Correlation of the type Bashkirian Stage (Middle Carboniferous, South Urals) with the Morrowan and Atokan series of the midcontinental and western United States
Jr. Groves et al., Correlation of the type Bashkirian Stage (Middle Carboniferous, South Urals) with the Morrowan and Atokan series of the midcontinental and western United States, J PALEONTOL, 73(3), 1999, pp. 529-539
The graphic correlation technique has been used to directly relate the stra
tigraphic appearances of key species in the Bashkirian Stage stratotype to
those in a North American composite section. The type Bashkirian is separat
ed from the underlying Serpukhovian Stage by an erosional unconformity and
associated lacuna of undetermined, but probably minor duration. Accordingly
, the base of the type Bashkirian (base of Bogdanovkian Horizon) is only sl
ightly younger than the international mid-Carboniferous boundary. A level w
ithin the upper part of the Tashastian Horizon (Upper Bashkirian Substage)
most likely correlates with the Morrowan-Atokan boundary. This level roughl
y coincides with a sequence boundary at the Bashkirian stratotype and with
a regional unconformity in the North American midcontinent. The top of the
Bashkirian Stage (top of Asatauian Horizon) is lower Atokan in North Americ
an terms. On the basis of recent Ar-40/Ar-39 and SHRIMP zircon geochronolog
y studies, the age of the mid-Carboniferous boundary is estimated at 314 Ma
and a horizon of early Atokan age is dated at 310.8 Ma. Accepting the pres
ent biostratigraphic correlations, these Values suggest a duration for the
Bashkirian Stage of slightly more than 3.2 m.y. and a duration of the Morro
wan Series of slightly less than 3.2 m.y.