Palaeolithic Palaeolithic (Old Stone Age) Britain is the period of the earliest known occupation of Britain by humans. The oldest known occupations of the island date to the end of the early Pleistocene, around 900,000 years ago. During the Palaeolithic, Britain was repeatedly colonised by archaic humans during temperate
interglacial periods, before retreating during the harsh cold
glacial periods. This process of colonisation and retreat is thought to have occurred at least 9 separate times. Habitation was intermittent, and even during periods of occupation may have reproduced below replacement level and needed immigration from elsewhere to maintain numbers. According to
Paul Pettitt and Mark White: : The British
Lower Palaeolithic (and equally that of much of northern Europe) is thus a long record of abandonment and colonisation, and a very short record of residency. The sad but inevitable conclusion of this must be that Britain has little role to play in any understanding of long-term human evolution and its cultural history is largely a broken record dependent on external introductions and insular developments that ultimately lead nowhere. Britain, therefore, was an island of the living dead. Prior to around 130,000 years ago Britain was permanently a peninsula of mainland
Europe, connected by chalk and clay rocks running across to northern France, allowing hominins to freely disperse into Britain. From around 500,000 years ago this land bridge began to erode, which was complete by around 130,000 years ago, resulting in Britain being an island during the
Last Interglacial (130-115,000 years ago) and most the
Holocene (from around 9,000 years ago), though it reconnected to Europe during
Last Glacial Period (115,000-11,700 years ago) and remained connected into the early Holocene via
Doggerland.
Paleomagnetic analysis shows that the sediments in which the stone tools were found have a reversed polarity which means they over 780,000 years old, prior to the
Brunhes–Matuyama reversal. The evidence is that the early humans were there towards the end of an
interglacial during that date range. There are two candidate interglacials - one between 970,000 and 935,000 years ago and the second from 865,000 and 815,000 years ago. Summer temperatures at Happisburgh were an average of and average winter temperatures were slightly colder than present day temperatures, around freezing point or just below. Conditions were comparable to present-day southern Scandinavia. Chronologically, the next evidence of human occupation is at
Pakefield on the outskirts of
Lowestoft in
Suffolk south of Happisburgh, dating to an interglacial period around 700,000 years ago (
Marine Isotope Stages 19-17), with lithic artefacts showing a core and flake industry. This site is in the vicinity of the lower Bytham river, and not the Thames which had now moved further south. Pakefield had mild winters and warm summers with average July temperatures of between . There were wet winters and drier summers. The oldest skeletal remains of humans in Britain are of "
Boxgrove Man", comprising a tibia and two incisor teeth from the lower jaw, suggested to represent remains of
Homo heidelbergensis, collected from the
Boxgrove site in West Sussex, dating to around 480,000 years ago at the end of Marine Isotope Stage 13. This site has also provided abundant evidence of human activity, including lithic artefacts of an Acheulean industry with handaxes, as well as an animal butchery, including of rhinoceroses (
Stephanorhinus hundsheimensis), deer, bear (
Ursus deiningeri) and horses, that occurred during a warm interglacial in coastal, grassland and forest environments. Boxgrove-type ovate handaxes are also found at other sites in Britain of MIS 13 age, and show a great increase in knapping skill over the much more crude handaxes found in Fordwich Pit and MIS 15 deposits. The extreme cold of the following
Anglian Stage (Marine Isotope Stage 12) was previously thought to have driven humans out of Britain altogether. The discovery of sharp, unworn stone tools sandwiched between two Anglian sediment layers at Fordwich Pit in Kent, however, suggests at least some human populations visited Britain during this ice age, perhaps during a relatively warm
interstadial period although probably not when glaciers reached their southern limit north of Old Park. , found near Clacton-on-sea, is the oldest known wooden weapon, at approximately 400,000 years old. The warmer, largely interglacial
Hoxnian Stage (Marine Isotope Stage 11) which followed the Anglian Glaciation, lasted from around 424,000 until 374,000 years ago initially saw the emergence of the
Clactonian flint tool
industry in places such as
Clacton-on-sea in Essex and
Swanscombe quarry in Kent. The Clactonian industry is distinguished from the Acheulean by its lack of use of handaxes. At Ebbsfleet near Swanscombe, the skeleton of a
straight-tusked elephant (
Palaeoloxodon antiquus), a gigantic species of elephant formerly native to Britain during interglacial periods, was found associated with Clactonian tools that were used to butcher it. The
Clacton spearhead, the oldest wooden weapon known anywhere in the world, is known from Hoxnian sediments near Clacton-on sea. Around 415,000 years ago, the Clactonian industry was replaced by an Acheulean industry using handaxes, which may represent a colonisation event that replaced the people using Clactonian tools.
Neanderthals (Middle Palaeolithic) Following a likely abandonment of Britain during MIS 10 glacial period, Neanderthals reappeared in Britain from around 330,000 years ago. The youngest evidence of an Acheulean industry with handaxes in Britain dates to around 250,000 years ago (late MIS 8), from Harnham, Wiltshire. Neanderthals practicing a
Mousterian industry utilizing advanced
Levallois stoneknapping techniques appear in Britain during late MIS 8 (by around 240,000 years ago), considerably later than continental Europe where it appears around 320,000 years ago, suggesting that the technology was brought by new migrants from the continent, marking the beginning of the
Middle Palaeolithic in Britain. Remains of early Neanderthals associated with Levallois stone tools have been discovered at
Pontnewydd Cave in Wales, dated to 225,000 years ago (MIS 7). Neanderthals were absent from Britain during the
Penultimate Glacial Period (MIS 6) from around 180,000 years ago. The
Last Interglacial, locally called the Ipswichian in Britain and the Eemian elsewhere in northern Europe, occurred around 130-115,000 years ago. During this time Britain was uninhabited by humans, but inhabited by large animals, similar to previous interglacial periods, such the living
hippopotamus (
Hippopotamus amphibius), which reached northwards to
Stockton-on-Tees, the
straight-tusked elephant (
Palaeoloxodon antiquus), the narrow nosed rhinoceros,
Irish elk, bison,
cave lions (
Panthera spelaea) and
cave hyenas (
Crocuta spelaea). It has been generally argued that Neanderthals were not present in Britain again until the MIS 4-3 transition during the
Last Glacial Period around 60,000 years ago. However finds from Great Pan Farm on the Isle of Wight have led to suggestions that Neanderthals may have been present in Britain already by 115-84,000 years ago, during the early Last Glacial Period in early
MIS 5. Britain had its own unique variety of late Neanderthal handaxe, the
bout-coupé.
La Cotte de St Brelade in
Jersey is the only site in the British Isles to have produced late Neanderthal fossils, with the site preserving evidence of butchery and possibly hunting of
woolly mammoth (
Mammuthus primigenius) and
woolly rhinoceros (
Coelodonta antiquitatis) by Neanderthals. Neanderthals are suggested to have become extinct in Britain by around 40,000 years ago.
Initial Upper Palaeolithic stone tools in Britain produced by modern humans are assigned to the
Lincombian–Ranisian–Jerzmanowician (LRJ) culture, which are probably around 45-40,000 years old. Stone tools found at a handful of sites across England and Wales indicate that Britain was occupied by
Aurignacian peoples, probably beginning no later than 37,000 years ago, which may represent a number of distinct occupations. The most famous example of a human skeleton from the British Upper Palaeolithic is the "
Red Lady of Paviland", an
ochre covered skeleton of a man (rather than a woman as previously thought) in coastal South
Wales, which was dated in 2010 to be around 34,000 years old. The glacial advances in northern Britain and highland Wales and broader climatic deterioration in Britain in the run-up to the
Last Glacial Maximum made Britain uninhabitable for humans, and they were probably absent from Britain by 28,000 years ago. Humans associated with
Magdalenian cultures recolonised Britain around 15,000 years ago, following the return of more favourable climatic conditions around the beginning of the
Bølling–Allerød Interstadial.
Gough's Cave, Somerset which was occupied by humans around 14,700 years ago, preserves evidence of
cannibalism, suggested to represent ritual
funerary endocannibalism, and the modification of skulls into
skull cups. The people occupying Gough's Cave likely had a diet heavily relying on large animals such as
red deer,
wild horse and bovines. , from
Creswell Crags, c. 10,500 BC
Creswell Crags on the Nottinghamshire-Derbyshire border, dating to around 15,700-12,800 years ago is one of the few localities with evidence of figurative
Paleolithic art in Britain, including wall engravings of bison and deer, birds and human figures, as well bone engravings, such as the
figure of a horse's head etched onto a rib fragment.
Cathole Cave in South Wales may also have a wall engraving of a reindeer, suggested to date to at least 12,500 years ago. Around 14-13,000 years ago, a new wave of hunter-gatherers arrived in Britain, associated with the
Western Hunter-Gatherer genetic cluster distinct from those of earlier British Magdalenian peoples, as exemplified by an individual from
Kendrick's Cave in North Wales, who appears to have had a diet heavy in freshwater or marine resources.
Mesolithic (c. 9,700 to 4,300 BC) from 10,000 years
Before Present (BP, top left), to 7000 BP (bottom right) The Younger Dryas was followed by the
Holocene, which began around 9,700 BC (approximately 11,700 years
Before Present), and continues to the present. By 8000 BC temperatures were higher than today, and birch woodlands spread rapidly, but there was a
cold spell around 6,200 BC which lasted about 150 years.
Doggerland would no longer have formed a continuous plain by around 7000 BC (9000 BP) and submergence was largely complete by 5000 BC (7000 BP). which would have required different hunting techniques. , c. 9000 BC|177x177px The older view of Mesolithic Britain as monotonous and unchanging, with the endless repetition of seasonal rounds is now being replaced with a more complex picture. Different periods of Mesolithic occupation in Britain are distinguished by the use of differently shaped
microlith (small lithic pieces used as spear tips and arrowheads) technology, though the chronology of a number of different British microlith industries is currently poorly resolved. reconstruction, c. 7600 BC At Star Carr, located on the former edge of a lake, and occupied c. 9300-8500 BC, wooden structures, including raised platforms, The later Mesolithic shows an increased construction of structures such as houses, pits and
hearths. Animal bones and in coastal areas, seashells were frequently dumped into
middens.
Hazelnuts were also widely exploited as a food source, with their charred remains often found at (particularly Middle) Mesolithic sites.
Neolithic (c. 4,300 to 2,000 BC) , c. 3000–2500 BC DNA analysis of human remains spanning the Mesolithic-Neolithic transition shows that the transition to the Neolithic c. 4000 BC was brought by the migration of
European Neolithic Farmers from the continent (with British Neolithic farmers being closely related to Neolithic farmers in the
Iberian Peninsula), who had ultimately originated in
Anatolia (the Asian part of modern Turkey) several thousand years earlier. The continental Neolithic farmers effectively appear to have replaced the previous Mesolithic hunter-gatherers, and there is little evidence of mixing of British Neolithic farmers and Mesolithic hunter-gatherers outside of Western Scotland, where some individuals appear to have had recent hunter-gatherer ancestry. The construction of the earliest earthwork sites in Britain began during the early Neolithic (c. 4400–3300 BC) in the form of
long barrows used for communal burial and the first
causewayed enclosures, sites which have parallels on the continent. The former may be derived from the
long house, although no long house villages have been found in Britain — only individual examples. The stone-built houses on
Orkney — such as those at
Skara Brae — are, however, indicators of some nucleated settlement in Britain. Evidence of growing mastery over the environment is embodied in the
Sweet Track, a wooden trackway built to cross the marshes of the
Somerset Levels and dated to 3807 BC. Leaf-shaped arrowheads, round-based pottery types and the beginnings of polished axe production are common indicators of the period. Evidence of the use of cow's milk comes from analysis of pottery contents found beside the Sweet Track. According to archaeological evidence from North
Yorkshire, salt was being produced by
evaporation of seawater around this time, enabling more effective preservation of meat. The Middle Neolithic (c. 3300–2900 BC) saw the development of
cursus monuments close to earlier barrows and the growth and abandonment of causewayed enclosures, as well as the building of impressive
chamber tombs such as the
Maeshowe types. The earliest
stone circles and individual burials also appear. site of
Silbury Hill in Wiltshire, southern England, c. 2400 BC. The Neolithic saw the construction of a wide variety of monuments in the landscape, many of which were
megalithic in nature. Different pottery types, such as
grooved ware, appear during the later Neolithic (c. 2900–2200 BC). In addition, new enclosures called
henges were built, along with
stone rows and the famous sites of
Stonehenge,
Avebury and
Silbury Hill, which building reached its peak at this time. Industrial flint mining begins, such as that at
Cissbury and
Grimes Graves, along with evidence of long-distance trade. Wooden tools and bowls were common, and bows were also constructed. ==Bronze Age==