Speleothem formation is influenced by several factors, and particularl
y, by climatic factors. The latter influence the lithostratigraphy of
endokarstic deposits, crystalline fabrics, types and abundance of poll
ens, isotopic ratios H-2/H-1, C-13/C-12, 18(O)/O-16. Thus speleothems
can constitute remarkable palaeoclimatic sequences and, sometimes they
can record astronomical cycles. First we describe the different cryst
alline fabrics and the different morphological types of stalagmitic se
ries. Then we recall the chronological potentialities of speleothems.