Domestic animals
30285 BCE to 2115 CE
Domesticated animals are those populations whose behavior, life cycle, or physiology have been systemically altered as a result of being under human control for many generations.
The term domestic animal applies to those animals that actually live in physical proximity to humans, such as pets and guard animals, or even food species kept very close, e.g.
to live on domestic food scraps and/or so their body heat can be used as 'stable heating'.
Dogs and sheep are among the first animals to be domesticated, followed by goats, then pigs, then cows and zebus, then cats.
Next up are chickens, then guinea pigs and donkeys, then water buffalo, horses, dromedaries, and bees.
And so on.
Domestic animals, in the widest sense, include animals as diverse as songbirds, common carp, pythons and leeches.
The domesticated animals of greatest significant to human history had all been domesticated by 2400 BCE.
These include: • dogs (between 30,000 BCE and 15,000 BCE in Eurasia), • sheep (between 11,000 BCE and 9000 BCE in Southwest Asia), • pigs (9000 BCE, Near East and China), • goats (8000 BCE, Iranian plateau), • cattle (8000 BCE, Europe, Asia and North Africa), • zebus (8000 BCE, India), • cats (7500 BCE, Near East), • chickens (6000 BCE, India and Southeast Asia), • guinea pigs (5000 BCE, Peru), • donkeys (5000 BCE, Egypt), • ducks (4000 BCE, China), • water buffalos (4000 BCE, India and China), • honey bees (4000 BCE, Europe, Asia and Africa), • horses (4000 BCE, Eurasian Steppes), • dromedary camels (4000 BCE, Arabia), • silkmoths (3000 BCE, China), • reindeer (3000 BCE, Russia) • pigeons (3000 BCE, Mediterranean Basin), • geese (3000 BCE, Egypt) • yaks (2500 BCE, Tibet) • Bactrian camels (2500 BCE, Central Asia) • llamas (2400 BCE, Peru) • alpacas (2400 BCE, Peru), and • guineafowl (2400 BCE, Africa).
Related Events
Showing 10 events out of 3518 total
Britain is grassland from 60,000 to 40,000 BCE, with giant deer and horse, woolly mammoths, rhino and carnivores.
West Africa (49,293 – 28,578 BCE) Upper Pleistocene I — Foragers of River Valleys and Green Sahara Corridors
Geographic and Environmental Context
The Atlantic and inland belt from Senegal and Mauritania east through Mali, Niger, Burkina Faso, and Nigeria (western and central), plus the forest–savanna margins of Guinea, Sierra Leone, Liberia, Côte d’Ivoire, Ghana, Togo, and Benin.
Anchors: Senegal–Gambia valleys, Inland Niger Bend and Inland Delta (Timbuktu, Mopti, Gao), Middle Niger–Kainji basin, Jos Plateau, Hausaland (Kano, Katsina, Zaria), Upper Volta basin, Gold Coast forest margins, Futa Jallon highlands, Dahomey Gap.
-
LGM: Sahara hyper-arid; Lake Chad contracted.
-
Sahel savanna narrowed to thin strip.
-
Niger–Senegal–Volta valleys shrank but retained perennial water.
Climate & Environmental Shifts
-
Cooler, drier; dust storms frequent.
-
Seasonal streams ephemeral; only major rivers provided continuity.
Subsistence & Settlement
-
Foragers along Senegal–Gambia and Niger hunted antelope, aurochs, and hippo.
-
Fishing supplemented lean seasons.
-
Futa Jallon uplands provided refugia with springs.
Technology & Material Culture
-
Core–flake tools, quartz microliths.
-
Shell and bone ornaments.
Movement & Interaction Corridors
-
Senegal–Niger corridor carried movement between coastal and inland refugia.
-
Green Sahara corridors limited but provided episodic exchange.
Cultural & Symbolic Expressions
-
Ochre use and body ornamentation.
-
Rock shelters in Mali/Senegal show symbolic traces.
Environmental Adaptation & Resilience
-
Mobility between rivers and upland refugia buffered aridity.
Transition
By 28,578 BCE, West African foragers had stabilized around perennial river corridors.
The archaeological site of La Ferrassie, located in the Dordogne region of France, provides some of the most compelling evidence of Neanderthal burial customs and ritual behavior. Dating to approximately 50,000 years ago, the site contains eight Neanderthal skeletons, including adults, children, and infants, all of whom appear to have been intentionally buried.
The Young Male Burial and Funeral Offerings
One of the most striking burials at La Ferrassie is that of a 15- to 16-year-old boy, who was laid to rest with a beautifully fashioned stone axe near his hand. His grave also contained charred wild cattle bones, which may be the remains of a funeral feast, suggesting that Neanderthals engaged in ritualized mourning practices.
Nearby, additional burials included the graves of three children and two adults, potentially forming a family burial plot—a rare find in Neanderthal archaeology.
The La Ferrassie 1 Skeleton: A Key Neanderthal Discovery
One of the most important individuals found at the site is La Ferrassie 1, an adult male Neanderthal whose skull, discovered in 1909, remains the largest and most complete Neanderthal skull ever found.
- His large brow ridge, sloping forehead, and protruding midface exhibit the classic Neanderthal traits.
- His teeth were heavily worn, particularly the front incisors, which display a slanted wear pattern not caused by chewing.
- One hypothesis suggests that he habitually held an object, such as an animal hide, between his teeth while scraping it with a tool—a possible behavioral adaptation indicating that Neanderthals used their teeth as tools.
Symbolism and Ritual at La Ferrassie
The complex burial practices at La Ferrassie hint at a Neanderthal belief system:
- One child’s skull was found separately from its lower skeleton and had been covered with a limestone slab with markings on its underside.
- This suggests some form of symbolic behavior or ritual practice, reinforcing the idea that Neanderthals had a relatively advanced cultural framework.
Legacy of the La Ferrassie Neanderthals
The intentional burials at La Ferrassie provide significant evidence that Neanderthals treated their dead with care, possibly engaging in mourning, funerary rituals, and symbolic behavior. These findings challenge older stereotypes of Neanderthals as primitive and instead suggest that they possessed a level of cultural and cognitive complexity previously attributed only to Homo sapiens.
Today, the remains from La Ferrassie are housed at the Museum of Man in Paris, where they continue to provide valuable insights into Neanderthal life, death, and ritual practices.
Archaeologists also find evidence of Stone Age technology in Aq Kopruk and Hazar Sum in north central Afghanistan.
Plant remains in the foothills of the Hindu Kush mountains indicate that northern Afghanistan is one of the earliest places to domestic plants and animals.
The Near and Middle East (28,577 – 7,822 BCE): Late Pleistocene–Early Holocene — Warming Shores, Spring Worlds, and Broad-Spectrum Economies
Geographic & Environmental Context
Across the millennia of deglaciation, the Near and Middle East cohered as a chain of water-anchored landscapes:
-
Southeast Arabia—the Dhofar escarpments with khareef fog-forests, the Ḥaḍramawt–Mahra wadi fans, the al-Wusta/Sharqiyah gravel and dune seas, and Socotra’s Hagghier uplands—turned inward to springs and outward to a retreating Aden–Arabian Sea shoreline.
-
The Middle East—Zagros–Upper Mesopotamia, the Tigris–Euphrates corridors, the Caucasus piedmont, Khuzestan/Fars lowlands, and the advancing Gulf shelf—oscillated between pluvial recovery and steppe stress before stabilizing in the Early Holocene.
-
The Near East—the Nile Valley and Delta, Sinai–Negev–Arabah, the southern Levant, western Anatolia’s Aegean littoral, and the Hejaz–Asir–Tihāma—saw drowned shelves, maturing estuaries, and rejuvenated floodplains.
Rising seas re-shaped coasts (Gulf transgression; Aegean embayments), while thawing headwaters revived perennial flow in the great river systems.
Climate & Environmental Shifts
-
Bølling–Allerød (c. 14.7–12.9 ka): Warmer, wetter conditions expanded Zagros gallery woods and Caucasus belts; Ḥaḍramawt/Dhofar wadis ran strong; Nile floods strengthened; Aegean and Gulf coasts grew more productive.
-
Younger Dryas (12.9–11.7 ka): Cooler, drier snapback: steppe spread across Upper Mesopotamia, wadis intermittently failed in SE Arabia, Nile discharge weakened; foragers pivoted to resilient wetland/coastal patches.
-
Early Holocene (post-11.7 ka): Sustained warmth and more reliable monsoons/westerlies: Zagros springs and Tigris–Euphrates marsh–riparian mosaics stabilized; Dhofar fog-forests rebounded; Nile and Aegean floodplains/estuaries matured as the Gulf flooded landward.
Subsistence & Settlement
A triad of broad-spectrum adaptations converged on semi-sedentary water nodes:
-
Southeast Arabia: Seasonal hamlets clustered at springheads and lagoon margins; diets paired gazelle–oryx–ibex with fish, shellfish, turtles, and mangrove resources. Inland rounds gathered fruits/nuts and hunted in the Mahra/Wusta belts; Socotra remained a wooded outpost likely without permanent settlement.
-
Middle East (Zagros–Upper Mesopotamia–Caucasus–Gulf rim): Spring-terrace camps and riparian hamlets exploited gazelle, onager, boar, riverine fish/mollusks, and seeds, acorns, pistachio/almond. In the Early Holocene, some groups tethered wild caprines, edging toward management on Zagros slopes; marsh fishing/waterfowling intensified in the lower Tigris–Euphrates as the Gulf advanced.
-
Near East (Nile–Levant–Aegean–Hejaz/Tihāma): Nile communities deepened fish–fowl–reed economies; Levantine and Aegean foragers harvested shellfish and nearshore fish alongside deer/boar; Red Sea shorelines with relict mangroves supported intermittent foraging.
Settlement was nodal and recurrent—springs, levees, dune spurs, and lagoon bars accruing hearths, pits, and cemeteries across centuries.
Technology & Material Culture
-
Microlithic bladelet/geometrics dominated hunting kits; hafted composite points and resins common.
-
Grinding stones, mortars/querns for nuts/seeds spread widely; bone harpoons/fish gorges, net weights, basketry, and ropework underpinned marsh/estuary fisheries.
-
Ground-stone tools rose late; incipient pottery appeared by the end of the period on the northern Iranian/Caspian and Anatolian fringes, initially for boiling and storage.
-
Early dugouts/rafts and reed craft likely on Nile backwaters and sheltered lagoons; cabotage along Aegean/Gulf/Arabian rims feasible during stable seasons.
Movement & Interaction Corridors
-
Zagros passes (Kermanshah–Khuzestan) funneled goods/people between uplands and Khuzestan plains; Karkheh–Karun–Shatt al-Arab backwaters linked to the Upper Gulf.
-
Caucasus Kura–Araxes fans connected highlands to Iranian forelands.
-
Ḥaḍramawt–Mahra–Dhofar wadis stitched coast and interior; short maritime hops likely reached the Horn of Africa.
-
The Nile remained the subregion’s master axis; Aegean island-hops and Red Sea shore lanes tied capes and wadi mouths.
These intertwined routes provided redundancy: when wadis failed or steppe widened, marsh, lagoon, and coast supplied calories and salt.
Cultural & Symbolic Expressions
-
Ochre burials and river/spring offerings recur from Zagros to the Nile; house-based ritual—hearth deposits, ancestor interments, stone slab markers—emerged in semi-sedentary camps.
-
Petroglyphs on Dhofar/Haima desert margins and Zagros outcrops (caprids, equids, processions) may root in these horizons.
-
Shell terraces and levee mounds served as feasting grounds and mnemonic landmarks, formalizing access to water and fisheries.
Environmental Adaptation & Resilience
A shared risk-spreading grammar took shape:
-
Dietary breadth + storage (dried meat/fish, nut pastes) buffered Younger Dryas shocks.
-
Flexible rounds (wetland–upland–coast) tracked shifting isohyets and resource pulses.
-
Proximity to springs/marshes anchored overwintering; early caprine tethering and focused seed processing foreshadowed managed food webs.
-
Lagoon/marsh anchoring during arid pulses sustained semi-sedentism without agriculture.
Long-Term Significance
By 7,822 BCE, the Near and Middle East had become a water-anchored, semi-sedentary world: mapped wadi networks in SE Arabia; spring-terrace and marsh hamlets in Zagros–Mesopotamia edging toward herd and seed management; and Nile–Aegean–Red Sea littorals refining wetland and coastal economies.
These intertwined traditions—grinding and storage, spring/levee fidelity, caprine protomanagement, marsh and lagoon fisheries, and seasonal cabotage—constituted the operating code from which the region’s first Neolithic cultivation and herding communities would soon crystallize.
The Middle East (28,577 – 7,822 BCE) Upper Pleistocene II — Bølling–Allerød Abundance, Younger Dryas Stress, Early Holocene Recovery
Geographic and Environmental Context
The Middle East includes Iraq, Iran, Syria, Armenia, Georgia, Azerbaijan, eastern Jordan, most of Turkey’s central/eastern uplands (including Cilicia), eastern Saudi Arabia, northern Oman, Qatar, Bahrain, the UAE, northeastern Cyprus, and all but the southernmost Lebanon.-
Anchors: the Tigris–Euphrates alluvium and marshes; the Zagros (Luristan, Fars), Alborz, Caucasus (Armenia–Georgia–Azerbaijan); northern Syrian plains and Cilicia; Khuzestan and Fars lowlands; the Arabian/Persian Gulf littoral (al-Ahsa–Qatar–Bahrain–UAE–northern Oman); northeastern Cyprus and the Lebanon coastal elbow (north).
Climate & Environment
-
Bølling–Allerød (c. 14.7–12.9 ka): rainfall rose; gallery woodlands expanded along Tigris–Euphrates and Zagros springs.
-
Younger Dryas (12.9–11.7 ka): cooler–drier snapback; steppe patches widened.
-
Early Holocene: stabilizing warmth; perennial springs recharged; Gulf shoreline advanced landward.
Subsistence & Settlement
-
Broad-spectrum foraging intensified (gazelle–onager–boar–fish–mollusks; seeds, acorns, pistachio/almond); semi-recurrent springhead hamlets in Zagros and Upper Mesopotamia (preludes to later Epipaleolithic “Natufian-like” economies outside our zone).
-
Seasonal coastal foraging at northeastern Cyprus and the Gulf rim.
Technology & Material Culture
-
Microlithic toolkits diversified; grinding stones and mortars for seeds/nuts; bone harpoons/fish gorges in marshy reaches.
-
Hafting resins, compound points; early basketry inferred.
Corridors
-
Zagros spring belts (Luristan–Kurdistan) and Upper Mesopotamian flanks; Caucasus piedmont fans; Gulf shelf retreat reshaped coastal access.
Symbolism & Ritual
-
Persistent ochre burials; ritual deposits at springs; engraved motifs (caprids, equids).
Adaptation & Resilience
-
Diet breadth + storage (dried meat/fish, nut pastes) buffered Younger Dryas shocks; flexible camp scheduling maintained returns.
Transition
Early Holocene stability primed semi-sedentary river–spring villages and the seed economies that will underpin later plant management.
(7,821 – 6,094 BCE) Early Holocene — Semi-Sedentary Spring Villages & Seed Processing
Climate & Environment
-
Thermal optimum onset: marsh–riparian mosaics in Lower Mesopotamia; wooded Zagros; productive Caucasus belts; Gulf continued transgression.
Subsistence & Settlement
-
Semi-sedentary hamlets on springheads/low terraces (Zagros–Upper Mesopotamia) combined hunting with seed–nut processing; wetland fishing/waterfowling in Tigris–Euphrates backwaters.
-
Early caprine management likely began on Zagros slopes (wild → managed herds).
Technology & Material Culture
-
Ground-stone mortars/querns proliferated; larger storage pits; microliths persisted; incipient pottery appears on the northern Iranian/Caspian periphery by late in the epoch.
Corridors
-
Zagros passes (Kermanshah–Khuzestan) linked uplands to Khuzestan plains; Karkheh–Karun marshes tied to the Upper Gulf.
Symbolism
-
House-based ritual (hearths, ancestor interments); stone slab markers; continued ochre.
Adaptation
-
Storage + proximity to springs anchored overwintering; mixed wetland–upland rounds hedged variability.
Transition
These lifeways foreshadow Neolithic cultivation/herding communities across the Zagros and Upper Mesopotamia.
Southeast Arabia (28,577 – 7,822 BCE) Upper Pleistocene II — Deglaciation, Coastal Productivity, and Wadi Networks
Geographic and Environmental Context
Southeast Arabia covers the southern and eastern margins of the Arabian Peninsula:-
Eastern Yemen (Hadhramaut, eastern Aden interior, al-Mahra).
-
Southern Oman (Dhofar Highlands with the khareef monsoon, al-Wusta gravel plains, Sharqiyah Desert fringes).
-
The Empty Quarter (Rubʿ al-Khālī) margins in adjoining Saudi territory.
-
The offshore island of Socotra in the Arabian Sea.
-
Anchors: Wādī Ḥaḍramawt–Shibam–Tarim, Dhofar escarpments (Ẓafār/Al-Balīd, Mirbat), al-Mahra dunes, al-Wusta plains, Sharqiyah sands, Socotra’s Hagghier Mountains and dragon’s-blood groves.
-
As glaciers melted, sea level rose; Gulf of Aden–Arabian Sea coasts retreated inland.
-
Hadhramaut wadis deepened; Dhofar fog-forests fluctuated with monsoon strength.
Climate & Environmental Shifts
-
Bølling–Allerød warming (14,700–12,900 BCE): lush monsoons, wadis flowed, upland belts expanded.
-
Younger Dryas (12,900–11,700 BCE): renewed aridity, wadis dried, dune advance.
-
Early Holocene (after 11,700 BCE): warm stable monsoon, reliable khareef in Dhofar.
Subsistence & Settlement
-
Broad-spectrum foragers: hunting gazelle, oryx, ibex; intensified fishing and shellfish harvests during wet phases.
-
Seasonal hamlets along wadis and coastal terraces, abandoned in dry pulses.
-
Socotra: rich woodlands sustained seabirds and goats, but permanent human settlement is still unlikely.
Technology & Material Culture
-
Bladelet industries matured; ground-stone tools appeared late.
-
Fish gorges, shell scrapers, net weights.
-
Basketry and rope-making inferred from toolkits.
Movement & Interaction Corridors
-
Hadhramaut–Mahra wadis critical wet-phase corridors.
-
Coastal cabotage feasible during stable periods; possible short-haul to Red Sea Horn.
Cultural & Symbolic Expressions
-
Ritual feasting likely at perennial springs.
-
Petroglyphs in Dhofar/Haima desert margins may trace back to these horizons.
Environmental Adaptation & Resilience
-
Flexible settlement and diet shifts buffered against Younger Dryas drought.
Transition
By 7,822 BCE, foragers had mapped wadi networks and sustained a dual economy of coast + upland.
Southern Africa (28,577 – 7,822 BCE): Late Pleistocene–Early Holocene — Rising Seas, Flood Pulses, and Shell-Midden Shores
Geographic & Environmental Context
During the long swing from the Last Glacial Maximum to the Early Holocene, Southern Africa cohered as a single water-anchored world.
Two complementary spheres organized lifeways:
-
Temperate Southern Africa — the Cape littoral and fynbos, Namaqualand, Highveld grasslands, Drakensberg–Lesotho massif, Karoo, and the Maputo–Limpopo basins—where rising seas carved modern embayments and lagoons and river valleys remained fertile through climatic swings.
-
Tropical West Southern Africa — the Okavango Delta, Zambezi–Chobe–Cuando/Linyanti–Caprivi wetlands, the Etosha Pan system and Owambo/Cuvelai drains, and the fog-nourished Skeleton Coast—an aquatic–savanna frontier driven by flood pulses and ITCZ rains.
Together these belts formed a ridge–river–coast continuum: shell-rich coves and estuaries at the Cape, grassland and spring corridors inland, and pulsing floodplains and pans to the north.
Climate & Environmental Shifts
-
Bølling–Allerød (c. 14,700–12,900 BCE): Warmer, wetter conditions greened fynbos and Highveld grasslands; Okavango inundations broadened and Caprivi wetlands expanded; woodland belts thickened around Etosha and along the Owambo/Cuvelai drains.
-
Younger Dryas (c. 12,900–11,700 BCE): A brief cool–dry pulse contracted marsh edges and inland water bodies; coastal reliance intensified along the Cape and Namaqualand; floodplain use narrowed to perennial channels and levees.
-
Early Holocene (after 11,700 BCE): Climatic stabilization brought stronger summer rains in the north and reliable winter–spring moisture in the south; flood regimes regularized, lagoons matured, and grasslands recovered.
Subsistence & Settlement
A continent-spanning broad-spectrum portfolio matured, balancing semi-sedentary anchoring with seasonal mobility:
-
Coasts (Temperate south): Strandloper adaptations flourished—large shell middens formed along the Cape and Namaqualand, with fish, mussels, limpets, seals, and seabirds as staples. Semi-sedentary cove camps persisted near rich shorelines and estuaries; inland rounds targeted antelope and dug geophytes in fynbos and grasslands.
-
Floodplains & pans (Tropical west): Semi-recurrent levee camps followed fish runs (catfish/tilapia), flood-recession grazing of antelope, and riparian fruits. The Caprivi supported large wet-season encampments on high levees; Etosha margin hunts focused on springbok, zebra, oryx near permanent water; the Skeleton Coast remained a short-visit zone for carrion and shellfish.
Across both spheres, settlement knit together resource-rich nodes—coves, levees, springs, and rock shelters—reoccupied across generations.
Technology & Material Culture
Toolkits were light, durable, and tuned to water:
-
Microlithic bladelets and backed segments for composite arrows and spears.
-
Fish gorges, bone harpoons, woven basket traps, and stake weirs for estuary and floodplain capture.
-
Grinding slabs for wild plant processing; basketry and cordage for transport and drying racks.
-
Ostrich eggshell (OES) flasks for water carriage and abundant OES beads as exchange media.
-
Early rafts/dugouts likely in calm estuaries and distributaries.
Movement & Interaction Corridors
Mobility braided coasts, valleys, pans, and deltas into one exchange field:
-
Coastal corridors linked shell-midden coves with river mouths and inland passes to the Highveld and Drakensberg.
-
Flood-ridge “causeways” among Okavango palm islands, Caprivi levee paths, and Omuramba routes to Etosha organized pulse-following rounds.
-
The Maputo–Limpopo system and interior river valleys moved beads, pigments, dried fish, and hides between grassland and shore.
These routes created redundancy: when drought pinched a basin or a run failed, another habitat or partner camp stabilized supply.
Cultural & Symbolic Expressions
Symbolic life was vivid and place-anchored:
-
Rock art in Drakensberg and Cederberg shelters flourished—polychrome animal–human scenes, trance dances, and eland-linked ceremonies.
-
Shell middens functioned as ancestral markers at coastal landings; bead strings and pigment caches accumulated at island groves and pan-edge shelters in the north.
-
Seasonal feasts at fish peaks and flood-begin events renewed access rules to weirs, springs, and groves—ritual governance of resources.
Environmental Adaptation & Resilience
Security rested on storage + scheduling + multi-ecozone use:
-
Smoked/dried fish and meats, rendered fats, roasted seeds, and stored geophytes buffered lean months and Younger Dryas stress.
-
Seasonal anchoring at rich coasts and pulse-following mobility across wetlands and pans spread risk.
-
Edge-habitat focus (back-bar lagoons, riparian woods, pan margins) maximized predictable returns as conditions shifted.
Long-Term Significance
By 7,822 BCE, Southern Africa had stabilized as a water-anchored forager world: shell-midden communities lined the temperate coasts, and floodplain societies tuned lifeways to the Okavango–Caprivi–Etosha pulse. The shared operating code—portfolio subsistence, storage, seasonal anchoring with mobile spokes, bead-mediated exchange, and shrine-marked tenure—set the durable foundation for later Holocene traditions of coastal strandlopers, floodplain specialists, and, eventually, pastoral and farming horizons on the distant skyline.
Temperate Southern Africa (28,577 – 7,822 BCE) Upper Pleistocene II — Deglaciation, Coastal Abundance, and Semi-Sedentary Middens
Geographic and Environmental Context
Temperate Southern Africa includes:-
South Africa (Cape littoral, Highveld, Drakensberg, Karoo, Namaqualand).
-
Lesotho and Eswatini.
-
Most of Namibia and Botswana, except the far northern sectors (Caprivi, Etosha, Okavango, Skeleton Coast — those are in Tropical Southern Africa).
-
Southern Zimbabwe and southwestern Mozambique (Maputo–Limpopo region).
Anchors: Cape littoral & fynbos, Drakensberg–Lesotho massif, Highveld grasslands (Witwatersrand, Free State), Namaqualand semi-desert, Kalahari southern margins, Great Karoo, Maputo–Limpopo basins, southern Zimbabwe plateau (Great Zimbabwe heartland).
-
Rising seas drowned coastal plains, forming modern embayments.
-
Grasslands contracted somewhat, but river valleys remained fertile.
Climate & Environmental Shifts
-
Bølling–Allerød: wetter, warmer; grasslands greened.
-
Younger Dryas: brief cold–dry pulse; coastal reliance intensified.
-
Early Holocene: stabilization, rainfall increased.
Subsistence & Settlement
-
Strandloper adaptations: large shell middens along Cape and Namaqualand coasts; fish, mussels, seals, seabirds.
-
Inland foragers hunted antelope, collected geophytes in fynbos and grasslands.
-
Semi-sedentary seasonal camps emerged at resource-rich coves.
Technology & Material Culture
-
Microlithic bladelets; fish gorges, bone harpoons.
-
Grindstones used for wild plant processing.
Movement & Interaction Corridors
-
Coastal canoe/raft possible for estuaries.
-
Inland passes tied grassland foragers with coastal strandlopers.
Cultural & Symbolic Expressions
-
Rock art flourished in Drakensberg and Cederberg shelters.
-
Middens used as ancestral markers.
Environmental Adaptation & Resilience
-
Seasonal anchoring at rich coasts, plus inland mobility, buffered Younger Dryas stress.
Transition
By 7,822 BCE, shell-midden communities lined coasts, precursors to later strandlopers.
West Africa (28,577 – 7,822 BCE) Upper Pleistocene II — Deglaciation, Mega-Lakes, and Savanna Expansion
Geographic and Environmental Context
The Atlantic and inland belt from Senegal and Mauritania east through Mali, Niger, Burkina Faso, and Nigeria (western and central), plus the forest–savanna margins of Guinea, Sierra Leone, Liberia, Côte d’Ivoire, Ghana, Togo, and Benin.
Anchors: Senegal–Gambia valleys, Inland Niger Bend and Inland Delta (Timbuktu, Mopti, Gao), Middle Niger–Kainji basin, Jos Plateau, Hausaland (Kano, Katsina, Zaria), Upper Volta basin, Gold Coast forest margins, Futa Jallon highlands, Dahomey Gap.
-
Deglaciation brought wetter pulses; Lake Chad expanded.
-
Niger Inland Delta broadened; Senegal estuaries lengthened.
Climate & Environmental Shifts
-
Bølling–Allerød (14.7–12.9 ka): wet pulse, savannas expanded.
-
Younger Dryas (12.9–11.7 ka): drought shrank rivers.
-
Early Holocene: African Humid Period onset.
Subsistence & Settlement
-
Foragers exploited mega-lake fisheries; hippo, crocodile, mollusks abundant.
-
Hunting on open savannas intensified.
-
Semi-sedentary lake camps formed.
Technology & Material Culture
-
Barbed bone harpoons (Niger, Chad); microliths.
-
Baked clay figurines (earliest Jōmon–Nok parallels).
Movement & Interaction Corridors
-
Lake Chad overflow connected Niger–Nile.
-
Niger Valley provided cultural trunk.
Cultural & Symbolic Expressions
-
Ritual deposits in middens; figurines mark symbolic systems.
Environmental Adaptation & Resilience
-
Broad-spectrum foraging buffered climatic swings.
Transition
By 7,822 BCE, semi-sedentary foragers flourished in wetland savannas.