Moose River Basin: geology and mineral potential - Geology Ontario

Mesozoic Palynology
Upper Albian
A distinctive palynoflora comprising 25 species was obtained by Norris et
al. (1976) from outcrop on the east bank of the Mattagami River in Kipling
Township, 0.8 km north of the foot of Long Rapids which is 9.7 km north of
Smoky Falls.
Apart from long-ranging species, the following are noteworthy:
Appendicisporites problematicus (Burger) Singh (Plate 4, fig. 21, 22)
Cicatricosisporites augustus Singh
Cicatricosisporites australis (Cookson) Potonie (Plate 3, fig. 17,18)
Cicatricosisporites hughesi Dettmann (Plate 3, fig. 16)
Cicatricosisporites sp. cf. C. hallei Delcourt and Sprumont (Plate 4, fig. 3)
Costatoperforosporites foveolatus Beak (Plate 3, fig. 32-34)
Cupuliferoidaepollenitesparvulus (Groot and Penny) Dettmann
Distaltriangulisporites perplexus (Singh) Singh (Plate 2, fig. 23)
Ornamentifera baculata Singh
Pristinuspollenites inchoatus (Pierce) B.D. Tschudy
Retitricolpites vulgaris Pierce
Rugubivesiculites reductus Pierce (Plate 10, fig. 9-12)
Tricolpites sagax Norris
Trilobosporites minor Pocock
Similarities with the I. purverulenta-C.annulatus Zone (late Middle and
early Late Albian) are evident. In addition, however, Pristinuspollenites
inchoatus, Rugubivesiculites reductus, Cupuliferoidaepollenites parvulus,
Retitricolpites vulgaris and Tricolpites sagax characterize this sample. These
species occur together in the Upper Albian of Alberta (Norris 1967; Singh
1971).
Norris, Jarzen, and Awai-Thorne (1975) have also reported the occurrence
of these species together with marine dinoflagellate assemblages in the upper
part of their Early Tricolpate Suite and higher subsurface Cretaceous horizons
in southern Alberta, suggesting an age of Late Albian for the base of this inter
val. Furthermore, the latter three angiosperm species occur together only near
the Subzone IlC-Zone III boundary of the Atlantic Coastal Plain, and placed by
Doyle and Robbins (1977) at the Upper Albian/Cenomanian boundary. Thus a
Late Albian age is considered probable for this sample, although further work
on the outcrop is required to confirm this.
CORRELATIONS
Correlations between the Moose River Basin, the Atlantic Coastal Plain
and Western Canada are shown in Figure 4.1. These correlations are based on
spore-pollen distributions as indicated in the previous discussion.
The Mattagami Formation was deposited principally during the Middle
and Late Albian and represents part of a major phase of cratonic sedimentation
recognizable also in Alberta, Saskatchewan, and Manitoba. These Albian sedi
ments are entirely non-marine in the Moose River Basin but farther west they
interdigitate with marine sediments (Singh 1971), e.g. Loon River Formation,
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