Understanding the response of the El Niño-Southern Oscillation (ENSO) to global warming requires quantitative data on ENSO under different climate regimes. Here, we present a reconstruction of ENSO in the eastern tropical Pacific spanning the past 10,000 years derived from oxygen isotopes in fossil mollusk shells from Peru. We found that ENSO variance was close to the modern level in the early Holocene and severely damped ~4000 to 5000 years ago. In addition, ENSO variability was skewed toward cold events along coastal Peru 6700 to 7500 years ago owing to a shift of warm anomalies toward the Central Pacific. The modern ENSO regime was established ~3000 to 4500 years ago. We conclude that ENSO was sensitive to changes in climate boundary conditions during the Holocene, including but not limited to insolation.
ResumenEl valle de Asia, situado a 100 kilómetros al sur de Lima, jugó un rol de importancia durante el Horizonte Medio. En efecto, los contextos funerarios de Huaca Malena, así como los finos textiles que los acompañan indican una fuerte relación con Wari, Pachacamac, la Costa Central y la Costa Norte. De acuerdo con la evidencia textil, el tránsito del Horizonte Medio al periodo Intermedio Tardío incrementó las relaciones con la costa central.Para el periodo Intermedio Tardío, de acuerdo a la información etnohistórica, el valle estuvo habitado por los coayllo, quienes tributaban a Pachacamac. Durante el Horizonte Tardío, los incas construyen importantes centros administrativos en el valle, y la cerámica durante este periodo se relacionó fuertemente con los estilos propios de los vecinos valles norteños de Mala,
Pachacamac is the name of the 15th-16th century Inca sanctuary on the Peruvian coast as well as the name of one of the principal oracles of Inca divinities. This effigy would have been destroyed by Pizarro in 1533 during his visit to the great monumental complex, and as such the originality and antiquity of the wooden statue-the so-called Pachacamac Idolhave been the subject of much controversy and debate. We present here previously unpublished dates that confirm its manufacture during the Middle Horizon (AD 500-1000), as well as evidence of its original polychromy. Traces of colors were observed on its different sections with portable microscopy and analyses with two different X-Ray Fluorescence spectrometry techniques, leading to identification of yellow, white, and red mineral pigments, including the presence of cinnabar. Dated between the 8th and 9th centuries, the statue would have been worshipped for almost 700 years, from the time of its creation to the time of the Spanish conquest, when Pachacamac was a major place of pilgrimage. These data not only offer a new perspective on Pachacamac's emblematic sacred icon, but also on the colorful practices of the Pre-Hispanic Andes.
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