this , together with the fact that vegetation , weathering processes , montane glaciers , lake size , lake salinity , and so forth are all likely to reflect the diverse aspects of climatic change differently , underscores the strictures of cooke ( 2 ) and flint ( 3 ) against the use of pluvials and intrlvasas a basis for subdividing quaternary time in africa .
C0040363
to
C0001737
africa