Chronology, stratigraphy and hydrological modelling of extensive wetlands and paleolakes in the hyperarid core of the Atacama Desert during the late quaternary

Marco Pfeiffer, Claudio Latorre, Calogero M. Santoro, Eugenia M. Gayo, Rodrigo Rojas, María Laura Carrevedo, Virginia B. McRostie, Kari M. Finstad, Arjun Heimsath, Matthew C. Jungers, Ricardo De Pol-Holz, Ronald Amundson

Research output: Contribution to journalArticle

9 Citations (Scopus)

Abstract

The halite-encrusted salt pans (salars) present at low elevations in the hyperarid core of the Atacama Desert in northern Chile are unique features of one of the driest and possibly oldest deserts on Earth. Here we show that these landscapes were shallow freshwater lakes and wetlands during the last glacial period and formed periodically between ∼46.9 ka and 7.7 ka. The moisture appears to have been sourced from increased Andean runoff and most of our chronologies for these deposits were coeval with the Central Andean Pluvial Event (17.5–14.2 ka and 13.8–9.7 ka), but we also find evidence for older as well as slightly younger wet phases. These environments supported a diverse hygrophytic-halophytic vegetation, as well as an array of diatoms and gastropods. Using a regional hydrological model, we estimate that recharge rates from 1.5 to 4 times present were required to activate and maintain these wetlands in the past. Activation in the late Pleistocene was part of a regional enhancement of water resources, extending from the Andes, downstream and through riparian corridors, to the lowest and most arid portions of the desert itself. This fundamentally unique environment was encountered by the earliest human explorers in the region, and most likely facilitated migration and encampments on a landscape that at present lacks macroscopic life on its surface.

Original languageEnglish (US)
Pages (from-to)224-245
Number of pages22
JournalQuaternary Science Reviews
Volume197
DOIs
StatePublished - Oct 1 2018

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hydrological modeling
stratigraphy
wetland
desert
chronology
deserts
wetlands
salt pan
Bacillariophyceae
present
riparian areas
halite
Last Glacial
hydrologic models
water resources
gastropod
Chile
activation
Gastropoda
recharge

Keywords

  • Atacama desert
  • Hyperaridity
  • Late quaternary
  • Paleogeography
  • Sedimentology
  • South America
  • Wetlands

ASJC Scopus subject areas

  • Global and Planetary Change
  • Ecology, Evolution, Behavior and Systematics
  • Archaeology
  • Archaeology
  • Geology

Cite this

Chronology, stratigraphy and hydrological modelling of extensive wetlands and paleolakes in the hyperarid core of the Atacama Desert during the late quaternary. / Pfeiffer, Marco; Latorre, Claudio; Santoro, Calogero M.; Gayo, Eugenia M.; Rojas, Rodrigo; Carrevedo, María Laura; McRostie, Virginia B.; Finstad, Kari M.; Heimsath, Arjun; Jungers, Matthew C.; De Pol-Holz, Ricardo; Amundson, Ronald.

In: Quaternary Science Reviews, Vol. 197, 01.10.2018, p. 224-245.

Research output: Contribution to journalArticle

Pfeiffer, M, Latorre, C, Santoro, CM, Gayo, EM, Rojas, R, Carrevedo, ML, McRostie, VB, Finstad, KM, Heimsath, A, Jungers, MC, De Pol-Holz, R & Amundson, R 2018, 'Chronology, stratigraphy and hydrological modelling of extensive wetlands and paleolakes in the hyperarid core of the Atacama Desert during the late quaternary', Quaternary Science Reviews, vol. 197, pp. 224-245. https://doi.org/10.1016/j.quascirev.2018.08.001
Pfeiffer, Marco ; Latorre, Claudio ; Santoro, Calogero M. ; Gayo, Eugenia M. ; Rojas, Rodrigo ; Carrevedo, María Laura ; McRostie, Virginia B. ; Finstad, Kari M. ; Heimsath, Arjun ; Jungers, Matthew C. ; De Pol-Holz, Ricardo ; Amundson, Ronald. / Chronology, stratigraphy and hydrological modelling of extensive wetlands and paleolakes in the hyperarid core of the Atacama Desert during the late quaternary. In: Quaternary Science Reviews. 2018 ; Vol. 197. pp. 224-245.
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abstract = "The halite-encrusted salt pans (salars) present at low elevations in the hyperarid core of the Atacama Desert in northern Chile are unique features of one of the driest and possibly oldest deserts on Earth. Here we show that these landscapes were shallow freshwater lakes and wetlands during the last glacial period and formed periodically between ∼46.9 ka and 7.7 ka. The moisture appears to have been sourced from increased Andean runoff and most of our chronologies for these deposits were coeval with the Central Andean Pluvial Event (17.5–14.2 ka and 13.8–9.7 ka), but we also find evidence for older as well as slightly younger wet phases. These environments supported a diverse hygrophytic-halophytic vegetation, as well as an array of diatoms and gastropods. Using a regional hydrological model, we estimate that recharge rates from 1.5 to 4 times present were required to activate and maintain these wetlands in the past. Activation in the late Pleistocene was part of a regional enhancement of water resources, extending from the Andes, downstream and through riparian corridors, to the lowest and most arid portions of the desert itself. This fundamentally unique environment was encountered by the earliest human explorers in the region, and most likely facilitated migration and encampments on a landscape that at present lacks macroscopic life on its surface.",
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AU - Gayo, Eugenia M.

AU - Rojas, Rodrigo

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