Caral, South America’s Oldest City (2600–1600 BC): ENSO Environmental Changes Influencing the Late Archaic Period Site on the North Central Coast of Peru

• Published in: Water (Basel) 2022-05, Vol.14 (9), p.1403
• Main Author: Ortloff, Charles R.
• Format: Article
• Language: English
• Subjects: Agricultural land; Agricultural resources; Agriculture; Analysis; Beach ridges; Beaches; Bottomland; Canals; Coastal zone; Coasts; Deposition; Drainage; Drought; El Nino; Environmental changes; Eolian sands; Flood damage; Flooding; Floods; Fluid dynamics; Fluid mechanics; Food; Food supply; Geophysics; Groundwater; Groundwater levels; Landscape; Marine resources; Ocean currents; Ridges; Rivers; Sediments; Shellfish; Slurries; Social aspects; Society; Soil erosion; Southern Oscillation; Sustainability; Swamps; Valleys; Water table; Water, Underground
• ISSN: 2073-4441; 2073-4441
• DOI: 10.3390/w14091403

The Late Archaic Period (2600–1600 BC) site of Caral, located ~20 km inland from the Pacific Ocean coastline in the Supe Valley of the north central coast of Peru, is subject to CFD analysis to determine the effects of ENSO (El Niño Southern Oscillation) events (mainly, El Niño flooding and drought events) on its agricultural and marine resource base that threatened societal continuity. The first step is to examine relics of major flood events that produced coastal beach ridges composed of deposited flood slurries—the C14 dating of material within beach ridges determines the approximate dates of major flood events. Of interest is the interaction of flood slurry with oceanic currents that produce a linear beach ridge as these events are controlled by fluid mechanics principles. CFD analysis provides the basis for beach ridge geometric linear shape. Concurrent with beach ridge formation from major flood events are landscape changes that affect the agricultural field system and marine resource food supply base of Caral and its satellite sites- here a large beach ridge can block river drainage, raise the groundwater level and, together with aeolian sand transfer from exposed beach flats, convert previously productive agricultural lands into swamps and marshes. One major flood event in ~1600 BC rendered coastal agricultural zones ineffective due to landscape erosion/deposition events together with altering the marine resource base from flood deposition over shellfish gathering and sardine and anchovy netting areas, the net result being that prior agricultural areas shifted to limited-size, inner valley bottomland areas. Agriculture, then supplied by highland sierra amuna reservoir water, led to a high water table supplemented by Supe River water to support agriculture. Later ENSO floods conveyed thin saturated bottomland soils and slurries to coastal areas to further reduce the agricultural base of Supe Valley sites. With the reduction in the inner valley agricultural area from continued flood events, agriculture, on a limited basis, shifted to the plateau area upon which urban Caral and the satellite sites were located. The narrative that follows then provides the basis for the abandonment of Caral and its satellite Supe Valley sites due to the vulnerability of the limited food-supply base subject to major ENSO events.