Debris flows have deposited inorganic Laminae in an alpine lake that is 75
kilometers east of the Pacific Ocean, in Ecuador. These storm-induced event
s were dated by radiocarbon, and the age of laminae that are Less than 200
years old matches the historic record of El Nino events. From about 15,000
to about 7000 calendar years before the present, the periodicity of elastic
deposition is greater than or equal to 15 years; thereafter, there is a pr
ogressive increase in frequency to periodicities of 2 to 8.5 years. This is
the modern El Nino periodicity, which was established about 5000 calendar
years before the present. This may reflect the onset of a steeper zonal sea
surface temperature gradient, which was driven by enhanced trade winds.