Thursday, September 17, 2026

 

Study of bone strength reveals new clues about human evolution


By comparing the strength of fossilized limb bones, a research team led by the Keck School of Medicine of USC uncovered new evidence about the movement patterns of early human ancestors




Keck School of Medicine of USC

Australopithecus and early Homo

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On the right is a depiction of an early Homo human ancestor characterized by relatively greater bone strength of the femur in the thigh compared to the humerus in the arm. To the left is a depiction of an older human ancestor, Australopithecus, characterized by more equivalent strength in the bones of the arm and thigh. 

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Credit: Image: Cullen Townsend

 





Bipedalism, or walking on two legs, is one of the key features that distinguishes humans from other apes. But when and why our ancestors transitioned from a life often spent in trees to a life spent almost exclusively on the ground remains a subject of debate.

New evidence from fossils representing two groups of human ancestors—Australopithecus and early Homo—adds an important piece to the puzzle. In the study, just published in the journal Science Advances, an international team led by the Keck School of Medicine of USC analyzed fossil data from seven human ancestors ranging from about 1.5 million to 3.7 million years old.

The researchers measured the strength of arm and thigh bones, which adapt to the forces placed on them during life, to learn about how human ancestors used their bodies and moved through their environments. Animals that spend more time moving in trees tend to have relatively strong arm bones, while humans who walk upright on the ground tend to have stronger thigh bones.

The research team found that Australopithecus, an early ancestor that lived roughly two to four million years ago, had a distinct approach that resembles both modern apes and humans. These individuals had strong arms, suggesting they spent substantial time in trees, while the strength of their leg bones showed a more human-like pattern, suggesting they walked like humans on the ground.

“Australopithecus combined an ape-like upper limb strength with a human-like pattern in the legs, suggesting they had a unique movement strategy that has no modern comparison,” said Kristian J. Carlson, PhD, a professor of clinical medical education at the Keck School of Medicine and the study’s lead author.

The early Homo individuals, descendants of Australopithecus that lived about 1.8 to 2.3 million years ago, had relatively strong leg bones and weaker arm bones—a pattern more similar to modern humans. The findings suggest that the transition from Australopithecus to Homo included a major shift in how human ancestors moved and lived.

“We’re proposing that relative limb strength is a ‘threshold trait’—a difference that marks an important and fundamental shift in behavior between Australopithecus and Homo,” Carlson said.

Measuring bone strength

To estimate bone strength, the researchers collected computed tomography (CT) scans, which use X-rays to create a series of detailed images of the bones and their internal structure. Using these images, they calculated the thickness and quantified the structure of bone shafts and estimated how resistant the bones would have been to bending and twisting. They compared the strength of the upper arm, thigh and shin bones within each individual.

Australopithecus had relatively strong arms compared with its thighs, similar to modern apes. But when researchers looked at the legs specifically, comparing the strength of thigh and shin bones, they found a human-like pattern. This indicates Australopithecuswas already using its lower limbs for upright walking, while still using its upper limbs for movement in trees. In contrast, the early Homo individuals had relatively stronger thighs compared with their arms, resembling a modern human pattern.

The findings contribute to a longstanding debate over how much time Australopithecus spent on the ground versus in trees. While some researchers have argued that these early ancestors spent the majority of their time on the ground walking upright, the new evidence suggests they continued to spend substantial time in trees, Carlson said.

Bipedalism and brain size

Other studies have shown how bone features changed over many generations as bipedalism evolved. This study adds a different kind of evidence by showing how individuals used their limbs during their lifetimes—and supporting the idea that a major shift in movement occurred by roughly two million years ago.

The researchers suggest this behavioral shift is particularly intriguing when considered alongside another major change in human evolution: the dramatic increase in brain size that began around the same time. Scientists have proposed many explanations for the increase, including language, tool use and changes in how human ancestors found food. Carlson and his colleagues posit that the move toward walking greater distances on the ground may have contributed to both the shift in relative limb strength and the increase in brain size.

“We speculate that the shift toward more walking may have placed new demands on the body and brain, which could help explain why these changes happened around the same time,” Carlson said.

About this research

In addition to Carlson, the study’s other authors are Tea Jashashvili from the Keck School of Medicine of USC and the Department of Biological Sciences at USC Dornsife College of Letters, Arts and Sciences; Ronald J. Clark and Dominic Stratford and Kathleen Kuman from the University of the Witwatersrand, Johannesburg, South Africa; Christopher B. Ruff and Adam D. Sylvester from John Hopkins University; Jason L. Heaton from the University of Alabama-Birmingham; Travis R. Pickering and A.J. Heile from the University of Wisconsin—Madison; M. Loring Burgess from Harvard University; Lauren Sarringhaus from James Madison University; Timothy M. Ryan from Pennsylvania State University; Amelie Beaudet from the University of Poitiers, France; Robin H. Crompton from the University of Liverpool, United Kingdom; and David Lordkipanidze from Tbilisi State University and the Georgian National Museum, Tbilisi, Georgia.

This work was supported by Standard Bank and JP Morgan Chase; the Palaeontological Scientific Trust; the National Research Foundation (South Africa) African Origins Platform, Strategic Research Infrastructure Grant [#75430] and Centre of Excellence in Paleosciences; the National Science Foundation [BCS-2609570, SBR-8919155, SBR-8919749, BCS-1316104 and BCS-1419564]; the Wenner-Gren Foundation for Anthropological Research; the L.S.B. Leakey Foundation; and the Keck School of Medicine of USC.

Little Foot study points to major shift in how human ancestors moved



A major change in how our ancestors moved through their environment took place between about three million and 1.8 million years ago



University of the Witwatersrand

Little Foot

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In the foreground (right) is a depiction of an early Homo human ancestor characterized by relatively greater bone strength of the femur in the thigh compared to the humerus in the arm. In the background (left) is a depiction of an older human ancestor, Australopithecus, characterized by more equivalent strength in the bones of the arm and thigh. The authors’ findings document a shift in relative bone strength between these two ancestors, signaling a fundamental change in how they used their upper limb during daily interactions with the surrounding environment. In early Homo ancestors, it appears that the upper limb was no longer appreciably used in weight-bearing activities, such as arboreal movements, that appear to have characterized Australopithecus ancestors.

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Credit: Kris J Carlson





New research on the limb bones of the famous Little Foot skeleton from the Wits Sterkfontein Caves suggests that a major change in how our ancestors moved through their environment took place between about three million and 1.8 million years ago.

The study, published in Science Advances, finds that Australopithecus, the group of hominins that includes Little Foot, combined regular tree-climbing with walking on two legs on the ground. However, by about 1.8 million years ago, early members of the genus Homo appear to have shifted much more strongly towards a life on the ground.

The findings are based on comparisons of the relative strength of arm and leg bones in fossil human ancestors, modern humans and living apes.

Professor Kristian Carlson of the University of Southern California, who is affiliated with the Evolutionary Studies Institute at Wits University, says the results point to a fundamental difference between Australopithecus and later Homo.

“Early human ancestors such as Australopithecus appear to have used trees as much as modern chimpanzees and gorillas do today, but when they were on the ground they were walking on two legs,” Carlson says.

“That combination is important because there is no living species that provides a good behavioural comparison for them.”

The researchers added new data from the approximately 3.67-million-year-old StW 573 skeleton, known as Little Foot, from the Wits Sterkfontein Caves in South Africa, and fossils from Dmanisi in Georgia dating to about 1.8 million years ago.

They compared the strength of bones in the arms and thighs, as well as strength patterns within the lower limbs.

Little Foot and other Australopithecus fossils show relatively strong arms compared with their thighs, a pattern closer to African apes than to modern humans. This suggests their arms were still regularly exposed to the loads associated with climbing and moving in trees.

But Little Foot’s lower limb tells a different story. The relationship between the strength of the thigh and lower-leg bones is closer to the modern human pattern.

“This is one of the most surprising results,” Carlson says. “The Australopithecus individual has a modern human-like signal within the lower limb, while the relationship between the arm and thigh is much more African ape-like.”

He says the combination highlights how unusual Australopithecus locomotion was.

“These ancestors were not simply moving like chimpanzees, nor were they moving like modern humans. They seem to have combined substantial use of trees with regular bipedal walking on the ground.”

In contrast, the Dmanisi fossils and other early Homo and Homo erectus individuals show limb-strength patterns much closer to those of modern humans. The researchers interpret this as evidence that, by about 1.8 million years ago, the human lineage had become far more committed to walking on two legs on the ground and was using trees much less.

The researchers propose that the difference may represent a “threshold” between the adaptive patterns of Australopithecus and Homo, similar to other major changes used to distinguish stages of human evolution.

What caused the shift remains uncertain. The authors suggest it could be linked to changes in ranging, food gathering and other pressures that favoured stronger lower limbs and greater dependence on life on the ground.

They also note that the change took place during a broad period in which brain size was increasing in the human lineage.

“We are not saying that one change caused the other,” Carlson says. “But the timing is intriguing. We hope the possible relationship between changes in limb use, ranging behaviour and brain size will stimulate further discussion.”

The study includes researchers from Wits University’s Evolutionary Studies Institute and the Sterkfontein Caves research programme, together with international collaborators.

 

Speeding glaciers drive half a century of polar ice loss



The longest satellite record ever assembled shows that Greenland and Antarctica have lost 11.3 trillion tonnes of ice since the 1970s, raising global sea levels by more than 3 centimeters




Northumbria University

Image-1-Greenland.-Credit-Dr-Sammie-Buzzard-scaled

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Greenland

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Credit: Dr Sammie Buzzard (CPOM / Northumbria University)






The longest satellite record ever assembled shows that Greenland and Antarctica have lost 11.3 trillion tonnes of ice since the 1970s, raising global sea levels by more than 3 centimetres – and that most of the loss has come from glaciers flowing faster into the ocean, not from melting at the surface.

An international team of polar scientists has produced the most complete picture of ice loss from Greenland and Antarctica to date. The Ice Sheet Mass Balance Inter-comparison Exercise (IMBIE) Team combined 42 independent satellite surveys, drawing on 27 satellite missions and reaching back to 1972 for Greenland and 1979 for Antarctica using the early Landsat archive.

The findings show the two ice sheets lost 11,309 billion tonnes of ice between 1979 and 2023, pushing global sea levels up by 31.4 millimetres. Greenland accounts for the larger share and Antarctica contributed 13.3 millimetres. Strikingly, 84% of the combined loss was driven by glaciers speeding up and pouring more ice into the ocean, with just 16% due to surface melting. The polar ice sheets are now responsible for around a quarter of all global sea level rise.

The assessment was led by Dr Inès Otosaka and Professor Andrew Shepherd at Northumbria University, and Dr Tyler Sutterley of the University of Washington Applied Physics Laboratory. It is supported by the European Space Agency (ESA) and the US National Aeronautics and Space Administration (NASA) and is published in the journal Scientific Data.

Dr Inès Otosaka, who led the study, said: “By reaching back to the 1970s, we can now see how the ice sheets have changed across half a century. More than four-fifths of the ice lost was discharged into the ocean by faster-flowing glaciers, rather than melted at the surface – which tells us the long-term trend is being driven by the dynamic response of the ice sheets to a warming ocean.”

The record shows ice losses climbing steeply from the 1990s onwards. Greenland, close to balance in the 1970s, saw its rate of loss rise from around 60 billion tonnes a year in the 1980s to 264 billion in the 2010s, a decade marked by repeated extreme summer melt events. Antarctica’s rate rose from around 48 billion tonnes a year in the 1980s to 202 billion in the 2010s, with all of its net loss caused by ocean melting of its outlet glaciers; West Antarctica’s ice discharge, led by Pine Island and Thwaites glaciers, has risen in every decade of the record.

The most recent years (2020–2023) brought a temporary slowdown in ice loss. Record snowfall over East Antarctica have offset some of the continent’s glacier losses elsewhere, while a run of milder Greenland summers roughly halved its surface melting. Scientists caution these are short-term fluctuations against a clear long-term trend, not a reversal of ice loss.

The findings also underline the ice sheets’ central role in future sea level rise. Their response to a warming climate is the single largest source of uncertainty in sea level projections: high-end estimates of global sea level rise by 2150 increase by a factor of 2.6 once the risk of ice-sheet instability is accounted for. A continuous, half-century record of how the ice sheets are behaving
is therefore vital to anticipating the risks facing the hundreds of millions of people who live in low-lying coastal areas.

Professor Andrew Shepherd, Head of the School of Geography and Natural Science at Northumbria University and founder of IMBIE, said: “Three centimetres of sea level rise may sound small, but that puts another six to nine million people at risk of coastal flooding and erosion. With the ice sheets set to lose much more ice in the decades ahead, global assessments like IMBIE are vital to protecting communities impacted by climate change.”

Dr Tyler Sutterley, IMBIE co-lead, said: “The added length of the record, the larger pool of participating teams and our improved ability to assess uncertainties make this the most robust assessment of ice sheet mass balance produced so far. Satellites give us continent-wide, year-on-year evidence of what is happening now, and that is exactly what we need to test models and narrow the uncertainties in projections of future sea level rise.”

Dr Diego Fernández, Head of the Science Section at ESA, said: “These findings show the fundamental importance of using satellites to monitor the ice sheets and to evaluate the models used to predict the effects of climate change. Sustaining missions such as CryoSat-2 and the Sentinels, and maintaining the long-term ice-sheet climate data record, is critical for the decades ahead.”

 

Further information
To request an interview with the IMBIE Team, please contact the Northumbria University Press Office at media.communications@northumbria.ac.uk. Dr Inès Otosaka can be reached at ines.otosaka@northumbria.ac.uk.

A media package with the paper, films, animations and photographs is available at https://imbie.org/news/. The paper ‘Mass balance of the Greenland and Antarctic ice sheets from the 1970s to 2023’ by the IMBIE Team is published in Scientific Data. Embargoed until 10:00 London / 05:00 US Eastern on 16th September 2026.

Notes to editors
1. The study is an outcome of the Ice Sheet Mass Balance Inter-comparison Exercise (IMBIE), supported by the ESA Climate Change Initiative, the NASA Cryosphere Program, and the NERC UK Centre for Polar Observation and Modelling.

2. It combined 42 independent estimates – 23 for Greenland and 19 for Antarctica – from satellite altimetry, gravimetry and the input-output method, with regional climate models used to separate surface processes from ice dynamics. Data came from 27 satellite missions, including ESA’s CryoSat-2, the EU’s Sentinels, NASA’s ICESat-2, the NASA / German Aerospace Center GRACE missions, and the early Landsat archive.

3. 360 billion tonnes of ice is equivalent to roughly 1 millimetre of global sea level rise. Between 1979 and 2023 the ice sheets lost a combined 11,309 ± 565 billion tonnes (31.4 ± 1.6 mm); Antarctica lost 4,780 ± 513 billion tonnes (13.3 ± 1.4 mm) and Greenland 6,215 ± 467 billion tonnes since 1972. Ice dynamics accounted for 84% of the combined loss.

4. The dataset extends the previous IMBIE assessment (Otosaka et al., 2023), which reported a combined 21.0 ± 1.9 mm sea level contribution between 1992 and 2020.

Northumbria University

Northumbria University, Newcastle, is a research-intensive university whose Centre for Polar Observation and Modelling leads UK research into how the polar ice sheets are responding to climate change, using satellite observations. www.northumbria.ac.uk



Antarctica

Credit

Professor Alison Banwell (CPOM / Northumbria University)



Antarctica

Credit

Professor Andrew Shepherd (CPOM / Northumbria University).

Contains modified Copernicus Sentinel data (2024–2025), processed by ESA [VIDEO] | 



Sea level contribution data from IMBIE; Ice sheet elevation change from satellite altimetry (Centre for Polar Observation and Modelling) [VIDEO] 


Sea level contribution data from IMBIE; Ice sheet elevation change from satellite altimetry (Centre for Polar Observation and Modelling). In collaboration with Northumbria University, University Grenoble Alpes, TUD Dresden University of Technology, Jet Propulsion Laboratory, University of Washington APL, University at Buffalo University of Liverpool, University of California Irvine, Technical University of Denmark, NOAA Geophysical Fluid Dynamics Laboratory, Canadian Geodetic Survey, Utrecht University, Université Paris-Saclay, Delft University of Technology, European Space Agency, University of Liège, University College London, Bjerknes Centre for Climate Research, University of Edinburgh, Danish Meteorological Institute, University of Arizona, Alfred Wegener Institute, Aarhus University, NASA Goddard Space Flight Center, Lancaster University, Istituto Nazionale di Geofisica e Vulcanologia, isardSAT, University of Texas at Austin, Seoul National University, University of Bologna, Indian Institute of Science, WSL Institute for Snow and Avalanche Research SLF.

Credit

: ESA/NASA IMBIE Initiative

 

First-of-its-kind preventative phage therapy provides promising results




Virginia Tech

lab

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(From left) Roger Bataglioli and Hiba Baaziz in the lab.

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Credit: Photo by Felicia Spencer for Virginia Tech.






The mammalian gut microbiome is teeming with a delicate balance of bacteria and the viruses that keep them in check, called bacteriophages, or phages. Each bacterial species usually has its own set of phage partners. 

When bad bacteria enter this ecosystem, there are typically no phages present, allowing them to cause mayhem. By the time the host is sick, it is too late for phages; they’ll simply reach a balance with the bad bacteria.

But what if the phages in the gut could prepare for the orally ingested pathogen and strike it down as it enters the gut, negating the need for a battle?

Associate Professor and Blackwood Junior Faculty Fellow Bryan Hsu and his team recently demonstrated that this prophylactic approach, using an engineered nonpathogenic E. coli bacterium, successfully protected mice from an oral salmonella infection. Their work was published in Nature Microbiology.

The team believes this is a step toward an additional weapon against illnesses. 

“Eventually, in the future, this could be used to treat other diseases,” said Rogerio A. Bataglioli, a postdoctoral fellow in the Department of Biological Sciences and lead author of the study. “It’s not about replacing antibiotics but having one more option on the shelf to fight infections.” 

Bacteriophages, or phages, are viruses of bacteria and do not infect humans or animals. Hsu said phage therapy, the use of phages to treat bacterial infections, is particularly hard to make successful for treating intestinal pathogens. 

“It’s challenging, especially in the gut, because phages and bacteria tend to coexist for long periods of time,” said Hsu, an affiliate with Fralin Life Sciences Institute’s Center for Emerging, Zoonotic, Arthropod-borne Pathogens.  

This coexistence makes establishing the high phage-to-bacteria ratio needed to treat intestinal infections hard to achieve. 

“That’s extremely challenging to achieve in your gut,” Hsu said. “And then once you have a bacterial infection in your gut, a lot of times it’s just not even accessible to phages. It’s already hidden away in the mucosa or cells of your body; it’s not just free-flowing to where the phages would be able to access them.”  

To work around these impediments, the team engineered a nonpathogenic E. coli bacterium to carry a phage that only infects salmonella. This ensures that when the phage is produced, it can specifically target the pathogen.   

Usually, this type of salmonella phage remains dormant in the salmonella bacterial genome, but Hsu’s team made several genetic modifications so that it is carried by E. coli, and, once it is released into the gut, it automatically kills salmonella in a process called lysis. This process rapidly increases the number of phages to fight the bacteria. The researchers coined this new type of phage-bacterial combination a “lytic phage-producing lysogen,” or “lyto-lysogen.”

Salmonella can typically detect phage DNA produced by non-salmonella bacteria and prevent it from replicating. But in this case, the researchers were able to disguise the phage.

“We were able to trick the salmonella bacteria into thinking the phage from E. coli was ‘not foreign’ by adding a salmonella gene into the E. coli genome,” Bataglioli said. “A phage that comes from our E. coli can infect salmonella, can propagate easily in salmonella, lyse it, and then all the phages that are produced from salmonella can just keep replicating.” 

This rapid reproduction eventually leads to the eradication of the infection from the gut. 

“What happens is that this good bacteria, the E. coli, produces all this antipathogen phage, and there is now a protective lining so that when salmonella comes in, just after passing through the stomach and at its weakest point, it meets this high, killer density of phages,” Hsu said.  

The researchers say they targeted salmonella due to its high global disease burden, as it can kill the elderly, children, and those with HIV; it has a high prevalence of antibiotic resistance; and it has been upgraded to a high-priority pathogen by the Centers for Disease Control and Prevention. They believe this work, however, has strong implications for other illnesses. 

“We’re starting off with salmonella, but expanding, obviously, with the correct adaptations to target other diseases; other bacterial pathogens, would be an interesting route to explore,” Bataglioli said. 

“We have a framework in place that shows that we could potentially put other phages in there and target other bacteria,” Hsu said. 

Bataglioli plans to continue his bacteriophage research with the School of Chemical Engineering at the State University of Campinas in São Paulo, Brazil, in the fall.

Funding for this research was provided by the National Institute of General Medical Sciences of the National Institutes of Health. Bataglioli’s funding was supported by the Postdoctoral Fellowship in Drug Delivery from the PhRMA Foundation. 

Other researchers involved in this study include the following: 

  • Hiba Baaziz, Ph.D., lab manager, biological sciences 

  • Hallie Avalos, currently a graduate student at Vanderbilt University Medical Center 

  • Lindsay Smith, undergraduate researcher, College of Science 

  • Zach Baker, Ph.D., current postdoctoral researcher at Colgate-Palmolive 

  • Rita Makhlouf, graduate student, biological sciences

  • David Da Silva Barreira, Ph.D., current postdoctoral researcher at the University of Wisconsin, Madison 

  • Harsimran Kaur, Ph.D., presidential postdoctoral associate in biological sciences 

  • Teresa Southard, associate professor at the Virginia-Maryland College of Veterinary Medicine