhonov said. “Here, Kiseok and Siqi managed to show that a coarsened description is not only an excellent approximation of the data but captures something general about community response to perturbations.”

    Putting the new model to use

    Understanding how the soil microbiome responds to these changes is useful for designing interventions. For example, if nitrogen fertilizer runoff from farms contaminates nearby waterways, officials could take measures to increase pH and remove excess nitrate to prevent algae blooms.

    “If you want to understand how these systems are going to respond to future perturbations, then delimiting the set of possible responses is obviously very useful,” Kuehn said.

    The researchers also think the same modeling approach can be applied to other environmental factors.

    “Focusing on the resilience of the community, which is expressed by biomass activity and the limiting nutrient, shows us that different amounts of perturbations will elicit different effects,” Lee said. “I think this means that we can apply it to elucidating functional responses in other microbial systems against different environmental changes, whether it be from temperature, pH, salinity, or something else.”

    The study, “Functional regimes define soil microbiome response to environmental change,” was supported by the National Science Foundation, the National Institute for General Medical Sciences, the Center for Living Systems at UChicago, the National Institute for Mathematics and Theory in Biology, the Simons Foundation, and the Chan-Zuckerberg Initiative. Additional authors include Kyle Crocker and Jocelyn Wang from UChicago and David Huggins from the United States Department of Agriculture.


    Continue Reading