Pf. Karrow et al., A proposed diachronic revision of late Quaternary time-stratigraphic classification in the eastern and northern Great Lakes area, QUATERN RES, 54(1), 2000, pp. 1-12
A succession of stratigraphic codes (1933, 1961, 1983) has guided attempts
to refine classifications and naming of stratigraphic units for Quaternary
deposits of the Great Lakes region. The most recent classifications for the
late Quaternary of the Lake Michigan lobe (1968) and the eastern Great Lak
es (1972) have been widely used, but later work has created the need for re
vision. An attempt has been made to integrate the two previous classificati
ons following the diachronic system of the 1983 Code of Stratigraphic Nomen
clature, A new nomenclature for the higher, more broadly recognized units w
as presented in 1997, We here present the diachronic nomenclature for finer
subdivisions recognized in the eastern and northern Great Lakes. Following
the interglacial Sangamon Episode, the three parts of the Wisconsin Episod
e are further subdivided as follows: the Ontario Subepisode (former Early W
isconsinan) comprises the Greenwood, Willowvale, and Guildwood phases; the
Elgin Subepisode (former Middle Wisconsinan) comprises the Port Talbot, Bri
mley, and Farmdale phases; and the Michigan Subepisode (former Late Wiscons
inan) consists of Nissouri, Erie, Port Bruce, Mackinaw, Port Huron, Two Cre
eks, Onaway, Gribben, Marquette, Abitibi, and Driftwood phases, Succeeding
interglacial time to the present is the Hudson Episode. (C) 2000 University
of Washington.