We reconstruct aspects of the history of Easter Island over the last 4-5 ce
nturies based on the study of a core from Rano Raraku Lake, situated in the
crater that contains the quarry of the island's giant statues or moai. We
use microfossils of plants and animals to identify five zones. The last thr
ee of these are separated by waves of immigration from South America and fr
om the subantarctic. We argue that the first or South American wave, dated
to the second half-of the 14th century, may represent a visit by South Amer
ican Indians. Magnetic information, pollen, diatoms, chrysophyte stomatocys
ts and fossil plant pigments reveal a synchronism between the South America
n contact and the cessation of moai quarrying. We therefore suggest that Am
erindians contributed to the cultural collapse of the island. The second or
subantarctic wave may reflect an early European Visit to the island, possi
bly by Cpt. James Cook in 1774, or by Jacob Roggeveen in 1722.