“…Further east, in the Urals, marine strata of Vereian age rest on the marine Bashkirian stratotype. In the midand southern Urals, fusulines around the Bashkirian/ Moscovian boundary are known from several sections (Sinitsyna & Sinitsyn, 1987;Ivanova, 2000Ivanova, , 2008Kulagina, 2008Kulagina, , 2009Kulagina et al, 2009). However, a break between the Bashkirian and the Moscovian could exist in some or all these areas (Ektova, 1969), this break being most conspicuous in the Moscow Basin.…”