Rr. Rogers et al., AR-40 AR-39 AGE AND CORRELATION OF THE NONMARINE 2 MEDICINE FORMATION(UPPER CRETACEOUS), NORTHWESTERN MONTANA, USA/, Canadian journal of earth sciences, 30(5), 1993, pp. 1066-1075
The age of the nonmarine Two Medicine Formation of northwestern Montan
a is currently based upon correlations with K-Ar-dated Western Interio
r ammonite zones. Ar-40/Ar-39 dating of biotite and plagioclase separa
ted from four bentonites and one crystal-rich tuff permits for the fir
st time direct determination of the age of Two Medicine strata. Biotit
e and plagioclase from a bentonite 10 m below the top of the Two Medic
ine Formation yield concordant Ar-40/Ar-39 ages of 74 Ma, while biotit
e and plagioclase from two bentonites and a crystal-rich tuff from app
roximately 100 m above the base of the formation cluster in age around
80 Ma. The total duration of Two Medicine deposition is estimated usi
ng these new radio-isotopic ages via extrapolation of an average rock
accumulation rate. The new Ar-40/Ar-39 ages facilitate regional correl
ation of the dinosaur-dominated paleofauna recovered from the Two Medi
cine Formation, and help constrain the timing of the Claggett and Bear
paw transgressions. The ages support correlation of the richly fossili
ferous upper lithofacies suite of the Two Medicine Formation with expo
sures of the Judith River Formation in Dinosaur Provincial Park, Alber
ta, Canada. Radioisotopically dated exposures of the Judith River Form
ation within Montana that include important Judithian ''age'' mammal l
ocalities correlate approximately with middle and lower parts of the m
iddle lidiofacies suite of the Two Medicine Formation. The new Ar-40/A
r-39 ages further indicate that the transgressions of the Claggett and
Bearpaw seas culminated within northwestern Montana at ca. 79.6 and 7
4.0 Ma, respectively.