Varved lacustrine sediments have been found from high latitude to low latit
ude, even in tropical area. Paleoenvironmental and paleoclimatic research h
as increasingly relied on the use of varved sediments to provide high-resol
ution geochronologies and climatic reconstructions. However, a special depo
sitional environment is necessary for varve formation and preservation. Gen
erally, varves can be found in the sediments of maar lakes because of their
special geological and hydrological environment. The preliminary research
showed that a few carbonate laminations are developed in the Huguangyan maa
r lake, south China. They are poorly developed and not annual laminations,
and may be related to periodically drought. Diatomaceous laminations are fo
und in the maar lakes in northeast China. Diatomaceous laminations with cyc
lic nature corresponding with seasonal diatom blooming are the credible nat
ural clock.