Thursday, August 21, 2025

Recovering by-products from U.S. metal mines could reduce need for critical mineral imports




Summary author: Becky Ham



American Association for the Advancement of Science (AAAS)





A new statistical analysis of geochemical datasets by Elizabeth Holley and colleagues suggests that the U.S. could reduce its dependence on critical mineral imports by recovering ore byproducts from its active metal mines. Holley et al. conclude that 90% recovery of these byproducts “could meet nearly all U.S. critical mineral needs; one percent recovery would substantially reduce import reliance for most elements evaluated.” A host of minerals, including cobalt, nickel, manganese, lithium, tellurium, germanium, and more, have been designated in the U.S. as critical minerals for their importance in technologies from batteries to magnets to solar panels. Increased demand and geopolitical conflict in major mining regions, along with the long timeline for developing new mines, make a new domestic source of these minerals an attractive prospect for the U.S. To estimate the amount of these minerals that could be recovered domestically as byproducts, Holley et al. analyzed two databases covering the main commodity production of U.S. metal mines and the geochemistry for 70 critical minerals analyzed across ore samples in the U.S. In most cases, recovering less than 10% of the byproducts would generate a larger gross dollar amount than the main products of U.S. metal mines, according to the researchers.

 

UC Irvine-led research team uncovers global wildfire paradox



Total burned area declined in past two decades while human impacts worsened



University of California - Irvine





Irvine, Calif.  Researchers at the University of California, Irvine and other institutions have spotted a contradiction in worldwide wildfire trends: Despite a 26 percent decline in total burned area from 2002 to 2021, the number of people exposed to wildfires has surged by nearly 40 percent.

The study, published today in Science, revealed another statistic that may come as a surprise to people who rely primarily on Western news sources: While high-profile wildfire disasters in the United States, Canada and Australia often dominate headlines, the researchers found that 85 percent of all human exposures to wildfires during that period occurred in Africa.

Just five central African countries – Congo, South Sudan, Mozambique, Zambia and Angola – accounted for half of all global human exposure. In contrast, the United States, Europe and Australia collectively constituted less than 2.5 percent of the total.

“Nevertheless, the western U.S. and particularly California are hot spots of intense fires globally,” said senior author Mojtaba Sadegh, an associate professor of civil engineering at Idaho’s Boise State University who earned a Ph.D. in civil and environmental engineering at UC Irvine in 2015. “Our previously published study shows that California experiences a disproportionately large share of U.S. fire impacts, accounting for 72 percent of human exposures despite comprising 15 percent of the nation’s burned area.”

The researchers analyzed population data and more than 18.6 million fire records from 2002 to 2021 to find that an estimated 440 million people worldwide were exposed to a wildfire encroaching on their home during this period – a number roughly equivalent to the entire population of the European Union. They discovered that human exposure to wildland fire increased by 7.7 million people, an average of 382,700 persons per year during the study period. This surge in human exposure was prompted not by a global jump in fire activity but primarily by population growth and migration into fire-prone landscapes.

Another factor illuminated by the research is a significant rise in the intensity of wildfires in North and South America. This is linked to the climate change-driven amplification of “fire weather,” which includes conditions like increased heat, lower humidity and strong winds.

Extreme fire weather has grown by more than 50 percent over the past four decades globally.

When combined with such human activities as land development and historical fire suppression practices, this trend has led to an escalating risk of destructive fires in regions like California. The frequency of conditions conducive to extreme-impact wildfires (like the 2025 Los Angeles fires) quadrupled from 1990 to 2022 across the state.

In Europe and Oceania, the study noted a decline in wildfire exposures, mainly because of population shifts from rural to urban areas. This highlights how both social and environmental factors play critical roles in shaping wildfire risk.

“The global paradox of decreased burn area and increased human impacts we uncovered … is due largely to an increasing overlap between human settlements and fire-prone landscapes,” said co-author Amir AghaKouchak, UC Irvine Chancellor’s Professor of civil and environmental engineering.

Underscoring a growing human vulnerability to wildfires – particularly in regions that receive little international attention – the research emphasizes the urgent need for proactive mitigation strategies to protect communities from the burgeoning threat of wildfires. These include vegetation management techniques like prescribed fires, public education and engineering solutions to reduce human-caused ignitions.

“As climate change intensifies fire weather and global populations continue to expand into fire-prone zones, proactive mitigation will be increasingly critical to reduce the risk of future wildfire disasters,” AghaKouchak said.

Study collaborators included Matthew Jones of England’s University of East Anglia; Seyd Teymoor Seydi of Boise State University; John Abatzoglou and Crystal Kolden of UC Merced; Gabriel Filippelli of Indiana University Indianapolis; Matthew Hurteau of the University of New Mexico; Charles Luce of the U.S. Department of Agriculture Forest Service’s Rocky Mountain Research Station in Boise; and Chiyuan Miao of Beijing Normal University. Funding was provided by the U.S. National Science Foundation.

About the University of California, Irvine: Founded in 1965, UC Irvine is a member of the prestigious Association of American Universities and is ranked among the nation’s top 10 public universities by U.S. News & World Report. The campus has produced five Nobel laureates and is known for its academic achievement, premier research, innovation and anteater mascot. Led by Chancellor Howard Gillman, UC Irvine has more than 36,000 students and offers 224 degree programs. It’s located in one of the world’s safest and most economically vibrant communities and is Orange County’s second-largest employer, contributing $7 billion annually to the local economy and $8 billion statewide. For more on UC Irvine, visit www.uci.edu.

Media access: Radio programs/stations may, for a fee, use an on-campus studio with a Comrex IP audio codec to interview UC Irvine faculty and experts, subject to availability and university approval. For more UC Irvine news, visit news.uci.edu. Additional resources for journalists may be found at https://news.uci.edu/media-resources.

 

Extinct human relatives left a genetic gift that helped people thrive in the Americas



A new study found that a gene passed down from extinct archaic humans provided an adaptive advantage for Indigenous people of the Americas and is still common today in people of Indigenous descent



Brown University






PROVIDENCE, R.I. [Brown University] — A new study provides fresh evidence that ancient interbreeding with archaic human species may have provided modern humans with genetic variation that helped them adapt to new environments as they dispersed across the globe.

The study, published in Science, focused on a gene known as MUC19, which is involved in the production of proteins that form saliva and mucosal barriers in the respiratory and digestive tracts. The researchers show that a variant of that gene derived from Denisovans, an enigmatic species of archaic humans, is present in modern Latin Americans with Indigenous American ancestry, as well as in DNA collected from individuals excavated at archeological sites across North and South America.

The frequency at which the gene appears in modern human populations suggests the gene was under significant natural selection, meaning it provided a survival or reproductive advantage to those who carried it. It’s not clear exactly what that advantage might have been, but given the gene’s involvement in immune processes, it may have helped populations to fight off pathogens encountered as they migrated into the Americas thousands of years ago.

“From an evolutionary standpoint, this finding shows how ancient interbreeding can have effects that we still see today,” said study author Emilia Huerta-Sánchez, a professor of ecology, evolution and organismal biology at Brown University. “From a biological standpoint, we identify a gene that appears to be adaptive, but whose function hasn’t yet been characterized. We hope that leads to additional study of what this gene is actually doing.”

Huerta-Sanchez co-authored the study with Fernando Villanea, a former post-doctoral researcher at Brown who is now at University of Colorado, Boulder; David Peede, a graduate student at Brown; and an international team of collaborators.

Not much is known about the Denisovans, who lived in Asia between 300,000 and 30,000 years ago, aside from a few small fossils from Denisova cave in Siberia, two jaw bones found in Tibet and Taiwan, and a nearly complete skull from China found this year. The finger fossil from Siberia contained ancient DNA, which enables scientists to look for common genes between Denisovans and modern humans. Prior research led by Huerta-Sánchez found that a version of a gene called EPAS1 acquired from Denisovans may have helped Sherpas and other Tibetans to adapt to high altitudes.

For this study, the researchers compared Denisovan DNA with modern genomes collected through the 1,000 Genomes Project, a survey of worldwide genetic variation. The researchers found that the Denisovan-derived MUC19 gene is present in high frequencies in Latino populations who harbor Indigenous American genetic ancestry. The researchers also looked for the gene in the DNA of 23 individuals collected from archeological sites in Alaska, California, Mexico and elsewhere in the Americas. The Denisovan-derived variant was present at high frequency in these ancient individuals as well.

The team used several independent statistical tests to show that the Denisovan MUC19 gene variant rose to unusually high frequencies in ancient Indigenous American populations and present-day people of Indigenous descent, and that the gene sits on an unusually long stretch of archaic DNA — both signs that natural selection had boosted its prevalence. The research also revealed that the gene was likely passed through interbreeding from Denisovans to another archaic population, the Neanderthals, who then interbred with modern humans.

Huerta-Sánchez said the findings demonstrate the importance that interbreeding had in introducing new and potentially useful genetic variation in the human lineage.

“Typically, genetic novelty is generated through a very slow process,” Huerta- Sánchez said.  “But these interbreeding events were a sudden way to introduce a lot of new variation.”

In this case, she said, that “new reservoir of genetic variation” appears to have helped modern humans as they migrated into the Americas, perhaps providing a boost to the immune system.

“Something about this gene was clearly useful for these populations — and maybe still is or will be in the future,” Huerta-Sánchez said.

She’s hopeful that the recognition of the gene’s importance will spur new research into its function to reveal novel biological mechanisms, especially since it involves coding genetic variants that alter the protein sequence.

The research was supported by The Leakey Foundation, the National Institutes of Health (1R35GM128946- 01, T32 GM128596, R35GM142978, R01NS122766), the Alfred P. Sloan Foundation, the Blavatnik Family Graduate Fellowship in Biology and Medicine, the Brown University Predoctoral Training Program in Biological Data Science (NIH T32 GM128596), the Burroughs Wellcome Fund and the Human Frontier Science Program.

 

The rise of plant life changed how rivers move, Stanford study shows




Stanford University
Unvegetated meandering stream 

image: 

A view of seasonal flow in Shoshone Creek – an unvegetated meandering stream in Nevada. (Image credit: M. Hasson and M. Lapôtre)

view more 

Credit: M. Hasson and M. Lapôtre





A new Stanford study challenges the decades-old view that the rise of land plants half a billion years ago dramatically changed the shapes of rivers. 

Rivers generally come in two styles: braided, where multiple channels flow around sandy bars, and meandering, where a single channel cuts S-curves across a landscape. Geologists have long thought that before vegetation, rivers predominantly ran in braided patterns, only forming meandering shapes after plant life took root and stabilized riverbanks. 

The new study, which will be published online by the journal Science on Thursday, Aug. 21, 2025, suggests the theory that braided rivers dominated the first 4 billion years of Earth’s history is based on a misinterpretation of the geological record. The research demonstrates that unvegetated meandering rivers can leave sedimentary deposits that look deceptively similar to those of braided rivers. This distinction is crucial for our understanding of Earth’s early ecology and climate, as a river’s type determines how long sediment, carbon, and nutrients are stored in floodplains. 

“With our study, we’re pushing back on the widely accepted story of what landscapes looked like when plant life first evolved on land,” said lead author Michael Hasson, a PhD student in Mathieu Lapôtre’s lab at the Stanford Doerr School of Sustainability. “We’re rewriting the story of the intertwined relationship between plants and rivers, which is a significant revision to our understanding of the history of the Earth.”

The muddy floodplains of meandering rivers – dynamic ecosystems created over thousands of years by river overflow – are among the planet’s most abundant non-marine carbon reservoirs. Carbon levels in the atmosphere, in the form of carbon dioxide, act as Earth’s thermostat, regulating temperature over vast timescales. Accurately budgeting for the carbon caches created by meandering rivers could help scientists build more comprehensive models of Earth’s ancient and future climate. 

“Floodplains play an important role in determining how, when, and whether carbon is buried or released back into the atmosphere,” Hasson said. “Based on this work, we argue carbon storage in floodplains would have been common for much longer than the classic paradigm that assumes meandering rivers only occurred over the last several hundred million years.”

Where the river flows

To gauge vegetation’s impact on river channel patterns, the researchers examined satellite imagery of about 4,500 bends in 49 current-day meandering rivers. About half of the rivers were unvegetated and half were densely or partly vegetated.

The researchers keyed in on point bars – the sandy landforms that develop on the inside bends of meandering rivers as water flow deposits sediments. Unlike the sandy bars that form in the middle of braided rivers, point bars tend to migrate laterally away from the centers of rivers. Over time, this migration contributes to meandering rivers’ characteristically sinuous channel shapes.

Recognizing that these sandy bars form in different places based on river style, geologists for decades have measured the trajectory of bars in the rock record to reveal ancient river paths. The rocks, typically of sandstones and mudstones, provide evidence for divergent river styles because each deposits different kinds of and amounts of rock-forming sediment, giving geologists clues for reconstructing long-ago river geometries. If sandstones showed little variation in the angle of bar migration, geologists interpreted the bars as moving downstream, and thus that a braided river created the deposits. 

Using this technique, geologists had noticed that rivers changed the way they behaved around the time that plants first evolved on Earth. This observation led to the conclusion that land plants made river meandering possible, for instance by trapping sediment and stabilizing riverbanks.

“In our paper, we show that this conclusion – which is taught in all geology curricula to this day – is most likely incorrect,” said Lapôtre, the paper’s senior author and an assistant professor of earth and planetary sciences at the Doerr School of Sustainability.

By looking at modern rivers with a wide range of vegetation cover, the researchers showed that plants consistently change the direction of point bar migration. Specifically, in the absence of vegetation, point bars tend to migrate downstream – like mid-channel bars do in braided rivers. 

“In other words, we show that, if one were to use the same criterion geologists use in ancient rocks on modern rivers, meandering rivers would be miscategorized as braided rivers,” Lapôtre said.

Rivers over time

The findings offer a provocative new window into Earth’s past eons, upending the conventional picture of how rivers have sculpted continents. If indeed carbon-loaded floodplains were laid down far more extensively over history, scientists may need to revise models of major natural climate swings over time, with implications for our understanding of ongoing climate change. 

“Understanding how our planet is going to respond to human-induced climate change hinges on having an accurate baseline for how it has responded to past perturbations,” Hasson said. “The rock record provides that baseline, but it’s only useful if we interpret it accurately.”

“We’re suggesting that an important control on carbon cycling – where carbon is stored, and for how long, due to river type and floodplain creation – hasn’t been fully understood,” he said. “Our study now points the way to better assessments.”

Additional co-authors are from the University of Padova and the University of British Columbia.


A drone view of the active channel and floodplain of Shoshone Creek in Nevada. The active river channel is moving through sediments it previously deposited. Former channel boundaries visible at the surface record the overall downstream migration of river bends, as Hasson et al. showed typically occurs in meandering rivers with bare, unvegetated banks. (Image credit: M. Hasson and M. Lapôtre)

Credit

M. Hasson and M. Lapôtre