The bed-by-bed standard of the Silurian for East Siberia is used to correla
te stratigraphic sequences all over the Siberian platform and Taimyr. Fossi
l faunas and floras of the standard are very representative, because the or
iginal type sections of the standard consist of deposits accumulated in sha
llow shelf settings favorable for biota evolution. Consecutive beds of the
standard are characterized by distribution parameters (abundance rates and
size ranges) of the following fossil groups: algae, stromatoporoids, tabula
tes, heliolitids, rugose corals, crinoids, gastropods, ostracodes, tentacul
itids, bryozoans, conodonts, scolecodonts, bivalves, brachiopods, trilobite
s, cephalopods, acritarchs, chitinozoans, and graptolites. The biocoenotic
analysis is based on data characterizing the taxonomy and relative abundanc
e of fossils in oryctocoenoses, and on the structure of the latter.