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1.- Increased runoff and groundwater discharge as evidenced by late Pleistocene phreatophyte assemblages in the Pampa del Tamarugal Basin, Atacama Desert, northern Chile (21 degrees S)
Geological Society of America (GSA); Boulder, CO; USA; United States, 2006
Geological Society of America, 2006 annual meeting
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2.- Late Pleistocene organic remains in Pampa del Tamarugal, northern Chile (21 degrees S); implications for past precipitation changes in the western Precordillera
Geological Society of America (GSA); Boulder, CO; USA; United States, 2006
Geological Society of America, 2006 annual meeting
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