Three hundred twenty one species of graptolites, chitinozoans, acritarchs,
cephalopods, trilobites, brachiopods, scolecodonts, conodonts, bryozoans, o
stracodes, gastropods, crinoids, tetracorals, tabulates, heliolitids, strom
atoporoids, and tentaculitids were recorded in the Silurian type areas of E
ast Siberia. Three type areas, namely, Moiero, Turukhansk, and Noril'sk, ar
e situated within the belt of shallow shelf facies predominantly bearing be
nthic species intermediate between the deep-water and shoal biotas. Faunal
and floral evolutionary stages were analyzed within local biointervals that
correspond to the global biointervals (biochrons). The species of wide and
limited stratigraphic ranges and peculiarities of their appearance and dis
appearance were revealed. The major trend of species evolution in the type
Silurian areas of East Siberia is their mass appearance and disappearance a
t the initial and terminal Silurian time. This was associated with the glob
al Silurian transgression at the beginning of the period and with the globa
l regression at the end. Both events affected most sedimentary basins of th
e platform. Secondary stages were associated with oscillations of the globa
l sea level.