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Caral–Supe civilization

Pre-Columbian era society in coastal Peru

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Archaeological Site locations within Peru, including El Paraiso, Caral, and Aspero
Ontrvet · CC BY-SA 3.0

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Through Mesopotamia, Archaeology and Visual arts

This civilization flourished along three rivers, the Fortaleza, the Pativilca, and the Supe. These river valleys each have large clusters of sites. Farther south, there are several associated sites along the Huaura River. The name Caral–Supe is derived from the city of Caral in the Supe Valley, a large and well-studied site.

Complex society in the Caral–Supe arose a millennium after Sumer in Mesopotamia, was contemporaneous with the Egyptian pyramids, and predated the Mesoamerican Olmecs by nearly two millennia.

In archaeological nomenclature, Caral–Supe is a pre-ceramic culture of the pre-Columbian Late Archaic; it completely lacked ceramics and no evidence of visual art has survived. The most impressive achievement of the civilization was its monumental architecture, including large earthwork platform mounds and sunken circular plazas. Archaeological evidence suggests use of textile technology and, possibly, the worship of common deity symbols, both of which recur in pre-Columbian Andean civilizations. Sophisticated government is presumed to have been required to manage the ancient Caral. Questions remain over its organization, particularly the influence of food resources on politics.

Archaeologists have been aware of ancient sites in the area since at least the 1940s; early work occurred at Aspero on the coast, a site identified as early as 1905, and later at Caral, farther inland. In the late 1990s, Peruvian archaeologists, led by Ruth Shady, provided the first extensive documentation of the civilization with work at Caral. A 2001 paper in Science, providing a survey of the Caral research, and a 2004 article in Nature, describing fieldwork and radiocarbon dating across a wider area, revealed Caral–Supe's full significance and led to widespread interest.

History and geography

The dating of the Caral–Supe sites has pushed back the estimated beginning date of complex societies in the Peruvian region by more than one thousand years. The Chavín culture, c. 900 BCE, had previously been considered the first civilization of the area. Regularly, it still is cited incorrectly as such in general works.

The discovery of Caral–Supe has also shifted the focus of research away from the highland areas of the Andes and lowlands adjacent to the mountains (where the Chavín, and later Inca, had their major centers) to the Peruvian littoral, or coastal regions. Caral is located in a north-central area of the coast, approximately 150 to 200 km (93 to 124 mi) north of Lima, roughly bounded by the Lurín Valley on the south and the Casma Valley on the north. It comprises four coastal valleys: the Huaura, Supe, Pativilca, and Fortaleza. Known sites are concentrated in the latter three, which share a common coastal plain. The three principal valleys cover only 1,800 km2 (690 mi2), and research has emphasized the density of the population centers.

The Peruvian littoral appears an "improbable, even aberrant" candidate for the "pristine" development of civilization, compared to other world centers. It is extremely arid, bounded by two rain shadows (caused by the Andes to the east, and the Pacific trade winds to the west). The region is punctuated by more than 50 rivers that carry Andean snowmelt. The development of widespread irrigation from these water sources is seen as decisive in the emergence of Caral–Supe; since all of the monumental architecture at various sites has been found close to irrigation channels.

The radiocarbon work of Jonathan Haas et al., found that 10 of 95 samples taken in the Pativilca and Fortaleza areas dated from before 3500 BCE. The oldest, dating from 9210 BCE, provides "limited indication" of human settlement during the Pre-Columbian Early Archaic era. Two dates of 3700 BCE are associated with communal architecture, but are likely to be anomalous. It is from 3200 BC onward that large-scale human settlement and communal construction are clearly apparent. Mann, in a survey of the literature in 2005, suggests "sometime before 3200 BCE, and possibly before 3500 BCE" as the beginning date of the Caral–Supe formative period. He notes that the earliest date securely associated with a city is 3500 BCE, at Huaricanga, in the Fortaleza area of the north, based on Haas's dates.

Haas's early third millennium dates suggest that the development of coastal and inland sites occurred in parallel. But, from 2500 to 2000 BCE, during the period of greatest expansion, the population and development decisively shifted toward the inland sites. All development apparently occurred at large interior sites such as Caral, although they remained dependent on fish and shellfish from the coast. The peak in dates is in keeping with Shady's dates at Caral, which show habitation from 2627 BCE to 2020 BCE. That coastal and inland sites developed in tandem remains disputed, however (see next section).

In 2025, new archaeological work led by Ruth Shady linked the abandonment of Caral to a prolonged drought around 2200 BCE, part of the global 4.2-kiloyear climate event. Excavations at associated sites such as Vichama on the Pacific coast and Peñico inland indicate that populations from the Supe Valley relocated rather than collapsed, rebuilding settlements that preserved Caral–Supe architectural layouts and ceremonial spaces. Temple friezes at Vichama depict scenes of famine, death and later renewal (including stylized images of starving figures, pregnant women, large fish and a lightning-struck toad), which researchers interpret as a visual record of the drought and the hoped-for return of rainfall. Archaeologists note a continued lack of fortifications or weaponry at these sites, suggesting that the society adapted to the climatic crisis without widespread warfare.

Influence

By around 2200 BCE, the influence of Norte Chico civilization spread far along the coast. To the south, it went as far as the Chillon valley, and the site of El Paraiso. To the north, it spread as far as the Santa River valley.

The Caral–Supe civilization began to decline c. 1800 BCE, with more powerful centers appearing to the south and north along the coast, and to the east inside the belt of the Andes. The success of irrigation-based agriculture at Caral–Supe may have contributed to its being eclipsed. Anthropologist Professor Winifred Creamer of Northern Illinois University notes that "when this civilization is in decline, we begin to find extensive canals farther north. People were moving to more fertile ground and taking their knowledge of irrigation with them". It would be 1,000 years before the rise of the next great Peruvian culture, the Chavín.

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