P. Mourguiart et al., LIMNOLOGICAL AND CLIMATOLOGICAL CHANGES I N THE LAKE-TITICACA BASIN (BOLIVIA) DURING THE LAST 30 MILLENNIA, Comptes rendus de l'Academie des sciences. Serie II. Sciences de la terre et des planetes, 325(2), 1997, pp. 139-146
A multidisciplinary approach has allowed the reconstruction of Late Pl
eistocene and Holocene lake fluctuations in the Lake Titicaca basin. T
hree high lake levels (prior to 25/28 kyr BP, between 14 and 10.5 kyr
BP and from 0.4 kyr BP) and two severe droughts (25/28 and 14 kyr BP a
nd 10.5 and 0.4 kyr BP) are the main paleohydrological characteristics
of the Lake Titicaca evolution.