Lm. Melnikova et al., CAMBRIAN BRADORIIDA AND PHOSPHATOCOPIDA (ARTHROPODA) OF THE FORMER SOVIET-UNION, Journal of micropalaeontology, 16, 1997, pp. 179-191
Some 40 bradoriid and phosphatocopid (Arthropoda) species are known fr
om the Cambrian of the former Soviet Union. The faunas occur chiefly i
n Asia (mostly Siberia and Kazakhstan; also Kirghizia); west of the Ur
als bradoriid and phosphatocopid faunas are sparse, occurring in the L
eningrad region, Belarus and Estonia. Most specimens are recovered as
crack-out material from elastic and impure carbonate rocks; acid resis
tant valves from limestones are a minor component of the known faunas.
Early Cambrian (Atdabanian-Botomian) faunas are widespread; middle an
d late Cambrian faunas are scarcer and are known largely from Siberia
and Kazakhstan. Though many species are seemingly short-ranging, curre
ntly most have only local biostratigraphic significance, with only a f
ew having practical international correlative value. Palaeogeographica
lly, faunas west of the Urals show affinites with those of the Early P
alaeozoic Baltica and Avalonia palaeocontinents (Olenellid trilobite r
ealm). Siberian and central Asian (Kazakhstan, Kirghizia, Gorny-Altay-
Mongolian belt) faunas show clear affinities with those of palaeoconti
nental South China and eastern Gondwana (Redlichiid trilobite realm).