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Orangutans can’t master their complex diets without cultural knowledge


Researchers reveal just how much wild orangutans depend on social learning to build diets spanning hundreds of different foods.


Max Planck Institute of Animal Behavior

Orangutans Can’t Master Their Complex Diets Without Cultural Knowledge 

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A young orangutan (Cinnamon) peers at her mother (Cissy) whilst using a stick to fish termites from a nest.

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Credit: Guilhem Duvot





When a wild orangutan leaves its mother after spending many years by her side, it has a mental catalog of almost 250 edible plants and animals, and the knowledge of how to acquire and process them.

A new study in Nature Human Behaviour reveals that no lone orangutan could build this encyclopedic knowledge through trial and error. Instead, this knowledge forms a “culturally-dependent repertoire”— a diverse set of knowledge that is only attainable through years of watching and exploring alongside others.

As humans, we must learn broad repertoires of knowledge to survive and thrive—ranging from local customs, to the skills to engineer new innovations like fishing spears and iPhones. Much of this cultural knowledge is too broad or complex for any single human to innovate from scratch in their lifetime. Rather, culture accumulates from the innovations of many individuals. Until now, it has been unclear whether similar processes are at play for wild non-human species. An international team of researchers has now investigated whether the breadth of wild orangutans’ diets exceeds what any one individual could acquire on their own within a relevant time frame.

“We provide convincing evidence that culture enables wild orangutans to construct repertoires of knowledge that are much broader than they could otherwise learn independently,” says first author Dr Elliot Howard- Spink, postdoctoral researcher from the Max Planck Institute of Animal Behavior, now a researcher at the University of Zürich.

“These diets must be the product of experiences and innovations of many other individuals, which have accumulated over time,” adds coauthor Dr Claudio Tennie, University of Tübingen. “The roots of humans’ cultural accumulation may therefore reach back at least 13 million years to our last common ancestor with great apes.”

Simulating how orangutans learn what to eat

The team wanted to know if young orangutans can independently learn their full set of edible plant and animal species before they become self-sufficient adults at around 15 years old—or if they need to learn this information from others. The researchers used extensive data collected on wild Sumatran orangutans living in the swamp forests of Suaq Balimbing, Indonesia. This included 12 years of daily observations, where the behaviors of orangutans were recorded every few minutes.

But this data set alone was not enough. The team needed to create scenarios in which young orangutans were cut off from different types of social interactions as they grew. “We would never do this to wild orangutans,” says Howard-Spink. Also, it was impossible for the scientists to follow orangutans every single day over the many years it takes the animals to grow up, while also recording all their learning opportunities. So, the scientists devised another way.

Using daily snapshots of real-life data, Howard-Spink built a simulation model that reenacted orangutans’ lives from birth to maturity at fifteen years old. The model incorporated three key social behaviors predicted to influence how the diet of orangutans develop: close-range observation of others while they ate foods in the forest (a behavior called ‘peering’); being in very close proximity to other orangutans who were feeding (which made them more likely to explore similar foods); or, simply being guided to suitable feeding sites, without any further social contact.

“Every single parameter of this model is based on our long-term data from wild orangutans,” says Dr Caroline Schuppli, who lead the study and is a group leader at MPI-AB. “It allows us to pinpoint which types of social interactions help young orangutans learn what to eat, and even to rank their importance.”

When all three types of social learning were available (the condition most similar to wild individuals), simulated orangutans cultivated adult-like diets—about 224 food types—at around the same age as wild orangutans. These similarities between the model and the wild confirmed the simulation’s accuracy and real-world applicability, the authors say.

“The fact that our simulation matched wild individuals’ development so closely is due to the extensive and uniquely detailed data collected from the wild at Suaq, and the hard work of a large team involved,” says Howard-Spink.

Discovering orangutans’ “cultural cuisine”

Howard-Spink then began cutting the simulated orangutans off from different social interactions. Just cutting off close-range observations (peering), had an effect: simulated orangutans had slower diet development and reached only 85% of the full wild diet repertoire by adulthood. But removing both peering and close-proximity associations left simulated apes with drastically narrower diets. These diets never approached the breadths possessed by wild adults, and essentially stopped developing well before the end of immaturity.

“Socially-isolated, simulated orangutans still had hundreds of thousands of opportunities to encounter food items during development,” says Howard-Spink. “But even massive amounts of exposure to food could not replace what was lost when they couldn’t engage in these social interactions.”

Says coauthor Andrew Whiten, University of St Andrews: “We’re seeing the strongest evidence yet that orangutan diets are culturally accumulated over many generations.”

The next step is to understand how this culturally-accumulated knowledge influences orangutans’ energy intake, survival, and success. “Given how much diet development suffers without social inputs, the effect of culture on orangutans’ daily lives is potentially profound,” adds Whiten.

The team will address this question as part of a further study. “We will again use empirically-validated simulations to understand how reliant orangutans are on cultural knowledge to survive and thrive in wild habitats,” says Schuppli.

Conserving accumulated cultures

Adult orangutans are generally solitary, making their long childhoods a precious window for cultural transmission. “In the wild, the constant presence of a mother, and fleeting associations with other individuals, are critical for orangutan learning and development during the early years,” says Schuppli. “It offers a crucial apprenticeship that paves the path to independence.”

With orangutan populations dwindling, this study has practical urgency. Orphaned apes, reintroduced without the full breadth of a wild diet, or introduced in different environments, may face starvation or poisoning from unfamiliar plants. “Reintroduction programs already teach orangutans to feed themselves outside captivity,” adds Schuppli. “Our study emphasizes how important this is to pass on their full cultural menu, so that these animals have the greatest chance of success in the wild.”

 

Ancient rocks reveal themselves as ‘carbon sponges’



University of Southampton
Cores 

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Cores of lava breccia, cemented with white calcium carbonate minerals, recovered from IODP Site U1557

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Credit: IODP JRSO





Sixty-million-year-old rock samples from deep under the ocean have revealed how huge amounts of carbon dioxide are stored for millennia in piles of lava rubble that accumulate on the seafloor.

Scientists have analysed lavas drilled from deep under the South Atlantic Ocean to understand how much CO2 is captured within the rocks due to reactions between the rocks and ocean.

The research, led by the University of Southampton, found that piles of lava rubble, formed due to erosion of seafloor mountains, form geological sponges for CO2.

It’s the first time the role of lava rubble as carbon sponges has been fully appreciated, and the research reveals secrets about Earth’s long-term carbon cycle.

Lead author of the research Dr Rosalind Coggon, Royal Society Research Fellow at the University of Southampton, said: “We’ve known for a long time that erosion on the slopes of underwater mountains produces large volumes of volcanic rubble, known as breccia – much like scree slopes on continental mountains.

“However, our drilling efforts recovered the first cores of this material after it has spent tens of millions of years being rafted across the seafloor as Earth’s tectonic plates spread apart.

“Excitingly, the cores revealed that these porous, permeable deposits have the capacity to store large volumes of seawater CO2 as they are gradually cemented by calcium carbonate minerals that form from seawater as it flows through them.”

Understanding past changes in the long-term carbon cycle

The movement of carbon between Earth’s interior, oceans, and atmosphere over millions of years controls how much CO₂ is in the air, which affects Earth’s climate.

To understand past climate changes, scientists study how much carbon moves in and out of different parts of the Earth system.

Dr Coggon explained: “The oceans are paved with volcanic rocks that form at mid-ocean ridges, as the tectonic plates move apart creating new ocean crust. This volcanic activity releases CO₂ from deep inside the Earth into the ocean and atmosphere.  

“However, ocean basins are not just a container for seawater. Seawater flows through the cracks in the cooling lavas for millions of years and reacts with the rocks, transferring elements between the ocean and rock. This process removes CO₂ from the water and stores it in minerals like calcium carbonate in the rock.”

The study determined how much CO2 is stored in the ocean crust, due to this process.

“While drilling deep into the seafloor of the South Atlantic, we discovered lava rubble that contained between two and 40 times more CO2 than previously sampled lavas,” said Dr Coggon.

“This study revealed the importance of such breccia, which forms due to the erosion of seafloor mountains along mid-ocean ridges, as a sponge for carbon in the long-term carbon cycle.”

The research was part of Expedition 390/393 of the International Ocean Discovery Program.

ENDS

Research vessel Joides Resolution

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Dr Rosalind Coggon

Dr Rosalind Coggon examining cores of upper ocean crust lavas cored during IODP Expedition 390

Credit

Alyssa Stephens, IODP JRSO

 

Antarctic mountains could boost ocean carbon absorption as ice sheets thin



Research led by polar scientists from Northumbria University has revealed new hope in natural environmental systems found in East Antarctica which could help mitigate the overall rise of carbon dioxide in the atmosphere over long timescales.



Northumbria University

Photo 1: Glaciers transport sediments from Antarctica to the coast. Credit: Dr Kate Winter, drone footage 

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Glaciers transport sediments from Antarctica to the coast. Credit: Dr Kate Winter, drone footage

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Credit: Credit: Dr Kate Winter, drone footage





Research led by polar scientists from Northumbria University has revealed new hope in natural environmental systems found in East Antarctica which could help mitigate the overall rise of carbon dioxide in the atmosphere over long timescales.

As Antarctica's ice sheets thin due to climate change, newly exposed mountain peaks could significantly increase the supply of vital nutrients to the Southern Ocean which surrounds the continent, potentially enhancing its ability to absorb atmospheric carbon dioxide, according to the research published in Nature Communications.

A team of scientists with expertise in oceanography, ice sheet modelling and geochemistry contributed to the study which looked at analysis of sediment samples from East Antarctica's Sør Rondane Mountains. They discovered that weathered rocks exposed above the ice surface contain iron concentrations up to ten times higher than previously reported from the Antarctic continent. This bioavailable iron is transported to the ocean by glaciers and icebergs, where it fuels the growth of phytoplankton – microscopic marine organisms that absorb CO₂ through photosynthesis.

The study found that sediments from mountain peaks protruding through the ice – known as nunataks – had over three times more extractable iron compared to sediments already being transported by glaciers. Some visibly rust-stained rock samples showed particularly elevated iron levels, suggesting that weathering processes on exposed surfaces create especially nutrient-rich material.

"Our results show that exposed bedrock in Antarctica acts like an iron factory," explained Dr Kate Winter, Associate Professor in the School of Geography and Natural Sciences at Northumbria University and lead author of the research paper. "Even though air temperatures rarely rise above freezing, sunlight can heat dark rock surfaces above 20°C in summer, creating the conditions needed for weathering and the formation of bioavailable iron compounds."

Dr Winter has travelled to Antarctica on fieldwork several times in recent years and has been supported by a Baillet Latour Antarctica Fellowship – a joint initiative of the Baillet Latour Fund and the International Polar Foundation (IPF). It provides scientists with the opportunity to conduct original research in East Antarctica’s cutting-edge Princess Elisabeth Antarctica research station.

Satellite observations confirm that coastal waters near to glacier outlets in the study region experience recurring phytoplankton blooms, demonstrating the biological importance of this natural iron delivery system. The blooms contribute to the Southern Ocean's role as a major carbon sink, absorbing atmospheric CO₂.

Dr Winter added: “The exciting thing is that we can take some hope from these findings because we know that carbon dioxide is a really important factor in climate change. From our research we now know that sediments from the Antarctic continent could help to draw down atmospheric carbon dioxide into the ocean. Whilst our study area is limited to one glacier system, what we need to understand is the potential impact of these many small amounts being drawn down together across the whole of Antarctica. Piecing together information to gather an accurate picture of how much these natural systems are working to reduce the amount of carbon in the atmosphere is crucial.”

However the research team, which includes scientists from the universities of Newcastle, Swansea, Plymouth, Edinburgh and Leeds, caution that there is a significant time lag in this process. Using ice flow models, they calculated that it takes between 10,000 and 100,000 years for iron-rich sediments collected in the mountains to reach the coast via glacial transport.

Dr Sian Henley, a marine scientist from the School of GeoSciences at the University of Edinburgh explained: “While the sediments we examine in the mountains today will take a long time to reach the ocean, we know from seafloor surveys that iron-rich sediments have been delivered to the coast for millennia, so the processes we record today give us a glimpse into changes we might expect to see in the future, as glaciers thin and more mountain surfaces are exposed in Antarctica.”

The study suggests that as temperatures continue to rise, several factors will increase iron delivery to the Southern Ocean:

  • More mountain peaks will emerge as ice sheets thin
  • Increased rock slope failures will deliver more sediment to glaciers
  • Enhanced weathering will produce more bioavailable iron compounds
  • Icebergs carrying this iron-rich sediment will distribute nutrients across vast ocean areas

The research provides important insights into how Antarctica's extreme environment connects with ocean ecosystems and the global carbon cycle. It also offers a glimpse into how this system may evolve as climate change continues to reshape the continent.

Discover more about research at Northumbria University which examines the future of ice on Earth.

FURTHER INFORMATION:

Visit the Northumbria University Research Portal to find out more about Dr Kate Winter’s work.

Thinning Antarctic glaciers expose high-altitude nunataks delivering more bioavailable iron to the Southern Ocean was published in Nature Communications on Monday 24 November 2025.

 

DOI: 10.1038/s41467-025-65714-y

 

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Dr Kate Winter collecting glacial sediments in Dronning Maud Land. Credit: Jacque Richon, IPF

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Credit: Jacque Richon, IPF


The Princess Elisabeth Antarctic Research Station is conveniently situated next to coastal margin mountains in East Antarctica. Credit: Dr Kate Winter, drone footage

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Credit: Dr Kate Winter, drone footage


Dr Kate Winter in East Antarctica. Credit: Jacque Richon, IPF

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Credit: Jacque Richon, IPF


During her fieldwork, Dr Kate Winter worked alongside renowned polar explorer Alain Hubert, who founded the International Polar Foundation. Credit: Henri Robert, IPF

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Credit: Henri Robert, IPF