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History of Gabon

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Through Neolithic, Atlantic Ocean and Ivory

From 1472 Atlantic contact reshaped coastal exchange. Myene-speaking polities on the Gabon littoral, including the Mpongwe in the Estuary and the Orungu and Nkomi farther south, acted as brokers linking river routes to European shipping. Trade focused on ivory, copper, salt, raffia cloth, and, by the late 1700s, captives; in 1788 about 500 people were embarked annually at " Gabon and Cape Lopez ", far fewer than the major outlets farther south. Domestic slavery predated overseas commerce and expanded with it, concentrating wealth and authority in lineages and chiefly houses. Coastal lifeways combined salt making, oyster harvesting at Mayumba, and diversified agriculture, while political organization ranged from clan-based councils among the Mpongwe to royal offices among the Orungu and Nkomi.

In 1862–1887 France expanded its control including the interior of the state, and took full sovereignty. In 1910 Gabon became part of French Equatorial Africa and in 1960, Gabon became independent.

At the time of Gabon's independence, two principal political parties existed: the Gabonese Democratic Bloc (BDG), led by Léon M'Ba, and the Gabonese Democratic and Social Union (UDSG), led by Jean-Hilaire Aubame. In the first post-independence election, held under a parliamentary system, neither party was able to win a majority; the leaders subsequently agreed against a two-party system and ran with a single list of candidates. In the February 1961 election, held under the new presidential system, M'Ba became president and Aubame became foreign minister. The single-party solution disintegrated in 1963, and there was a single-day bloodless coup in 1964. In March 1967, Leon M'Ba and Omar Bongo were elected president and vice president. M'Ba died later that year. Bongo declared Gabon a one-party state, dissolved the BDG and established the Gabonese Democratic Party (PDG). Sweeping political reforms in 1990 led to a new constitution, and the PDG garnered a large majority in the country's first multi-party elections in 30 years. Despite discontent from opposition parties, Bongo remained president until his death in 2009.

Early history

Archaeology

Late Stone Age, Neolithic, and Early/Late Iron Age sequences are documented in the Lope–Okanda–Ogooue region and on the coast.

  • Coastal Neolithic at Owendo (Libreville): lithics, pottery, shells, hearths dated to 5040 ± 130 BP.
  • Lopé II (middle Ogooue): charcoal from Late Stone Age layers dates to 10320 ± 110 BP, 9170 ± 100 BP, and 6760 ± 120 BP; a much later pit with ceramics dates to 2370 ± 35 BP and 2210 ± 45 BP, indicating reoccupation by pottery-using groups long after the earlier occupations.
  • Ceramic traditions and early ironworking:
    • Yindo pottery attested at Okanda I, Lope II, Toube I, Maboue I, Okanda V; highest date at Okanda I 3560 ± 75 BP.
    • After about AD 650, the earlier pit features disappear. Later radiocarbon dates indicate renewed occupations at several sites: Lope XV (AD 1046–1293), Lope V (AD 1215–1414), Otoumbi III (AD 1398–1442), and Lope X (AD 1623–1808).
  • Ritual evidence (late precolonial): the Iroungou burial cave near Mouila yielded at least 28 individuals and 512 grave goods (iron currency hoes, bracelets, gongs, long spatulate rods), with radiocarbon placing use in the 14th–15th centuries AD.

Precontact period

Rainforest hunter-gatherers (often called Pygmy groups, including the Babongo, Baka, and Bakoya) are the earliest known inhabitants of the area, their presence has been attested since the Upper Pleistocene (roughly 43,000–13,000 BC). Archaeology in the Ogooue valley shows Late Stone Age sites long before farming, and genetics points to deep splits between foragers and farmers. Bantu-speaking communities appear by the Early Iron Age, at least the 3rd–2nd centuries BC, and expand through the first millennium AD.

The Bantu expansion is found in the middle Ogooue valley, where Late Stone Age occupations were replaced by Early Iron Age communities around 2400–2300 BP (c. 400–300 BC), notably at Lalara and Otoumbi. Paleoenvironmental studies identify a late Holocene episode of rainforest fragmentation around 2500–2000 BP (c. 550–50 BC) across Central Africa, including Gabon, which created savanna–forest mosaics conducive to such settlements. This timing and geography are consistent with broader models of Bantu expansion that emphasize movement along habitat corridors and slower spread through dense rainforest.

Early Iron Age metallurgy in Gabon is documented by smelting furnaces and slag at sites such as Oveng (Estuaire Province), confirming local iron production and its role in the west-Central African spread of Bantu speakers. Prior to coastal contact, lineage-based communities and flexible chiefly authority embedded in riverine exchange networks structured social and political life in equatorial Africa, a framework widely applied to precolonial Gabon, especially along the Ogooue corridor.

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