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400,000-year-old Neanderthal Fire-Making Technology

Rob Davis explains how excavations by the British Museum at Barnham, Suffolk, have uncovered evidence for arguably the most important innovation in human history, the ability to make fire. 

Looking back through history and prehistory, it is clear how fundamental fire has been to the development of human civilisation. Great changes in human existence have had fire at the heart of them. The agricultural revolution required fire to turn crops into food, creating the surpluses that enabled the first towns, cities and monuments. The Copper Age, Bronze Age, Iron Age, all dependant on fire to extract metal from ore and shape and combine it to make tools, weapons, jewellery and more. The industrial revolution and space age, powered by combustion. Fire is not just utilitarian, it is prominent in belief systems across the world, both extant and historically documented. Prometheus, Vesta’s flame, Shiva the divine cosmic dancer, the burning bush, Sacred Fire, the Holy Spirit, incense, funeral pyres; fire emblematic of and a conduit to the divine. We are a species that has harnessed and exploited the transformative power of fire, not just to survive and thrive on this planet, but also to make sense of the world around us.

The Barnham evidence

sparks being produced by striking iron pyrite with a flint handaxe
Artist’s reconstruction of sparks being produced by striking iron pyrite with a flint handaxe. (Credit: Craig Williams, Illustrator, Department of Europe and Prehistory)

Since 2013, a team of archaeologists and scientists from the British Museum, Natural History Museum, Queen Mary University of London, UCL, University of Liverpool and Leiden University has been investigating the evidence for early fire-use at the Lower Palaeolithic site at Barnham, Suffolk. The evidence shows that the ability to create and control fire is not restricted to our own species, but a technology shared with other types of human that inhabited this world 400,000 years ago. Excavation of an ancient land surface has revealed an abundance of burnt materials associated with stone tools made and discarded by early Neanderthals. A patch of heated sediment, reddened like fired clay, is the remnants of a Neanderthal campfire. Adjacent to this is a cluster of artefacts, including fire-cracked handaxes, residues of fire-side activities. Most important of all, fragments of iron pyrite, brought to the site by Neanderthals for one purpose, to light fires by striking the pyrite with flint to create sparks. This is an extraordinary discovery, pushing back the earliest evidence for this technology by some 350,000 years.

Fire and early humans

Mastering fire is arguably one of the most important developments in human evolution. It seems likely that there is a very long history of human interaction with fire over more than a million years. It has been envisaged as a three stage process, beginning with foraging and scavenging in burnt landscapes following forest fires. The second stage involved the harvesting of wildfires, which were an occasional and unpredictable resource in the landscape. Embers collected in this way would have to be transported and then maintained, and once extinguished it became a waiting game for the next lightning strike. It is only with the third stage, the ability to create fire, that it could become a reliable addition to daily life. The knowledge of how to make fire enabled habitual use, which ultimately led to a reliance on fire for survival.

Artist’s reconstruction of an early human demonstrating the use of iron pyrite with flint to create sparks and light a fire
Artist’s reconstruction of an early human demonstrating the use of iron pyrite with flint to create sparks and light a fire. (Credit: Craig Williams, Illustrator, Department of Europe and Prehistory)

For early human hunter-gatherers, fire provided warmth and light and safety, a means to cook food to remove toxins and tenderise meat. It enabled humans to spread and thrive in colder, harsher environments, to explore subterranean spaces. Some of these benefits likely impacted biological and social evolution too. Cooking widened the range of available food sources and made food more readily digestible, which may have led to changes in the gut, but also freed up energy for development of the brain. Campfires acted as social hubs, focal points for interactions. Critically, fire extended the waking day by several hours. Humans live in complex social groups that require a significant daily time investment to maintain relationships. Socialising by firelight freed up daylight hours for hunting and gathering, collecting resources and making tools. It provided a setting for intense socialisation and development of language, storytelling and myth-making. With fire, humans could both feed and navigate larger, more complex societies.

The archaeology of early fire-use

Artist’s reconstruction of a group of early humans gathered around a fire after dusk
Artist’s reconstruction of a group of early humans gathered around a fire after dusk. (Credit: Craig Williams, Illustrator, Department of Europe and Prehistory)

There is still much we don’t know. To what extent is the evidence from Barnham representative of technological practises across the Palaeolithic world 400,000 years ago? Did other large-brained human species, such as the Denisovans in eastern Eurasia or early Homo sapiens in Africa, also light their own fires? And if so, did they invent fire-lighting technology independently, or adopt it through exchange of ideas and behaviours between human groups, or was it inherited from a common ancestor? How did the use of fire by early humans vary through time and space? 

The problem is that fire-use rarely preserves well in the archaeological record and, prior to the development of hearth structures, it is notoriously hard to demonstrate. Ash and charcoal can easily be blown or washed away, and baked sediments can be eroded and dispersed. Heated artefacts survive but it is often difficult to rule-out incidental burning in a wildfire. Many of our early sites preserve evidence of activities related to resource collection, tool production or butchery, situations that wouldn’t have necessarily called for the immediate use of fire. Domestic sites located in sheltered parts of the landscape outside of major river valleys or coastal plains are potentially underrepresented in the archaeological record. The evidence is patchy, ambiguous and hard to interpret.

In light of these challenges, it is the preservation of the evidence at Barnham that is exceptional, whereas the technology itself may have been widespread 400,000 years ago. Indeed, there are other sites of similar age that also provide evidence of fire-use in the form of baked sediments, charcoal and associated heated artefacts and bones. Notable sites include Beeches Pit, located just 10 km to the southwest of Barnham in Suffolk, Menez-Dregan and Terra Amata in France, and Gruta da Aroeira in Portugal. Together, these sites point to an increase in the importance of fire to early humans between 500,000 and 400,000 years ago. Barnham provides an explanation, the advent of fire-making.  

The transformative power of fire

Through time, humans would come to find ways to use fire to advance other technologies. The first archaeologically visible applications occur from 300,000 years ago. The rare survival of wooden artefacts at Schöningen, Germany, show the use of fire to harden spear tips. Tools begin to be hafted at this time, with evidence for the use of fire to produce birch bark tar for use as a glue for attaching stone blades and points to handles. At Qesem Cave, Israel, there is the earliest evidence for controlled heating of stone to improve its qualities for tool production. There was likely a multitude of other uses that do not leave an imprint on the archaeological record. Much later came ceramics and metals. Bit by bit, humans found new ways to utilise the power of fire to change the properties of materials and start to transform the world around them. 

Many aspects of early human day-to-day life are alien to most of us in the modern world. Few people today have made tools from stone or wood, foraged for nuts, roots and tubers, or hunted animals with spears and butchered them with stone tools. We do know fire, though. Sitting round a campfire, listening to the chatter and laughter of our companions while staring at the flickering flames, it feels timeless, primeval. This is a profoundly human experience, which connects us across deep time to early human societies, be they Neanderthal or Homo sapiens or any other fire-using species, and in doing so it speaks to their unmistakable humanity.

Further Reading

Davis, R.J, Hatch, M., Hoare, S., Lewis, S.G., Lucas C., Parfitt, S.A., Bello, S.M., Lewis, M., Mansfield, J., Najorka,J., O’Connor, S., Peglar, S., Sorensen, A., Stringer, C.B., Ashton, N.M. (2025). Earliest evidence of making fire. Nature.

Project team

Nick Ashton, Silvia Bello, Rob Davis, Marcus Hatch, Sally Hoare, Mark Lewis, Simon Lewis, Claire Lucas, Jordan Mansfield, Jens Najorka, Simon O’Connor, Simon Parfitt, Sylvia Peglar, Andrew Sorensen and Chris Stringer

With thanks to…

Mareike Stahlschmidt, Christopher Jeans, Will Lord and Craig Williams 

Duke of Grafton, Matthew Hawthorne, David Heading, Edward Heading, Richard Heading, David Switzer, Luke Dale, Xin Ding, Sophie Hunter, Dylan Jones, Izzy Klipsch, Murat Özturan, Aaron Rawlinson, Ian Taylor and Tudor Bryn Jones. 

The research has been funded by the Calleva Foundation.

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The Quest for Fire

Nick Ashton explains how four years of forensic investigations at Barnham in Suffolk demonstrate the world’s oldest evidence of making fire at 400,000 years ago.

Discovery

team starting to plan the strategy for excavation
Quarry cut in foreground revealing reddened cay beneath the black ancient soil. The team is starting to plan the strategy for excavation. (Photo: Rob Davis)

The first inkling that I had of something unusual was a small patch of reddened clay, almost terracotta in colour. It was a sunny afternoon in June 2021, and the seasonal excavation was midway through the three weeks, running like clockwork in the overgrown former claypit. I was surplus to requirements, so decided to investigate a quiet, shaded part of the site. The min-digger had provided a tantalising glimpse of a dark ancient soil in 2019, but with Covid in 2020, we hadn’t had time to investigate further. With half a thought for a quiet nap in the cool of the large oak, I instead picked up my spade and trowel, clearing the area of two seasons of leaf-litter and re-found the patch of dark organic-rich clay – the soil of an ancient landsurface.

Previous excavations of this 5 cm thick dark clay had revealed very little archaeology, but it marked much richer pond-edge sediments that lay underneath, containing flint flakes and tools, left by early Neanderthals over 400,000 years ago. A lone handaxe had been found on the landsurface in 1991, but some 15 m to the west. 

Trowelling down to the surface of the clay, revealed an area a metre across and on the front edge, the cut made by clay-pit workers over a century earlier. It was in cleaning down this steep edge that the reddened clay was first revealed, with dark clay above and below. My immediate thought was that the reddening indicated heating. I waited until the end of the afternoon when colleagues wandered over to take a look – a few raised eyebrows, gentle nods and the understated comment ‘intriguing’. We all shared that wonderful feeling of being on the threshold of an important discovery.

Excavation and proof

Having a hunch of early fire-use is not good enough, so it took four years to convincingly demonstrate that the heating was caused by humans, not part of a natural fire. Unfortunately, archaeology involves destruction, so trying to understand the extent of the reddened clay involved a lot of head-scratching to ensure we understood the form of the structure, as well as leaving enough in place for future researchers. We were fortunate, as one of our team was Claire Lucas, a brilliant excavator with much experience on similar sites in France. Tentative steps led to excavating diagonally opposed corners giving us a clear idea of the size – about 50 cm across – and enough sediment for analysis. In fact, quarrying in the 1900s had probably removed over half the structure.

Excavation of a Neanderthal fireplace at Barnham
Excavation of a Neanderthal fireplace at Barnham, Suffolk, UK. (Photo: Jordan Mansfield)

So how could we distinguish between natural and human burning? First, we had to demonstrate that the reddened clay had been heated and, if so, was it in situ? Fortunately, we now have a raft of geochemical tests and specialists in France, Germany, Austria and Britain who could help. Changes in the mineral structure of the clay showed heating to over 700 °C, while microscopic examination indicated that the sediment was in place, and not moved. Furthermore, tests suggested not just one burning event but repeated burning in the same place. The conclusion was clear – we had a campfire, or hearth, that had been used by people on several occasions.

But where were the humans? Excavation of surrounding areas revealed a concentration of flint artefacts around the campfire. Remarkably, this included four heat-shattered handaxes that gave us a direct link between people and the campfire. This matched up with four other sites in Britain, France and Spain with evidence of fire use, also dated to around 400,000 years ago. But there was one more surprise.

fire-cracked handaxe found next to a Neanderthal fireplace
A fire-cracked handaxe found next to a Neanderthal fireplace at Barnham, Suffolk, UK. (Photo: Jordan Mansfield)

Making fire

Human fire-use goes back deep in time (over a million years), perhaps by benefiting from wildfires and naturally cooked game. The next step was recovering embers to create campfires, but the critical turning point was the ability to make fire. From this point on, humans were no longer reliant on natural events but could regularly use fire where and when they wanted. When was this breakthrough? Sites in northern France had evidence of late Neanderthals making fire at 50,000 years, but a new piece of evidence from Barnham shows it to be considerably earlier.

fragment of iron pyrite
A fragment of iron pyrite found on a 400,000 year old land surface at Barnham, Suffolk, UK. (Photo: Jordan Mansfield)

In 2017 we had excavated an area of the landsurface towards the eastern end of the site that contained concentrations of heated flint. Here, we had struggled to demonstrate human fire-use. But in among the heated flint, we had found a tiny piece of iron pyrite. It is well known that pyrite can be used to strike flint to create sparks to light tinder, but we also know that it occurs naturally in chalkland areas, such as this part of Suffolk. Almost ignored for several years, we puzzled over the pyrite again, and in fact found a second piece, but how could we link the pyrite to making fire? It took a while, but a solution emerged.

I’ve worked with Simon Lewis from 1988, since when he has worked on the geological aspects of our joint projects, many in this area of Suffolk, the Breckland. Part of the work has involved identifying stones in the river and glacial deposits of the area to understand the processes behind their deposition – rivers bringing quartz and quartzites from the Midlands, or ice sheets with sandstone from Yorkshire. In total he has identified 121,000 stones from 26 sites in the Breckland – a fantastic database for checking on the prevalence of pyrite. We checked the old record sheets, then physically checked the samples from around Barnham – not a single piece of pyrite had been found through 36 years of systematic fieldwork. In other words, pyrite is incredibly rare in the Breckland. The conclusion is that humans brought pyrite to Barnham with the intention of making fire – the earliest evidence anywhere in the world.

Intelligent Neanderthals

There are some incredible long-term implications of fire-making which have been written about elsewhere – improved diet and digestion through cooking, enlargement of the brain and the social importance – but it also provides insights into the knowledge and intelligence of early Neanderthals. Making fire is not easy. They had the knowledge of where to collect pyrite, how to strike it against flint to create sparks, and the properties of effective tinder – some dried fungi can be used – to create fire. Once discovered, this knowledge had to be transferred to the next generations, perhaps around the embers of a dwindling fire.  

Further Reading

Davis, R.J, Hatch, M., Hoare, S., Lewis, S.G., Lucas C., Parfitt, S.A., Bello, S.M., Lewis, M., Mansfield, J., Najorka,J., O’Connor, S., Peglar, S., Sorensen, A., Stringer, C.B., Ashton, N.M. (2025). Earliest evidence of making fire. Nature.

Project team

Nick Ashton, Silvia Bello, Rob Davis, Marcus Hatch, Sally Hoare, Mark Lewis, Simon Lewis, Claire Lucas, Jordan Mansfield, Jens Najorka, Simon O’Connor, Simon Parfitt, Sylvia Peglar, Andrew Sorensen and Chris Stringer

With thanks to…

Mareike Stahlschmidt, Christopher Jeans, Will Lord and Craig Williams 

Duke of Grafton, Matthew Hawthorne, David Heading, Edward Heading, Richard Heading, David Switzer, Luke Dale, Xin Ding, Sophie Hunter, Dylan Jones, Izzy Klipsch, Murat Özturan, Aaron Rawlinson, Ian Taylor and Tudor Bryn Jones. 

The research has been funded by the Calleva Foundation.

 

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Climate signals from Hoxne

A new paper by Prof David Horne and colleagues sheds further light on the ‘Arctic Bed’ at Hoxne

The name ‘Hoxne’ has a special place in the lexicon of Palaeolithic archaeology. The brickyard and adjacent pits located near the village of Hoxne in northeast Suffolk have long been famous for John Frere’s discovery in 1797 of several “objects of curiosity”, which later become known as handaxes, and the recognition of their antiquity and significance. More recently John Wymer’s systematic excavations at the site in the 1970s provided a detailed account of the geology, environment and archaeology at the site. It is also an important site for Quaternary geology and biology more generally; Richard West’s classic work on the palaeobotany, published in 1956, provided a detailed assessment of the interglacial vegetation history at Hoxne, and was the basis of the formal definition in 1973 of the Hoxnian Stage of the British Pleistocene. This interglacial is now generally correlated with Marine Isotope Stage (MIS) 11 of the ocean record which dates to around 425,000 to 360,000 years ago.

Schematic section through the Quaternary deposits at Hoxne. The Hoxnian interglacial is represented by strata E-D and the cold interval by Stratum C.

A perhaps less well remembered but no less noteworthy contribution to research at Hoxne is that of Clement Reid (1853-1916). Reid, a geologist and palaeobotanist, and officer of the Geological Survey, is known for his detailed mapping and description of the Quaternary deposits in Britain and elsewhere, and, with his wife Eleanor, was one of the pioneers of the use of plant macrofossils to reconstruct past vegetation changes. Reid directed excavations at Hoxne in 1895 on behalf of the British Association. This work laid the foundations for understanding the site, and established the stratigraphic succession of a series of lacustrine clays (bed E), peat (bed D) and overlying lacustrine and fluvial sediments (beds C-A). Reid identified macrofossils of dwarf species of birch and willow in Bed C, hence the term the ‘Arctic bed’ for this part of the succession, which he regarded as being deposited during a period of cold climate conditions following the main part of the interglacial and succeeded by a further phase of temperate climate conditions when beds A and B were deposited.

A 50cm monolith through part of Stratum C at Hoxne, sampled during AHOB excavations in 2003
A 50cm monolith through part of Stratum C at Hoxne, sampled during AHOB excavations in 2003

One hundred and twenty-five years later, the Hoxne succession has again been investigated for its fossil content and palaeoclimatic significance. A new paper by Dave Horne and colleagues published in Quaternary Research provides quantitative palaeotemperature estimates from three invertebrate fossil groups; beetles, chironomids and ostracods, which are found within the Hoxne deposits, including Stratum (=Reid’s Bed) C. Using the results from the Beetle Mutual Climate Range (BMCR), the Chironomid Transfer Function (CTF) and the Mutual Ostracod Temperature Range (MOTR) methods, a multi-proxy consensus approach was used to reconstruct the temperature variations during the deposition of the Hoxne succession. The results indicate that summer temperatures during the Hoxnian interglacial were similar or up to 4oC higher and winter temperatures were similar or up to 3oC lower than today. In contrast the temperature reconstruction for Stratum C indicates summer temperatures 2.5oC cooler and winter temperatures between 5-10oC cooler than today. A return to more temperate conditions after the deposition of Stratum C, completes the warm-cold-warm oscillation represented at Hoxne. This climate signal can be correlated with sub-stage variations within MIS 11 of the deep ocean record and also provides a palaeoclimatic backdrop for human occupation of the site some 385,000 years ago.

The paper is not available under OA. However, it will be available on QMRO in due course.