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This document is a correction notice for an article titled "Taguatagua 3: A new late Pleistocene settlement in a highly suitable lacustrine habitat in central Chile (34°S)" published in the journal PLoS ONE. The correction states that the images for Figures 4 and 5 in the article were incorrectly switched. The correct figures and their captions are provided in the correction notice. The figures depict the relative frequencies of faunal remains and taphonomic modifications, as well as taphonomic modifications on gomphothere bones. The authors of the article are listed as Rafael Labarca, Matías Frugone-Álvarez, Liz Vilches, José Francisco Blanco, Ángela Peñaloza, Carolina Godoy-Aguirre, Álvaro Lizama-Catalán, Cristóbal Oyarzo, Carlos Tornero, Erwin González-Guarda, Ayelen Delgado, Marcela Sepúlveda, and Paula Soto-Huenchuman. [Extracted from the article]

Assessing past and ongoing climate change in the central Andes is critical for understanding the impact of future environmental changes under anthropogenic warming. Emerging from springs located in Bolivia and flowing into northern Chile's Atacama Desert, the Silala River contains inset, terraced wetland (or in‐stream) deposits that provide a unique opportunity to study the impact of past hydroclimate change in a sensitive groundwater system with a small catchment area. After an initial (late Pleistocene) period of deep incision to form the present ravine, in‐stream wetland fine‐grained deposits formed during three phases of aggradation dated to >8.5–1.9 ka (Unit 1), >0.65–0.2 ka (Unit 2), and <0.2 ka to the recent 20th century (Unit 4). These phases of accumulation were coeval with periods of well‐dated records of elevated groundwater tables throughout northern Chile. Phases of abrupt downcutting occurred due to a lowering of the water table after 1.9 ka and before 0.2 ka. The cycle of erosion and deposition clearly continues to the present as evinced by the very recent (21st century) incision of Unit 4 (>1.5 m in some areas) throughout sectors of the Silala where dried‐out standing vegetation can be seen. Such recent incision may be due to multiple different factors, including recent climate change coupled with intense extraction of groundwater resources by the copper mining industry. This article is categorized under:Human Water > Water GovernanceScience of Water > Hydrological ProcessesScience of Water > Water and Environmental Change [ABSTRACT FROM AUTHOR]