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Hydrous mantle minerals reveal possible source of seismic anisotropy in stagnant slabs

Phys.org: Earth science - Sun, 05/24/2026 - 14:30
Seismic waves traveling through Earth's interior often propagate at different speeds depending on their direction, a phenomenon known as seismic anisotropy. Such anisotropy is commonly detected beneath subduction zones, particularly near stagnant slabs in the mantle transition zone and uppermost lower mantle. However, the physical origin of these signals has remained uncertain.

Enhancing GNSS-IR altimetry accuracy based on a novel gated memory sea surface height inversion model

Publication date: 15 May 2026

Source: Advances in Space Research, Volume 77, Issue 10

Author(s): Yifan Shen, Guangjian Xu, Liang Chen, Qiang Wang, Huizhong Zhu, Wei Zheng, Peifeng Kang, Shijie Zhao

A framework to identify winter fallow arable lands through machine learning methods

Publication date: 15 May 2026

Source: Advances in Space Research, Volume 77, Issue 10

Author(s): Dan Li, Wenzuo Zhou, Yichen Hu, Xinyu Yao

Integrating remote sensing and hydraulic modeling for suspended sediment concentration (SSC) estimation in the Zarrineh River, Iran

Publication date: 15 May 2026

Source: Advances in Space Research, Volume 77, Issue 10

Author(s): Seyedreza Dorri, Masoud Ghodsian, Mohammad Sharifikia

Can acoustic resonances in metals be excited by excitations of a bounded plasma? − First experiments

Publication date: 15 May 2026

Source: Advances in Space Research, Volume 77, Issue 10

Author(s): Anja Schlicht, Jan Kodet, Mario Hannemann, Boris Strelnikov

Exploring Kolmogorov–Arnold networks for hyperspectral crop classification – an evaluative study

Publication date: 15 May 2026

Source: Advances in Space Research, Volume 77, Issue 10

Author(s): Shruti Gupta, Ashish Kumar, Rahul Dev Garg, Neeraj Jain

LEO-augmented real-time kinematic with different multi-GNSS/multi-frequency combinations

Publication date: 15 May 2026

Source: Advances in Space Research, Volume 77, Issue 10

Author(s): Yang Sun, Pan Li, Liang Zhang, Zhiyuan Wu, Jingkai Yuan, Mingbao Wei, Meifang Wu, Kan Wang, Bao Shu, Guanwen Huang, Qin Zhang

Comparative analysis of surface albedo estimation methods using Landsat 8 and 9 satellite imagery over multiple ground observation sites

Publication date: 15 May 2026

Source: Advances in Space Research, Volume 77, Issue 10

Author(s): Emirhan Ozdemir

MP-Net: An end-to-end approach based on time-frequency fusion for earthquake magnitude prediction

Geophysical Journal International - Sat, 05/23/2026 - 00:00
AbstractAccurate and rapid magnitude prediction is critical for earthquake early warning systems, directly affecting emergency response decisions and public safety. With global seismic monitoring networks expanding to over 15,000 stations and the emergence of crowdsourcing-based IoT device monitoring systems, daily seismic data has reached petabyte scales, posing enormous challenges for real-time processing under the typical 3-10 second warning window constraint. Existing deep learning methods predominantly adopt single-modal information processing strategies, focusing either solely on temporal features of time-domain waveforms or spectral information after frequency-domain transformation, failing to fully exploit the joint evolution patterns and complementary information of seismic signals in the time-frequency domain, thereby limiting prediction accuracy and generalization performance. This paper proposes MP-Net, an end-to-end deep learning framework based on multi-scale time-frequency fusion for local magnitude (ML) prediction. The method employs a dual-branch architecture that simultaneously processes raw three-component waveforms and spectrograms: the time-domain branch captures features from microscopic waveform details to macroscopic energy evolution through parallel multi-scale convolutions; the frequency-domain branch combines hierarchical 2D convolutional networks with adaptive spectral attention mechanisms to automatically identify magnitude-related frequency components while suppressing noise; a cross-attention based fusion module achieves deep integration of complementary information from both modalities. To preserve the absolute amplitude information physically consistent with the ML definition, logarithmic amplitude features are extracted prior to waveform normalization and provided as auxiliary inputs to the fusion layer. Comprehensive experiments on the large-scale STEAD dataset demonstrate substantial improvements over baseline models: mean absolute error decreased to 0.28, coefficient of determination R2 reached 0.872, with 82.5% of predictions achieving acceptable precision (error≤0.5). The proposed approach provides an efficient and accurate solution for real-time single-station magnitude prediction, applicable to earthquake early warning systems operating in both centralized and distributed computing environments.

A Machine-learning-based Method for Integrating Seismic Data from Heterogeneous Sources

Geophysical Journal International - Sat, 05/23/2026 - 00:00
SummaryIn marine seismic exploration, various types of seismic sources are employed to visualize geological structures beneath the seafloor, depending on survey objectives. Airgun sources, which generate large amounts of energy by releasing compressed air underwater, are typically used for imaging deep area; however, they have limited vertical resolution due to their low peak frequencies. In contrast, sparker sources generate wavelets with high peak frequencies using bubbles produced by discharging electrical energy to vaporize water, resulting in high vertical resolution. Sparker sources are useful for the detailed imaging of shallow strata but have a shallow penetration depth due to their low source energy. This paper proposes a method to integrate airgun and sparker data to broaden the frequency bandwidth and thus achieve more accurate geological interpretations. The study used small-scale airgun data and sparker data acquired in Yeongil Bay, Pohang, South Korea. A machine-learning-based shaping filter model was developed along with synthetic training data representing the airgun and sparker source wavelet characteristics, and the trained models were applied to regularize these source wavelets. Subsequently, time-variant spectral whitening (TVSW) and weighted integration were performed to yield the flattened broadband frequency spectrum. The integrated data have enhanced penetration depth and vertical resolution compared with the original single-source datasets, thus overcoming the interpretational limitations imposed by their limited frequency bandwidth and penetration depth and enhancing the reliability of associated geological interpretations.

Estimation of site effects in the Kumamoto area, Japan, using aftershock acceleration records of the 2016 Kumamoto Mj 7.3 earthquake

Geophysical Journal International - Sat, 05/23/2026 - 00:00
SummarySite amplification in the Kumamoto area, Japan, is analyzed using 985 high-quality horizontal strong-motion records from 45 aftershocks (Mj = 2.7–4.9) recorded within 24 hours following the 2016 Kumamoto Mj 7.3 earthquake, as observed by 51 K-NET and KiK-net stations. For the generalized inversion technique (GIT), a reference station is required as a standard. In the GIT process, the number of events available for analysis is limited to those recorded by the reference station, and the stations whose site effects can be estimated are restricted to those that record common events with the reference station. To overcome the limitation of the GIT, the ‘transfer-station generalized inversion method (TSGI),’ a modified GIT, is introduced to increase the number of analyzed events and stations. The site responses obtained from GIT and TSGI for the same stations exhibit a high degree of consistency, thereby demonstrating the effectiveness of the TSGI. The discrepancies between the ${{Q}_S}$ estimates of GIT and TSGI can be attributed to the gradual expansion of the region represented by ${{Q}_S}$ as more events and stations are included in the inversion. However, the results of GIT and TSGI are relative to the reference station that may itself exhibit site effects. Thus, a reference-independent technique, i.e. genetic algorithm (GA), is also introduced to obtain the absolute site amplifications. The results show that at frequencies greater than about 1 Hz, the site response of the reference station is significantly lower than the theoretical amplification factor of 2, resulting in an overestimation of the site responses at other stations. When the results of GIT are corrected with the site response of the reference station obtained from GA, these two results agree very well for most of the stations. This indicates that the results of GIT are reliable if the reference station is an ideal surface rock station, and that the GA produces accurate absolute site amplification factors for the stations investigated in this study. In addition, we analyze the high-frequency attenuation characteristics of S-waves in the Kumamoto area, and establish $\kappa $ models for different site conditions and an empirical ${{\kappa }_0}$-${{V}_{S30}}$ relationship.

Some technologies use accelerated natural processes to capture carbon, but can they store it durably?

Phys.org: Earth science - Fri, 05/22/2026 - 20:20
Natural geological processes have been regulating Earth's climate for millions of years. Accelerated versions of these processes are now being promoted as technologies to draw down carbon from the atmosphere—and some are rapidly moving from concept to real-world deployments.

Arctic thaw unleashes mining-like pollution across hundreds of Arctic waterways

Phys.org: Earth science - Fri, 05/22/2026 - 20:00
Thawing permafrost is rapidly transforming dozens of Arctic streams into acidic, metal-laden waterways, according to new research published in Science. The study shows how thawing permafrost exposes sulfide minerals that react with oxygen and water—a process similar to what occurs in mining pollution. The reactions release acidity and heavy metals such as zinc, nickel, cadmium, and aluminum into surrounding waters.

NASA Announces “Realignment” Toward Human Spaceflight

EOS - Fri, 05/22/2026 - 17:37
body {background-color: #D2D1D5;} Research & Developments is a blog for brief updates that provide context for the flurry of news regarding law and policy changes that impact science and scientists today.

Today, NASA announced an agencywide realignment that includes combining related mission directorates to sharpen the agency’s focus on human spaceflight.

“This initiative reflects NASA’s extreme focus on executing the mission in direct support of the National Space Policy,” NASA Administrator Jared Isaacman said in a press release about the realignment.

The National Space Policy refers to Executive Order 14369: Ensuring American Space Superiority, which was released by the Trump administration in December 2025. The order sets national priorities of returning Americans to the Moon, establishing a lunar base, developing a nuclear reactor in space, developing the commercial space economy, and enhancing the United States’ national security space architecture.

NASA’s Artemis II crew captured this image of the Moon eclipsing the Sun during their flyby of the Moon on 6 April 2026. Credit: NASA

NASA’s six existing mission directorates will be slimmed down to four. Exploration Systems Development and Space Operations will be combined into a new Human Spaceflight Mission Directorate and will facilitate human spaceflight in low-Earth and lunar space environments. Aeronautics Research and Space Technology will be folded into a new Research and Technology Mission Directorate, tasked with researching and developing nuclear power and propulsion. The structure of the Science Mission Directorate (SMD) and Mission Support Directorate remain unchanged at the time of publication. All directorate leaders will now report directly to the NASA Administrator (Isaacman) to ensure that each remains focused on their directorate’s new mission.

“There will be no reduction in force, no program cancellations, no closures, but we will achieve cost savings through more efficient execution and taking an active role in delivering the outcomes the world has been waiting for from NASA,” Isaacman said.

More Efficient?

At first glance, it is hard to see how combining four mission directorates into two, refocusing the missions of each, and pushing for increased efficiency and cost reduction will not result in some loss of talent either through positions being eliminated or individuals finding themselves in jobs they do not want to hold.

In a letter to NASA employees, Isaacman went into more detail about the specifics of this realignment and described how it will shift the agency’s internal bureaucratic authority away from directorates and toward NASA’s field centers. Prior to this, centers like Goddard Space Flight Center in Greenbelt, Md., and Johnson Space Center in Houston would need to compete for funding that had been appropriated to directorates based on the programs or missions they were tasked with.

A NASA source based in Houston told Ars Technica that the competition for funding “has been an absolute disaster.”

 
Related

This new realignment “will adjust the funding distribution, so Centers have the financial support needed to sustain the baseline critical capabilities independent of near-term mission assignment,” Isaacman stated. “This shift will allow Center Directors to focus on maintaining the infrastructure, workforce, and capabilities required for current and future missions.”

Isaacman was unclear about when these changes will take effect, and policy analysts are unsure whether the realignment will be recognized by Congress through its appropriations process. The most recent Fiscal Year 2027 appropriations bill for NASA, which advanced out of the House Committee on Commerce, Justice, and Science on 13 May, allocates funding for six mission directorates, not four. The Senate appropriations committee is expected to release its proposed budget for NASA in the coming weeks, and the two bills must still undergo a lengthy reconciliation process.

In fiscal year 2026, Congress broke with the president’s budgetary priorities for NASA and passed a budget that ignored several of the administration’s proposed financial and mission cuts. Whether Congress will do the same this year and maintain the prior breakdown of directorates will become clear in the coming months.

—Kimberly M. S. Cartier (@astrokimcartier.bsky.social), Staff Writer

These updates are made possible through information from the scientific community. Do you have a story about how changes in law or policy are affecting scientists or research? Send us a tip at eos@agu.org. Text © 2026. AGU. CC BY-NC-ND 3.0
Except where otherwise noted, images are subject to copyright. Any reuse without express permission from the copyright owner is prohibited.

Rice feeds billions of people—but its role in fueling climate change is growing

Phys.org: Earth science - Fri, 05/22/2026 - 15:20
Rice feeds more than half the world. From terraced paddies in Southeast Asia to irrigated fields in China and India, it underpins daily meals for billions of people.

How the Great Pyramid of Giza has survived 4,500 years of Egyptian earthquakes

Phys.org: Earth science - Fri, 05/22/2026 - 14:00
The Great Pyramid of Giza in Egypt has survived more than 4,500 years. Earthquakes have repeatedly shaken the region, including the magnitude 5.8 Cairo earthquake in 1992, which dislodged some of the pyramid's outer casing stones. Yet the main body remained essentially intact.

Germany to Return Contested Dinosaur Fossil to Brazil

EOS - Fri, 05/22/2026 - 11:18

For many years a source of irritation, a fossil of the Brazilian spinosaurid Irritator challengeri is now bringing some joy to paleontologists in its homeland.

Following a successful public campaign for restitution, the piece is returning to Brazil from the collection of Germany’s State Museum of Natural History Stuttgart (SMNS), where it has been kept for the past 30 years—a situation that Brazilian paleontologists and lawmakers deemed illegal.

Representatives of both countries made the announcement last month during Brazilian President Luiz Inácio Lula da Silva’s visit to Germany. In a joint statement, they announced the German museum’s “willingness” to “hand over” the fossil to Brazil and start a new, more transparent era of international collaboration.

“It is a very expected and cherished move because it represents a huge scientific and social victory for the Global South and for Brazil.”

“Finally, the Irritator will be back to its original place,” said paleontologist Allysson Pontes Pinheiro, director of the Plácido Cidade Nuvens Paleontology Museum.

The museum, located in northeastern Brazil where the fossil was discovered in the 1990s, will host the Irritator when it returns to Brazil. “It is a very expected and cherished move because it represents a huge scientific and social victory for the Global South and for Brazil,” Pinheiro said, highlighting that the return will allow local scientists and the population to have access to a heritage that would be difficult and expensive to access abroad.

The Irritator challengeri fossil is one of many that have been illegally obtained from South America by researchers from the Global North. Considered the most complete spinosaurid skull ever described, the 110-million-year-old specimen was taken from the Araripe Basin in northeastern Brazil and described in 1995 by British paleontologist David Martill and his German colleague Eberhard “Dino” Frey. Martill and Frey worked on at least one other fossil smuggled from Brazil to Germany, an Ubirajara jubatus specimen, which was repatriated in 2023 and is currently housed at Plácido Cidade Nuvens.

Martill and Frey named the newly discovered species in reference to their irritation upon learning that the skull had been manipulated by fossil dealers to get a better price. Little did the researchers know that the fossil would irritate many other scientists, especially those from the animal’s homeland.

Revisiting a Fossil with “Problematic Status”

In 2023, triggered by the publication of a paper that acknowledged the fossil’s “problematic status,” paleontologists in South America published an open letter to the Ministry of Science, Research and Arts of Baden-Württemberg State demanding its return. The document received about 300 signatures from scientists and lawyers and was followed by a viral social media campaign involving influencers and a more recent public petition on Change.org that gathered more than 34,000 signatures.

“This campaign showed us that it is worth continuing to fight for our fossils.”

The restitution request is based on Brazilian legislation passed in 1942 that determined that fossils found in the country are the state’s property and cannot be traded or exported without explicit authorization. In addition, a more recent Brazilian ordinance (dating to 1990) mandates that any holotype (a fossil used to describe a new species, such as the contested Irritator specimen) must remain in the country. Regardless, SMNS maintained the fossil had been legally purchased from a private dealer in Germany in 1991.

“We are very happy the Brazilian law is now being respected,” said Aline Ghilardi, a paleontologist at the Federal University of Rio Grande do Norte who was at the forefront of the repatriation campaign. “This campaign showed us that it is worth continuing to fight for our fossils.”

At the time of publication, SMNS had not responded to requests for comment.

A Long Process of Decolonization

But Ghilardi is not entirely satisfied. She didn’t like the wording of the announcement, which used the expression “hand over” rather than return, repatriate, or restitute.

“The statement was a missed opportunity to demonstrate the German government’s willingness to decide in favor of a restitution process,” she explained. “It seems there is resistance to making these restitutions as actual restitutions. It appears as if it is theirs by right and that they will hand over the fossil to Brazil as part of scientific cooperation.”

Ghilardi expressed that she will believe the repatriation will actually happen only when a specific return date is announced. (As of publication, it has not.) She also hopes that the Irritator case is not an isolated incident, but part of an ongoing trend of restitutions intended to break the pattern of neocolonialism in science.

A 2025 study published by Ghilardi and colleagues in the journal Palaeontologia Electronica showed that of nearly 500 invertebrate species described from fossils found in the Araripe Basin—one of Brazil’s richest and most threatened regions of geodiversity—about half have holotypes stored in institutions across Europe, Asia, and North America, violating Brazilian law.

Most of these smuggled fossils are hosted in Germany. “Some foreign colleagues complained about our campaign, saying that it looked like we were persecuting Germany,” Ghilardi said. “But that is not the case. It is just the numbers.”

It is possible, she noted, that other countries hold even more specimens that were not described in the scientific literature and therefore could not be counted.

The same study also found that more than 200 species were described in publications that did not include any Brazilian scientists as coauthors, despite Brazilian legislation requiring foreign research on Brazilian fossil material to be conducted in partnership with local institutions.

Wave of Repatriation

Paleontologist Serjoscha Evers at the Universität Freiburg, who authored the 2023 study on the Irritator fossil, wrote in an email to Eos that he welcomed the news of the dinosaur’s return.

However, he also wondered whether the decision is just “a diplomatic favor that resulted from the public pressure, or foreshadowing a broader wave of repatriations based on a legal conclusion that the fossils are unlawfully in German custody.”

Paleontologists involved in the Irritator restitution efforts said that since the campaign began, they have been receiving emails from museums and institutions worldwide seeking information on the procedures for returning fossils to Brazil.

Germany recently said it would “hand over” the Irritator challengeri fossil to Brazil. This illustration suggests what the dinosaur would have looked like before it was a fossil, about 110 million years ago. Credit: PaleoGeekSquared/Wikimedia Commons, CC BY-SA 4.0

The Plácido Cidade Nuvens Paleontology Museum, the final destination of the Irritator, has received several restitutions itself, including 45 fossils originally collected from the Araripe Basin and previously held by the University of Zurich in Switzerland, the fossil of a crustacean that was in the possession of the Universidad Nacional del Nordeste in Argentina, and a fish fossil seized in Italy.

According to Pinheiro, the museum’s director, paleontologists and the Brazilian government have listed at least 90 Brazilian holotypes still held in Germany. And the Brazilian Ministry of Foreign Affairs confirmed to Eos that it is currently negotiating the return of nine fossils held in undisclosed countries.

“We have been talking with colleagues from the museums where these materials are hosted, and they seem very favorable to returning them,” Pinheiro observed. “It is a huge advancement and a great change of behavior from important museums that have been holding heritage from the Global South.”

—Sofia Moutinho (@sofiamoutinho.bsky.social), Science Writer

Citation: Moutinho, S. (2026), Germany to return contested dinosaur fossil to Brazil, Eos, 107, https://doi.org/10.1029/2026EO260167. Published on 22 May 2026. Text © 2026. The authors. CC BY-NC-ND 3.0
Except where otherwise noted, images are subject to copyright. Any reuse without express permission from the copyright owner is prohibited.

Weak Faults Play a Strong Role in the Tibetan Plateau’s Deformation

EOS - Fri, 05/22/2026 - 11:15

As the Indian and Eurasian continental plates collide, the Tibetan Plateau is slowly deforming. For decades, geoscientists debated how this deformation occurs: Is the plateau like a block of crumbly aged cheddar, deforming mostly at its faults, or is it more like French brie, moving like a very viscous liquid being pushed slowly to the east?

A new study published in Science shows that both theories are at work. The study’s findings provide the most comprehensive picture yet of the Tibetan Plateau’s deformation and offer valuable information for earthquake hazard assessments in the region.

The new model that combines the two theories is a “significant advance,” said Eric Fielding, a geodesist who was not involved in the study. Fielding is a staff member at NASA’s Jet Propulsion Laboratory but did not speak on behalf of the agency. “It’s clearly the result of a very large amount of work,” he said.

A Deformation Investigation

For decades, scientists have held differing views on the Tibetan Plateau’s deformation. One camp modeled the plateau’s deformation with movement occurring mostly at its faults, while the other modeled the movement like a thick fluid deforming areas beyond faults.

“These two communities have carried on modeling deformation in different ways” and have never fully resolved the differences between their models, said Tim Wright, a geodesist at the University of Leeds in the United Kingdom and lead author of the new study.

It’s tricky to measure the plateau’s deformation, though, because it changes so slowly: One of the fastest faults on the plateau, the Kunlun Fault, moves at about just 10 millimeters per year. “These are rates that are less than your fingernails growing,” Wright said.

And because much of the Tibetan Plateau’s terrain is inaccessible, there’s a dearth of ground-based stations to track movement, meaning most geodetic data for the area must come from satellites.

“It’s a boon for science to have that consistent acquisition of the same kind of data for 10 years.”

Tracking such nearly imperceptible movement with satellites hundreds of kilometers above requires enormous amounts of data collected over many years. Wright and his colleagues finally had those data after 10 years of observations from the European Space Agency’s Sentinel-1 satellite mission, which launched in 2014.

“Because the signals are so small, you need to wait for some time before you accrue enough deformation that you can actually measure it,” Wright said. The 2014–2024 data they analyzed are “giving us a really clean signal,” he said.

“It’s a boon for science to have that consistent acquisition of the same kind of data for 10 years,” Fielding said.

Using tens of thousands of satellite images alongside ground-based satellite navigation system stations, Wright and the team constructed comprehensive velocity maps of the deformation of the plateau. Results showed that a mix of theories best describes the mechanism.

“We think what’s really happening is a combination of both,” Wright said.

Wright, who described himself as “formerly of the viscous deformation camp,” was surprised by the prominent role that faults played in the plateau’s deformation. Previously, he said, he would have described the faults as passive markers within the underlying flow of the landmass. But the data show that the faults influence a much broader area of the plateau: “The whole deformation of the plateau is influenced by those faults,” he said.

The study “shows clearly that these major fault systems are responsible for a large part of the strain within the plateau,” Fielding said.

Mapping Seismic Hazards

“We have very little information about the history of earthquakes on these faults in this area.”

Knowing how the plateau deforms can also help scientists create more accurate seismic hazard assessments for the millions of people who may be affected by earthquakes there, particularly at the edges of the plateau. “We have very little information about the history of earthquakes on these faults in this area,” Fielding said.

The research team is working with the Global Earthquake Model Foundation, a nonprofit earthquake research collaboration, and other organizations to incorporate their findings into hazard assessments.

Wright and the research team recently used a similar methodology to map the deformation field of the entire Alpine-Himalayan belt, which stretches from Spain to eastern China. The same methods could be used to map the deformation of the western United States, another area where both viscous and fault-related deformation may affect large population centers, Fielding said.

—Grace van Deelen (@gvd.bsky.social), Staff Writer

Citation: van Deelen, G. (2026), Weak faults play a strong role in the Tibetan Plateau’s deformation, Eos, 107, https://doi.org/10.1029/2026EO260162. Published on 22 May 2026. Text © 2026. AGU. CC BY-NC-ND 3.0
Except where otherwise noted, images are subject to copyright. Any reuse without express permission from the copyright owner is prohibited.

Warm Waters Disrupt Seagrasses’ Microbial Environment

EOS - Fri, 05/22/2026 - 11:14
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Renske Jongen, an ecologist at the University of Sydney, calls seagrass ecosystems the “tropical rainforests” of the ocean. These underwater flowering plants offer habitats to marine life, protect coastlines from damage, and, like rainforests, store enormous amounts of carbon.

They’re also under threat from pollution, development, and warming ocean waters, which stress plants and slow growth rates. Seagrass populations have been declining globally for nearly a century, and recent estimates suggest 7% of seagrasses are lost worldwide each year.

A new study published in New Phytologist shows that warming waters may affect a microscopic aspect of the seagrass ecosystem, too: the microbes that live in their sediments. The new insight can inform efforts to restore seagrasses, the authors write.

Seagrasses are “getting attacked from both sides,” said Jongen, the lead author of the new study. Warming water stresses the plants themselves, while “something changes in the sediment that makes them grow worse.”

Sediments and Seagrass The research team transplanted seagrasses from elsewhere in Lake Macquarie to a preexisting, artificially warmed area to run their experiment. Credit: Renske Jongen

To test how microbial communities affect seagrass growth under warming temperatures, Jongen and the research team transplanted seagrasses and their sediment from both warm and cool areas of Lake Macquarie, a coastal saltwater lake in New South Wales, Australia, into an artificially warmed part of the lake. The artificially warmed part of the lake has received intermittent plumes of heated water from a nearby power plant since 1984, leading to a consistent temperature increase of 1°C–3°C (1.8°F–5.7°F) compared with the rest of the lake.

For half of the seagrasses, the team also used an autoclave, an instrument that uses steam to sterilize materials, to kill most of the microbes in their associated sediment before transplanting them to the experimental garden. “By looking at how plants respond with and without their microbes, you can get an idea for whether [those microbes] help or harm the plant under certain environments,” Jongen said.

The plants were then left to grow for 28 days before the team measured how they’d fared.

The warm-origin seagrasses in their original, warm-origin sediments with microbes intact grew the slowest once they were in the artificially heated waters, producing 35% less aboveground biomass than their counterparts whose sediment microbial communities had been killed. That result suggests that the microbial community in warmed sediment contributes to seagrass stress, the authors wrote.

“These plants, in general, do not like sediments that have been exposed to warmer temperatures.”

“These plants, in general, do not like sediments that have been exposed to warmer temperatures,” Jongen said. She was surprised that the plants that came from the warm areas had the worst outcomes but hypothesizes that perhaps these plants were already too stressed from warm waters to deal with the changes to sediment bacterial communities that occurred after they were transplanted into the even warmer part of the lake.

“It’s just like us, for example: When we don’t sleep or we’ve had a stressful week, then we get sick more easily,” she said.

Jongen said more research is needed to say for sure why warmed sediment seems to change microbial communities in a way that harms seagrasses. But research has shown that some microbes in ocean sediment produce sulfide, which can be toxic to seagrasses if it accumulates, especially if those seagrasses are already stressed. Warmer conditions may allow these sulfide-producing microbes to grow more quickly, harming the plants.

The new research highlights the “context dependency of host-microbe interactions,” said Karolina Zabinski, a marine ecologist at the University of California, Davis, who was not involved in the new study. Previous research by Zabinski and others also showed that seagrass growth depends on their associated sediment microbiome.

Restoration Lessons

The new study “serves as a great springboard” for both academics seeking to understand seagrass-microbe interactions and practitioners working on seagrass restoration in the field, Zabinski said.

For academic researchers, the paper raises exciting questions about how the microbial communities present in the sediment actually function, she said. Though the study identified the types of microbes in the seagrasses’ sediments, it didn’t evaluate the abilities of those microbes, which genes they possess or express, or how those microbes interacted with each other. “What are their actual genes, and what are they doing?” Zabinski asked.

“When plants don’t do well, we can’t just assume it’s inherent to the plants—we have to remember it could be driven by the microbes that they’re interacting with.”

For seagrass restoration practitioners, the study could offer new methods to try to improve restoration success. Some projects, for example, aim to take plants from warmer environments and transplant them to seagrass ecosystems that will face warming stress in the future as the climate changes. “It seems pretty intuitive that maybe those plants will have the traits or the genetics to respond to that warming,” said Randall Hughes, a marine ecologist at Northeastern University in Boston who was not involved in the new study. But the study’s results highlight “that intuition is not always reliable.”

“Certainly, having experimental studies like this helps us think about those restoration efforts in a more informed way,” she said. “When plants don’t do well, we can’t just assume it’s inherent to the plants—we have to remember it could be driven by the microbes that they’re interacting with.”

Jongen hopes to continue studying related questions about how seagrasses respond to warming waters. In particular, she’d like to investigate how long changes to the sediment microbial community last and whether those changes reverse once a marine heat wave subsides.

The research team collected sediments and seagrasses from different sites within Lake Macquarie before transplanting the plants into an artificially warmed area of the lake. Credit: Renske Jongen

Ultimately, the answers to these questions will help scientists better predict where seagrasses are in danger and how they might be helped. “If we lose the seagrasses, we don’t only lose the seagrasses, we lose all the other benefits that they provide,” Jongen said. “I think they deserve a little bit more attention.”

—Grace van Deelen (@gvd.bsky.social), Staff Writer

Citation: van Deelen, G. (2026), Warm waters disrupt seagrasses’ microbial environment, Eos, 107, https://doi.org/10.1029/2026EO260166. Published on 22 May 2026. Text © 2026. The authors. CC BY-NC-ND 3.0
Except where otherwise noted, images are subject to copyright. Any reuse without express permission from the copyright owner is prohibited.

Atlas reveals rocks with rare earth element potential, helping pinpoint new deposits

Phys.org: Earth science - Fri, 05/22/2026 - 09:00
A new atlas charts the global distribution of unusual, critical-metal-bearing igneous rocks, finding that they often form near the thick and ancient cores of the world's major continents. Researchers from Cambridge's Department of Earth Sciences mapped occurrences of CO2-rich igneous rocks—the world's primary source of rare earth elements—finding that their distribution is strongly tied to variations in Earth's rigid outer layer, the lithosphere.

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