Wednesday, April 23, 2025

 

Study lays out scientific path to recouping the costs of climate change




Dartmouth team reports the first scientific framework for tying emissions from individual fossil-fuel companies to specific damages linked to climate change




Dartmouth College





Drought-fueled wildfires in Southern California, a devastating hurricane in the southern Appalachian Mountains, and catastrophic floods in New England are among the most recent disasters to bring the increasingly astronomical costs of climate change into focus.

As a growing number of local and national governments struggle to recover from—and protect against—more frequent and destructive climate disasters, some have directly sought compensation from fossil fuel companies through civil cases and "polluters pay" laws. But many of these actions are being challenged or slowed in court, partly due to the difficulty in showing that specific climate impacts occurred because of any one company's greenhouse gas emissions.

new study published April 23 in the journal Nature, however, provides a tool for potentially recouping the costs of extreme weather amplified by climate change. The researchers lay out a scientific framework they report can be used to trace specific climate damages back to emissions from individual fossil fuel companies.

The framework combines climate modeling with publicly available emissions data to contrast the current climate and its impacts to what it would be like without the heat-trapping gases a company's activities released into the atmosphere. This causal link is known as a "but for" standard—as in, a climate catastrophe likely would not have occurred but for an individual firm's actions, the researchers report.

"We argue that the scientific case for climate liability is closed, even if the future of these cases remains an open question," says Justin Mankin, the study's senior author and associate professor of geography at Dartmouth. The study, he says, answers a question first posed in 2003 of whether science could ever link an individual firm's emissions to climate change.

"Just over 20 years later, we find the answer to be 'yes,'" says Mankin, who directs the Climate Modeling and Impacts Group at Dartmouth. "Our framework can provide robust emissions-based attributions of climate damages at the corporate scale. This should help courts better evaluate liability claims for the losses and disruptions resulting from human-caused climate change."

Mankin and the study's first author, Christopher Callahan, a postdoctoral scholar at Stanford who began working on the project as a PhD candidate at Dartmouth, deploy the framework to provide the first causal estimates of regional economic losses due to extreme heat resulting from the emissions of individual fossil fuel companies.

Extreme heat linked to carbon dioxide and methane from just 111 companies cost the world economy $28 trillion from 1991 to 2020, with $9 trillion of those losses attributable to the five top-emitting firms, according to the study. The highest-emitting investor-owned firm they examined may be responsible for $791 billion to $3.6 trillion in heat-related losses over that period, the researchers report.

"Our findings demonstrate that it is in fact possible to compare the world as it is to a world absent individual emitters," Callahan says.

"The affluence of the Western economy has been based on fossil fuels," he says, "but just as a pharmaceutical company would not be absolved from the negative effects of a drug by the benefits of that drug, fossil fuel companies should not be excused for the damage they've caused by the prosperity their products have generated."

The study, Callahan and Mankin say, benefits from 20 years of accumulating real-world climate impacts, the increased availability of climate and socioeconomic data, and methodological advances in "climate attribution science," a form of modeling that allows scientists to track the effects of climate change almost in real time.

Climate attribution is the crux of Vermont's 2024 Climate Superfund Act, which was partially informed by Mankin's testimony and an early version of the Nature study. Passed in the wake of devastating statewide floods in 2023, the law empowers the state attorney general to compel major fossil fuel companies to help cover the cost of disasters that can be scientifically linked to their emissions. A recent lawsuit challenges the state's authority to collect such damages, as well as Vermont's ability to accurately use climate attribution science to determine them.

The attribution framework reported in Nature incorporates established, peer-reviewed scientific methods for identifying the effect of specific emission levels on extreme weather. Callahan and Mankin also build on advances in the physical and social sciences that have drawn clearer connects between greenhouse gases, local climate change, and economic losses.

Critically, the model goes a step further than existing research by removing total emissions—measured in billions of tons—from the equation to identify a company's specific greenhouse gas footprint. Previous attribution models have hinged on concentrations of greenhouse gases in the atmosphere, which are measured in parts-per-million that are harder to attribute to specific sources, Callahan says.

"Our approach simulates emissions directly, allowing us to trace warming and its repercussions back to specific emitters," Callahan says. His and Mankin's focus on extreme heat builds on their previous work calculating global financial losses due to heat waves and the economic damages individual countries have caused to others by contributing to climate warming.

"Extreme heat is indelibly linked to climate change itself and the losses from it have been an instigator for legal claims. So, it's an obvious place to illustrate the broad application of our approach," Mankin says.

"We also live in a world that has warmed considerably over the past 20 years," he says. "This analysis is not a predictive exercise where we ask what the future holds. Instead, it's a documentary effort where we show what has already happened and provide the reason why."

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Melting glaciers at the end of the Ice Age may have sped up continental drift, fueled volcanic eruptions



University of Colorado at Boulder
Continental drift speeds up 

image: 

Graphic showing the Mid-Atlantic Ocean Ridge (red line) and how melting ice from Greenland caused changes in the motion of Earth's crust (purple arrows).

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Credit: Tao Yuan and Shijie Zhong





Around 10,000 years ago as the last Ice Age drew to a close, the drifting of the continent of North America, and spreading in the Atlantic Ocean, may have temporarily sped up—with a little help from melting glaciers, according to a new study from scientists at the University of Colorado Boulder.

In the new research, geophysicists Tao Yuan and Shijie Zhong used computer simulations, or models, to travel back about 26,000 years into the planet’s past. At the time, the massive Laurentide Ice Sheet, which stretched over North America as far south as Pennsylvania, started to recede. Melting ice flooded into the oceans, and sea levels worldwide rose by an average of around 1 centimeter per year.

The scientists discovered that this global thaw may have also had unexpected consequences—including for plate tectonics, or the internal clockwork that has, for billions of years, torn Earth’s continents apart and crushed them together.

According to the team’s calculations, the motion of the North American continental plate may have sped up by 25% as the ice melted. Between about 12,000 to 6,000 years ago, spreading at the Mid-Atlantic Ocean Ridge, which sits between the North American and Eurasian plates, may have increased by as much as 40%.

“As ice volume was greatly reduced, it caused a huge motion in Earth’s crust,” said Yuan, a graduate student in the Department of Physics at CU boulder. “Scientists knew that the ice melting caused the plates to uplift. But we show that they also moved a lot horizontally due to the ice melting.”

The researchers published their findings April 23 in the journal Nature.

Their results may have implications for the planet today. Ice sheets over Greenland are once again melting at a rapid rate, which, in a strange twist, could drive an increase in volcanic eruptions in Iceland not far away.

“That story that we’ve been telling for a long, long time—that processes like seafloor spreading and continental drift operate at timescales of millions of years driven by Earth’s internal engine, thermal convection,” said Zhong, a professor of physics. “That’s still true, but we show that glacial forcing can also cause significant motion on relatively short timescales of 10,000 years.”

Moving gears

The research, which was funded by the U.S. National Science Foundation, takes a deep dive into the Mid-Atlantic Ocean Ridge. This feature runs for thousands of miles down the center of the Atlantic Ocean and cuts through the island of Iceland. It’s a turbulent place: There, magma from deep within the planet bubbles up through the crust, cooling into solid rock and helping to force the continents of North America and Europe away from each other.

For generations, scientists believed that this process was largely steady—with the ridge spreading by a consistent 2 centimeters every year for the past several million years.

“That’s a fairly well-known, textbook number,” Zhong said.

But could the textbooks be wrong?

To find out, Zhong and Yuan used computer models to recreate the Earth as it was thousands of years ago. The researchers simulated what might happen as glaciers that were kilometers thick disappeared from modern-day Canada and Greenland—shifting that weight off dry land and into the ocean.

It helps to picture the globe as a memory foam mattress. If you’re lying on a mattress and get up, the foam will slowly bounce back to its original shape. Something similar happened on Earth as ice sheets melt, Zhong and Yuan said.

As the weight of the Laurentide Ice Sheet was redistributed around the planet, parts of North America began to bounce back up. (Today, land around Canada’s Hudson Bay is still rising by around 1 centimeter per year because of that rebound). According to the new study, the melting may have also affected the horizontal motion of North America and the Mid-Atlantic Ocean Ridge.

Volcanic eruptions

The thaw may also have had explosive consequences for Iceland, which sits not far away from Greenland, Yuan and Zhong said.

Geological evidence, for example, suggests that the island underwent a period of intense volcanic activity at the end of the last Ice Age, which has since quieted down. Enhanced spreading at the Mid-Atlantic Ocean Ridge due to ice melting from Greenland may have contributed to that fiery past—allowing more magma to rise to the surface, fueling the eruption of volcanoes and geysers.

“This pattern of volcanism may have been partly due to the glacial melting that we studied,” Zhong said.

Today, ice over Greenland isn’t melting fast enough to have much of an impact on the planet’s continental drift. But it could still have a major influence on Iceland over the next several hundred years, especially if glaciers begin to disappear at an accelerating rate.

“Ice sheets in Greenland and West Antarctica are still melting,” Yuan said. “We think the ice melting could enhance seafloor spreading and volcanism at nearby mid-ocean ridges in the future.”

 CANADA

Severe, lasting impairment that some consider ‘worse than death’ affects many residents after long-term care admission




Institute for Clinical Evaluative Sciences



Ottawa, ON, April 23, 2025 – 20% of residents newly admitted to long-term care became permanently unable to make everyday decisions for themselves within five years, according to new research from Bruyère Health Research Institute and ICES. 

A significant number of long-term care (LTC) residents experience states of severe cognitive and physical impairment, leaving them unable to make personal decisions—like what to eat or what to wear—and unable to communicate with staff or loved ones.  

“Our study set out to trace the experiences of residents newly admitted to long-term care, and those who lived a year or more in a state of severe disability,” says lead author Ramtin Hakimjavadi, Internal Medicine Resident at the University of Ottawa. “We should be talking more about what a meaningful, high-quality end of life looks like, given most older adults at this stage prioritize quality of life.”  

The study included 120,238 adults 65 and older who were newly admitted to LTC facilities in Ontario, Canada, between 2013 and 2018. Participants were followed until death, discharge from LTC, or April 1, 2023. 

Key Findings 

  • 20% of residents admitted to LTC became permanently unable to make everyday decisions for themselves, over the following five years and half lived for more than 262 days with this level of disability.  

  • 13% of residents admitted to LTC became totally dependent for all care including bathing, toileting and eating over the study period. Half of these people lived for more than 45 days with this level of disability.  

  • Residents under 80 years old and those who had dementia were more likely to live longer once they reached total care dependence and were unable to make any decisions for themselves. 

  • Residents with do-not-resuscitate or do-not-hospitalize orders did not live as long after developing impairment or severe disabilities compared to residents without advance care directives. 

“In interviews, long-term care residents have expressed that loss of independence is more distressing to them than the thought of dying. We are not offering resident-centered or evidence-based care if we don’t talk about the possibility of severe disability and ask about the circumstances when life prolonging treatments would not be acceptable,” says Hakimjavadi. 

In this population of LTC residents, 65% had a Do-Not-Resuscitate (DNR) order and 25% had Do-Not-Hospitalize orders. These advance care directives reduced time spent living with severe disability, likely because the residents' preferences were discussed, and care partners or providers knew how to support their end-of-life decisions.  

“Residents, their family members, and care teams should have open discussions about what quality of life means to the resident, considering the possibility of prolonged disability,” says senior author Dr. Daniel Kobewka, an investigator at Bruyère Health Research Institute and adjunct scientist at ICES.  

“Planning ahead can help ensure that future care aligns with personal values, including the choice to prioritize comfort and dignity over life-prolonging interventions,” adds Kobewka. 

 

ICES is an independent, not-for-profit research and analytics institute that uses population-based health information to produce knowledge on a broad range of healthcare issues. ICES leads cutting-edge studies and analyses evaluating healthcare policy, delivery, and population outcomes. Our knowledge is highly regarded in Canada and abroad and is widely used by government, hospitals, planners, and practitioners to make decisions about healthcare delivery and to develop policy. For the latest ICES news, follow us on BlueSky and LinkedIn: @ICESOntario 

The Bruyère Health Research Institute conducts world-class research to maximize quality of life and shape the future health care. As part of an academic sciences centre, our research supports evidence-based care with a focus on aging and long-term care, palliative care, rehabilitation and recovery, and social accountability. To learn more, visit http://www.bruyere.org.   

 

Remembering the cold: scientists discover how memories control metabolism




Trinity College Dublin





New multidisciplinary research led by Prof. Tomás Ryan from Trinity College Dublin shows that the brain forms memories of cold experiences and uses them to control our metabolism. This newly published study is the first to show that cold memories form in the brain – and map out how they subsequently drive thermoregulation.

The discovery may have important applications in therapies designed to treat a range of disorders – from obesity to cancer – in which thermoregulation and metabolism (or a lack of control in this area) plays a role, as well as opening the door to more fundamental research, which could help us better understand how memories impact our behaviour and emotions.

In 1897, the physiologist Ivan Pavlov first described classical conditioning, where animals and humans form associations between different aspects of the environment. He showed that dogs could be trained to salivate in hopeful anticipation of food, when an associated bell was rung. Classical or Pavlovian conditioning has since become a core staple of neuroscience and psychology.

Long-term memories are stored in the brain as ensembles of inter-connected cells, termed engrams. Increasingly, modern neuroscience is beginning to identify engrams that encode for bodily representations, such as experiences of infection; inflammation; food consumption; and pain. 

The researchers behind this work hypothesised that the brain may form engrams for temperature representations, and that these would serve to help an organism survive in changing temperatures. But to identity these engrams they first had to test whether cold memories could form in the first place. 

While memories are generally measured as changes in animal behaviour, the Ryan Lab collaborated with Prof. Lydia Lynch (then at Trinity College Dublin, now at Princeton University). They focused on metabolism as a first-order readout of cold experience, because mammals are known to increase their metabolism to create heat in the body when the environment is cold, via a process of adaptive thermogenesis.

Lead author of the article published today in the leading international journal, Nature,, Dr Andrea Muñoz Zamora, successfully trained mice to associate a cold experience of 4oC with novel visual cues that were only present in designated cold contexts. After a few days, mice were presented with the visual cues in the same context, but at room temperature. Crucially, the team discovered that the animals would upregulate their metabolism to induce predictive thermogenesis when they were “expecting” the environment to be cold.

Having established that mice could form memories of cold experiences, the team then delved into how this was happening in the brain. Using activity-dependent gene labelling, the scientists were able to genetically hitchhike onto the engram cells coding for the cold memory in a brain region known as the hippocampus. Remarkably, when these cold engram cells were artificially stimulated (using a technique called optogenetics), the mice increased their metabolism in order to generate heat. And in a converse experiment, to double-check the central finding, when cold engram cells were inhibited the mice were unable to express cold memories in response to the conditioned visual cues.

Dr Muñoz Zamora, said: “We discovered that when mice are exposed to a cold temperature they form memories that allow them to up-regulate their body's metabolism when they anticipate cold experiences in the future.”

Prof. Lynch added: “A large part of this learned control of body temperature seems to be due to increased activity of brown adipose tissue – or brown fat – which can be controlled by innervations originating in the brain. Our brain must learn from the bodily experiences of cold, but then feeds back to control how our fat cells respond to cold.”

Dr Aaron Douglas, who was joint lead author on the study, said: “Numerous clinical disorders, ranging from obesity to forms of cancer, may be treated by manipulating thermoregulation through brown adipose tissue. In the future, it will be important to test whether the manipulation of cold memories in humans could provide novel avenues for altering metabolism for therapeutic purposes.”

This research opens many new doors for further discovery research, as well as the development of treatments. Understanding how representations of cold experiences affect broader brain functions such as emotion, decision-making, and social behaviour will provide insights into the embodied nature of the mind, for example. 

“The sophisticated aspects of our minds evolved from more basic, visceral, bodily representations,” said Prof. Ryan. “Understanding how these components of our brain affect our behaviour in general is crucial to understanding our emotions and our use of memory.”

“This integrative piece of work offers a quintessential example of inter-disciplinary science. Neuroscience requires collaboration and it was the synergy with Prof. Lynch that allowed the unusual combination of memory engram work with metabolism research.”

 

Phoenician culture spread mainly through cultural exchange



Study challenges long-held assumptions about the Mediterranean Phoenician-Punic civilization, one of the most influential maritime cultures in history



Max Planck Institute for Evolutionary Anthropology

Punic Necropolis of Puig des Molins, Ibiza 

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Punic Necropolis of Puig des Molins on the island of Ibiza. The new ancient DNA study sequenced human remains from this and other important Phoenician-Punic archaeological sites.

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Credit: © Photo Raymar, MAEF




To the point

  • Secret of the Phoenician-Punic civilization's success: Their culture spread across the Mediterranean not through large-scale mass migration, but through a dynamic process of cultural transmission and assimilation.
  • Melting pot of ancient people: The study found that Punic populations had a highly variable and heterogeneous genetic profile, with significant North African and Sicilian-Aegean ancestry.
  • Highly interconnected: Ancient Mediterranean societies were cosmopolitan, with people from different regions trading, moving often over large distances and having offspring with each other. This provides new insights into the region's cultural and population history in the first millennium BCE. 

The Phoenician culture emerged in the Bronze Age city-states of the Levant, developing prominent innovations such as the first alphabet (from which many present-day writing systems derive). By the early first millennium BCE, Phoenician cities had established a vast maritime network of trading posts as far as Iberia, spreading their culture, religion, and language throughout the central and western Mediterranean.

By the 6th century BCE, Carthage, a Phoenician coastal colony in what is now Tunisia, had risen to dominate this region. These culturally Phoenician communities associated with or ruled by Carthage became known as “Punic” by the Romans. The Carthaginian empire left its mark in history, particularly well-known for the three large-scale “Punic Wars” with the rising Roman Republic, including the Carthaginian general Hannibal’s surprise campaign to cross the Alps.

Within the framework of the Max Planck-Harvard Research Center for the Archaeoscience of the Ancient Mediterranean, co-directed by Johannes Krause, Director at the Max Planck Institute for Evolutionary Anthropology, and Michael McCormick of Harvard University, an international team of researchers has now presented a study on the genetic history of these ancient Mediterranean civilizations.

New perspective on the spread of Phoenician culture

The new study aimed to use ancient DNA to characterize Punic people's ancestry and look for genetic links between them and Levantine Phoenicians, with whom they share a common culture and language. This was made possible by sequencing and analyzing a large sample of genomes from human remains buried in 14 Phoenician and Punic archaeological sites spanning the Levant, North Africa, Iberia, and the Mediterranean islands of Sicily, Sardinia, and Ibiza.

The researchers revealed an unexpected result. “We find surprisingly little direct genetic contribution from Levantine Phoenicians to western and central Mediterranean Punic populations,” says lead author Harald Ringbauer, who was a post-doctoral scientist at Harvard University when he began this research, and is now a group leader at the Max Planck Institute for Evolutionary Anthropology in Leipzig, Germany. “This provides a new perspective on how Phoenician culture spread—not through large-scale mass migration, but through a dynamic process of cultural transmission and assimilation.”

The study highlights that Punic sites were home to people with vastly different ancestry profiles. “We observe a genetic profile in the Punic world that was extraordinarily heterogeneous,” says David Reich, a professor of Genetics and Human Evolutionary Biology at Harvard University who co-led the work. “At each site, people were highly variable in their ancestry, with the largest genetic source being people similar to contemporary people of Sicily and the Aegean, and many people with significant North African associated ancestry as well.”

Ancient DNA reveals cosmopolitan nature of Punic world

The results underscore the Punic world's cosmopolitan nature. Individuals with North African ancestry lived next to and intermingled with a majority of people of mainly Sicilian-Aegean ancestry in all sampled Punic sites, including Carthage. Moreover, genetic networks across the Mediterranean suggest that shared demographic processes—such as trade, intermarriage, and population mixing—played a critical role in shaping these communities. The researchers even found a pair of close relatives (ca. second cousins) bridging the Mediterranean, one buried in a North African Punic site and one in Sicily.

“These findings reinforce the idea that ancient Mediterranean societies were deeply interconnected, with people moving and mixing across often large geographic distances,” says Ilan Gronau, a professor of Computer Science at Reichman University in ​​Herzliya, Israel, who co-led the work. He adds: “Such studies highlight the power of ancient DNA in its ability to shed light on the ancestry and mobility of historical populations for which we have relatively sparse direct historical records”. 

Painted Ostrich egg from the Punic necropolis in Villarricos (Spain). These eggshells were a popular Punic grave good, highlighting the cultural influence spreading from North Africa.

Credit

© Museo Arqueológico Nacional Madrid